Abstract
The European green agenda aims to preserve the environment and climate, reduce CO2 emissions, and replace fossil fuels with renewable energy. It mostly relies on electric vehicles, energy storage, solar, and wind power plants. It requires an order of magnitude higher amount of critical minerals (In this text, the term minerals is often used for individual chemical elements, although it is common to refer to combinations of chemical elements that have a corresponding chemical composition, crystallization, and name.), poorly represented in the lithosphere, with problematic recycling, with extraction requiring considerable amounts of energy, fossil fuels and causing unacceptable damage to people and nature in countries that supply raw materials. Rising global average temperatures cast doubt on the overall effects of decarbonisation. The time frame of profit-oriented planning is too short and cannot respect the dynamics of the energy sector. Together with market uncertainty, regulations, and incentives did not encourage investors to take all the steps we had hoped for. The long-term needs and availability of key minerals are considered together with an overview of the financial and environmental conditions offered to the population in the countries where mining is carried out. Growing popular resistance to cheap and environmentally damaging mining and increasing demand for critical minerals may call into question the sustainability of current practices. The development of new technologies should be geared towards solutions that use abundant minerals in the lithosphere, while long-term sustainability requires, within a much-desired paradigm shift, that fair conditions be offered to the population of countries that supply critical minerals. The main objective of this article is to use scientifically based considerations to identify the key issues of the title topic, to assess this complex and multidisciplinary subject, and to draw feasible conclusions and recommendations.
Graphical Abstract
Coltan mine in Rubaya, Democratic Republic of Congo (taken from WikiPedia, https://en.wikipedia.org/wiki/Rubaya_mines)

1 Introduction
The global average surface air temperature during the first nine months of 2024 [1] exceeded pre-industrial levels by 1.54°C. At the same time, global annual energy consumption from fossil fuels is growing several times faster than the combined growth of energy from solar and wind power plants [2], while CO2 emissions have reached a historic maximum. These disturbing data suggest that the adequacy and appropriateness of measures taken to mitigate climate change should be re-examined. The largest global emitters of CO2 are energy and transportation [3], which brought electric vehicles, solar power plants, wind farms, and grid storage in the backbone of low-carbon technologies [4]. While phasing out fossil fuels is quite slow, the backbone solutions listed require much greater consumption of critical raw materials [5,6], geochemically scarce minerals that are present in the earth’s crust (lithosphere) in an amount considerably less than 0.01%. Already existing crisis in the supply of essential minerals is aggravated by the decline in the ore grade, which increases the energy intensity, and by the neglect of socio-environmental aspects [7]. The latter increases the resistance of the local population to companies that practice cheap mining at the expense of the environment, with harmful effects on the living world and public health. An unfavorable series of events and circumstances further increases China’s already large dominance in the field of mineral procurement. Meanwhile, green agenda could increase demand for critical minerals up to nine times in the electricity sector and up to seven times in the transport sector [8]. Faced with the laws of physics, the aforementioned actions encounter insurmountable obstacles, which is where the cause of the failures so far should be sought. All such policies and strategies which only consider one aspect could bring about severe problems in other areas.
While the world is faced with significant risks brought about by climate change [9], the regions that provide the world with minerals for low-carbon technologies are additionally threatened by multifold increased exploitation in unfavorable financial and environmental conditions [10]. Limited reserves [11], declining ore grade and increasing energy expenditure to extract and refine minerals (i.e. energy intensity), reveal a growing scarcity of most critical minerals. Many devices and systems that were called renewable cannot be renewed and rebuilt due to the scarcity of minerals. Many recent technologies are facing bottlenecks in their supply chain that has raised concerns for their future use [12]. A study of the quantities of critical minerals needed for green agenda devices and key mineral [12] reserves highlights the need to review low-carbon technologies and eliminate the negative consequences of current mineral procurement practices. The second section of this document [12] provides an overview of contemporary low-carbon solutions and an estimate of the required quantities of critical minerals, sufficient to achieve climate neutrality by 2050. An estimate of the grid storage capacity necessary for the integration of solar and wind power plants by 2050 is also provided. The third section presents the current availability of critical minerals, an overview of their reserves, resources, energy intensity, and prospects for their long-term availability. The considerations in the fourth section start from the goals of net-zero emissions in 2050 and give the aggregate quantities of batteries, electric vehicles, solar power plants, and wind power plants that need to be produced for this purpose. Based on this, the necessary amounts of critical minerals are determined and then expressed as a share of global reserves as well as multiples of current annual demand. The fifth section presents the general experiences of mineral resource exploitation in various countries and regions around the world. As a characteristic and illustrative example, the sixth section is dedicated to the financial, environmental, social, and political implications of the planned exploitation of lithium, boron, and other essential minerals in Serbia, including the Jadar River Valley, which is sought to supply the European Union (EU) and thus reduce dependence on Chinese minerals. The summary of the key findings, proposed remedies, and feasible solutions are given in Section 7, along with conclusions.
2 Contemporary low-carbon technologies and their requirements for critical minerals
Data on trends in energy consumption, changes in the energy mix, and CO2 emissions can be found in accessible and mutually consistent sources [2,13–15]. The global annual primary energy reaches 659 EJ, with less than 18% supplied from solar, wind, biofuels, hydropower, and traditional biomass. The amount of energy from fossil fuels exhibits an annual growth of 7.37 EJ, considerably larger than the most optimistic estimate (2.32 EJ) of combined growth in solar and wind from 2022 to 2023 (objective estimates state 1.21 EЈ). Relative share of coal, natural gas, and oil in fossil fuels is 0.342, 0.316, and 0.342 (relative), respectively. Road transportation and air transport use 0.144 and 0.028 (relative) of the energy from fossil fuels. As a consequence, total CO2 emissions exceeded 40 GtCO2 (41.6), thus reaching the historical maximum, with fossil fuel CO2 reaching 37.4 GtCO2, and the rest from deforestation and other sources.
The global need for critical minerals depends on the quantity and ratings of low-carbon devices, such as electrical vehicles (EV), and solar and wind power plants. It also depends on the specific amount of minerals needed to build individual unit-rated devices. Based on the net-zero emission scenario of [2], Table 1 summarizes the predicted rise in the annual production of electrical energy and the predicted increase in annual production from grid-connected solar and wind power plants. The required installed capacity of the corresponding plants is calculated using capacity factors obtained as a global average, calculated from global annual energy production and installed power in 2022. The value RES Total (Renewable Energy Sources Total) of Table 1 is larger than RES (electrical) due to a relatively small but finite share of wind and sun energy used off-grid. The last column in Table 1 (New capacity) represents the difference between globally installed capacity in 2050 and globally installed capacity in 2022. The number of units that will need to be produced by 2050 is greater than the New capacity due to the replacement of many existing sources that will have reached the end of their useful life in the meantime. This addition is not taken into account in subsequent calculations, so all estimates of the necessary amounts of critical minerals that will follow in the subsequent considerations should be considered as a lower limit.
Energy and installed power from wind and solar electrical power plants 2022–2050
| Electricity [TWh] | Installed power [GW] | RESe in 2050 = | RESe in 2050/ | RES | New capacity | |||||
|---|---|---|---|---|---|---|---|---|---|---|
| TWh | 2022 | 2030 | 2050 | 2022 | 2030 | 2050 | =Wind(e) + Sun(e) | /Electricity | Total | 2022–2050 |
| Wind(e) | 2,125 | 7,070 | 23,442 | 933 | 3,104 | 1,0292 | 54,679 | 0.7116 | 67,791 | 9,359 GW |
| Sun(e) | 1,291 | 8,177 | 31,237 | 1,134 | 7,180 | 27,430 | 26,296 GW | |||
| Electricity | 29,033 | 38,207 | 76,838 | |||||||
Wind(a) and Sun(e) raws reflect global annual electrical energy production and installed power capacity of grid-connected wind and solar power plants. The last row Electricity designates global annual production of electrical energy. The values in column RES Total are larger than in RESe due to a share of wind and sun energy used off-grid, for the production of hydrogen or other purposes. The last column New capacity corresponds to the new wind and solar power plants connected to the grid.
In addition to decarbonization in the energy sector, there are plans to replace internal combustion engine (ICE) vehicles with electric vehicles. The global share of electric vehicles has reached 3% [16], which corresponds to a number of about 40 million. Of the approximately 82 million cars sold annually, about 8% are battery-powered electric cars, about 16% are hybrid cars, while about 76% of cars have an IC-Engine [17]. Replacing all existing ICE-powered cars with battery-powered electric vehicles (BEV) would require the production of over 1.4 billion (1.4e9) EVs. Key materials required for making one BEV are obtained from [18] and listed in Table 2. The cars with ICE engines require considerably lower quantities of the key minerals. Among the critical minerals listed in Table 2, they need just 12 kg of copper and some 1 kg of manganese. The data in Table 3 was obtained in a different way, by summing the critical minerals necessary for the production of an EV battery [16,17,18,19], and adding the critical materials used in the electric motor and the glider (the rest of the car, except the battery and the electric motor) [18,19]. Some 12 kg of copper and 2 kg of manganese are required for the electric motor, and also some 16 kg of copper and 10 kg of manganese for the glider. With minor differences, there is a good match between the two tables.
Key materials for one electric vehicle with 50-kWh battery
| Cu | Li | Ni | Mn | Co | Graphite | Rare Earths (total) | Neodymium |
|---|---|---|---|---|---|---|---|
| 53 kg | 9.1 kg | 40.1 kg | 24 kg | 12.8 kg | 66.7 kg | 1.5 kg | 0.5 kg |
Key materials for one electric vehicle with 50-kWh battery
| Cu (battery) | Cu (car) | Li (battery) | Ni (battery) | Mn (battery) | Mn (total) | Co (battery) | Graphite (battery) | Neodymium (car) |
|---|---|---|---|---|---|---|---|---|
| 25 kg | 53 kg | 9 | 39 kg | 12 kg | 24 kg | 14 kg | 67 kg | 0.5 kg |
Data obtained by adding 12 kg of copper and 2 kg of manganese for the motor and some 16 kg of copper and 10 kg of manganese for the glider.
The key minerals required for wind and solar power plants are calculated from the data found in [16,17,18,19] and presented in Table 4. While the estimates for the first seven minerals are taken from the IEA publication [18], the quantity of neodymium is obtained by averaging the most recent designs, with a reduced quantity of Nd. Therefore, the ratio between the Nd and the rare earth mixture, taken from [18] and given in Table 4, differs from the expected one. Namely, in advanced designs of wind turbines, the quantity of rare earth mixture is lower than 243 kg/MW. It is important to notice that many older onshore wind turbines use gearboxes and doubly-fed induction generators; hence, the figures of Table 4 for rare earths and neodymium do not apply to them.
Key materials for wind and solar power plants in (kg/MW)
| Copper | Nickel | Manganese | Chromium | Molybdenum | Zinc | Rare earths (total) | Neodymium (*) | |
|---|---|---|---|---|---|---|---|---|
| Offshore | 7,852 | 296 | 741 | 518 | 148 | 5,407 | 243 | 50 |
| Onshore | 2,889 | 444 | 741 | 518 | 111 | 5,407 | 243 (***) | 50 |
| Copper | Silicon | Silver (**) | ||||||
|---|---|---|---|---|---|---|---|---|
| Solar | 2,814 | 3,926 | 40 |
(*) The quantity of Nd is calculated as lower average of most recent installations, and it is not in expected proportion. Similar data can be obtained by using the figures related to the battery and adding 12 kg of copper and 2 kg of manganese for the motor and some 16 kg of copper and 10 kg of manganese for the glider. (**) The quantity of Ag is calculated as the lower average of the most recent installations, taking into account most recent savings in silver usage in PV. (***) Older onshore wind turbines use gears and doubly fed induction generators which do not use permanent magnets.
Electrification will raise the demand for key minerals from 2 to 7 times by 2030 [2]. Annual demand for Cu for electrification alone is expected to increase from 5.8 to 12.2 Mt, most of it used for expanding transmission and distribution grids. Annual demand for Si (Silicon) would rise from 0.8 to 2 Mt, mostly for solar panels [2]. Recent developments have reduced the quantity of silver used in solar panels below 8 g/m2, thus reducing the requirements from 80 t of Ag for each installed GW of solar panels down to 40 t/GW.
The increasing share of solar and wind power plants creates a need for grid-connected energy storage. Wind and solar power cannot be controlled at will, and therefore excess energy must be stored and used in “dunkelflaute” intervals with no wind and no sun.
One of the storage systems promoted within the green agenda is utility-grade battery storage, although there are other solutions such as reversible hydroelectric plants, compressed air storage, thermal storage technologies, and others. It is necessary to estimate the total amount of grid storage that may be needed by 2050. In an electric power system with a total source power (p SRC), a total load (p LOAD), and a power (p INTER) arriving via interconnections with neighbouring systems, the power of energy exchange with the storage (p STOR) is given by equation (1), and it represents the first derivative of the stored energy (W STOR). The power (p SRC) corresponds to the aggregate power of controllable and uncontrollable production equation (2). For the purposes of this calculation, the instantaneous power (p SRC(t)) is presented in a simplified form, as a sum of 7 groups that differ in controllability, peak power, total annual energy, dependence on weather conditions, dynamics and characteristic time intervals. The seven components in equation (3) correspond to the instantaneous power of baseload sources (p BASE), wind power plants (p WIND), solar power plants (p SUN), run-of-river hydropower plants (p HE_ROR), dam hydropower plants (p HE_DAM), combined cycle and cogeneration gas power plants (p GASC), and open cycle gas power plants (p GASO). The power (p LOAD) (3) corresponds to the aggregate power of controllable and uncontrollable consumption. The calculation assumes that part of the load (p CONT(t)) is a flexible part of the demand, and it is modeled as the energy consumption that can be planned, managed, increased, reduced, or shifted in time if needed. Load control can help reduce the storage capacity needed. From now on, the highest flexibility targets set so far are assumed to be achieved by 2050, whether on an hourly, daily, weekly, or seasonal scale. It is also assumed that the power of the interconnections (p INTER) is not limited; that is to say, all necessary interconnections will be built and power limitations will never restrict energy exchanges where a surplus in one system coincides with a deficit in the other, at all technically and economically justifiable distances. By the nature of the changes in production and consumption, exchanges in the east-west direction are primarily on a daily basis, while exchanges in the north–south direction also include a seasonal component.
The overall calculation of minimum storage capacities is reduced to a base period of one year, performed with a 10-min resolution. It consists of determining technically, economically, and logistically feasible vectors of the instantaneous power of controllable sources (p BASE, p GASO, p GASC, p HE_ROR, and p HE_DAM) for a period of one year and with a resolution of 10 min, along with planning the changes in controllable part of the load (p CONT(t)), so as to obtain the minimum required energy storage capacity, i.e. the minimum difference between the extreme values of W STOR(t) in equation (4). It has to be noted that hydropower plant management is restricted and conditioned by inflows, while for base sources, periodic repairs must be planned and carried out. The calculation is based on the seemingly optimistic, but still partly realistic, assumption that all changes in wind and solar power, changes in power consumption, and changes in hydroelectric power plant inflows for the observed year will be known at the very beginning of the year. This assumption significantly reduces the time required to find optimal vectors using modern Matlab tools.
The calculation results yield the annual change in p STOR(t) and W STOR(t) in the case of optimal control of sources and loads. The obtained results allow for determining the power and capacity for each of the storage technologies that need to be implemented. For each of the storage technologies, there are two basic parameters that define them, namely the storage capacity (i.e. the maximum energy that can be stored in them) and the storage power (i.e. the maximum rate of change of said energy). The dependence of the required storage capacity on the share of solar and wind power plants is shown in Figure 1. The discontinuous character of the curve shown results from the fact that it is not a representation of an analytical expression, but rather a set of points obtained through individual optimization for each of the given quotas of wind and solar energy (on the abscissa). The optimization includes variables of a binary nature as well as variables with discontinuous change. For the share of wind and solar power plants planned for 2050 [2] in the scenario with zero net emissions, and for the projected annual electricity production, the total necessary storage capacity exceeds 6,000 TWh, some 8% of the global annual electricity.

Combined storage capacity of a well-interconnected system based on the share of wind and solar energy in total electricity production.
Important conclusions about the most suitable storage technologies can be obtained starting from the vector of calculated storage power p STOR(t) for a period of about a year, whose 10-min samples need to be arranged in decreasing amplitudes. The corresponding results are shown in Figure 2, for 2022 (a) and 2050 (b). The maximum storage power in 2050 will be 3,2 times larger than the average annual power of the considered electrical network. It can be seen that the intervals with extreme charging and extreme discharging power will be relatively short, suggesting that such needs can be met by battery storage.

Storage power vector reordered and sorted according to its amplitudes. In 2022 (a) and in 2050 (b). In 2050, according to the zero net emissions scenario, annual electricity production is close to 77 PWh, which corresponds to an average total load (p LOAD) of 8,790 GW.
In order to verify the viability of the present low-carbon solutions, it is of interest to study the availability of Cu, Ni, Mn, Cr, Mo, Zn, rare earths, Nd, Si, Ag, Li, Co, graphite, and some other critical materials.
3 Availability of critical minerals and prospective of their reserves and recycling
Most critical minerals are considerably more abundant in the earth’s crust (lithosphere) than in seawater. There are also critical minerals in the magma, but their concentration is too low to justify their exploitation with available technologies. The most significant source of minerals is, for now, the continental part of the lithosphere. A particularly valuable insight into the availability of minerals from the lithosphere was provided in the research of Skinner [20]. Within 10–50 km of depth, at least traces are available for 88 chemical elements. Only 12 elements are present at levels above 0.1% by weight, and these are O, Si, Al, Fe, Ca, Mg, Na, K, Ti, H, Mn, and P. These elements are considered geochemically abundant, and they were widely used in traditional industries. Notwithstanding steadily declining grade of ore, geochemically abundant minerals will be readily available and there are no major technological barriers to their extraction.
Other elements (Zn, Cr, Ni, Cu, Co, U, Sn, Ag, and Au.) are considered geochemically scarce, yet many of them are used in low-carbon devices and systems. The exploitation of scarce minerals is further complicated by the nature of their distribution in the lithosphere. They rarely form separate minerals in common rocks, and the vast majority of their content is represented as randomly distributed atoms [20] trapped by isomorphous substitution where a scarce atom replaces an atom of an abundant element. A very small fraction of the total scarce mineral content is found within geologically limited volumes in higher concentrations. These volumes are the result of some rather rare circumstances in which scarce compounds of desired minerals occur in much higher concentrations than in areas with isomorphous atomic substitutes. An example is Pb, which represents 0.001% of the continental crust, while it is obtained from ores containing at least 2% Pb. Proven Pb ore reserves are more than 105 times smaller than the total amount of Pb in the lithosphere [20].
When these very small amounts of scarce minerals are depleted, the remaining portions of scarce minerals will be present as isomorphic atomic substitutions, very difficult to exploit. When the reduction in ore grade falls below the level called mineralogical barrier, the ore is not amenable for exploitation due to logistic barriers, technological problems, and a considerable increase in energy intensity. Excluding special cases (Au, U, and Ga.), the barrier lies somewhere between 0.01 and 0.1% [20]. In the case of scarce minerals other than Pb, it is of interest to estimate their share available in concentrations higher than the mineralogical barrier, ruling out their presence as isomorphic atomic substitutes at very low concentrations.
The report [21] establishes a mineralogical barrier for Cu at 0.1%, and it states that only 0.01% of total Cu in the continental crust is found with ore grades above 0.1%. For most scarce minerals, the share of their content in the lithosphere beyond the corresponding mineralogical barrier falls between 0.001 and 0.01%. Once the barrier is reached, previously used concentration, smelting and refining can no longer be employed, and the energy demand for alternative processes can jump by a factor of 100 to 1,000 times [20]. Therefore, exploitation of ore grades below the mineralogical barrier seems rather unlikely. A visible decline in the ore grade of Au, Ag, and several other metal ores has already begun.
An overview of critical minerals is given in Table 5, largely based on [11,12,18–22], including the relevant resources, reserves, annual demand, and energy intensity (i.e., the total internal and external energy consumption required to obtain the unit quantity of the desired mineral).
Critical minerals: Demand, reserves, resources and energy intensity
| Mineral (name) | Resources [Mt] | Reserves [Mt] | Demand [Mt/year] | Energy [MWh/t] | W1Y [TWh] for 1 yr sply. | W1Y versus Welectric | W1Y versus Wprimary |
|---|---|---|---|---|---|---|---|
| Copper | 5,600 | 1,000 | 28 | 10.2 | 285.6 | 0.009837 | 0.001561 |
| Nickel | 350 | 130 | 3.6 | 48 | 172.8 | 0.005952 | 0.000944 |
| Manganese | ∞ | 1,900 | 20 | 8 | 160 | 0.005511 | 0.000874 |
| Graphite | 800 | 280 | 1.6 | 31 | 49.6 | 0.001708 | 0.000271 |
| Neodymium | 32 | 8 | 0.057 | 16 | 0.912 | 3.14 × 10−5 | 4.98 × 10−6 |
| Chromium | 12,000 | 560 | 41 | 20 | 820 | 0.028244 | 0.004481 |
| Molibdenum | 25.40 | 15 | 0.284 | 20 | 5.68 | 0.000196 | 3.1 × 10−5 |
| Zinc | 1,900 | 220 | 13 | 14.4 | 187.2 | 0.006448 | 0.001023 |
| Argentum | 1.74 | 0.61 | 0.026 | 416 | 10.816 | 0.000373 | 5.91 × 10−5 |
| Lithium | 105 | 28 | 0.18 | × | × | × | × |
| Li2CO3 | from spodumene | 0.92 | 60.5 | 55.66 | 0.001917 | 0.000304 | |
| Li2CO3 | from brine | 0.92 | 9.1 | 8.372 | 0.000288 | 4.57 × 10−5 | |
| Cobalt | 120 | 11 | 0.23 | 245 | 56.35 | 0.001941 | 0.000308 |
| Rare earth | 478 | 110 | 0.164 | 16 | 2.624 | 9.04 × 10−5 | 1.43 × 10−5 |
| Hi grade Si | ∞ | ∞ | 9 | 410 | 3,690 | 0.127097 | 0.020164 |
A certain impermanence of estimated reserves arises from their definition of being economically exploitable now or in the near future, from their dependence on the results of geological exploration and economic factors, and from the innate volatility of technological, legal, and market studies. Since the resources are defined as concentrations of minerals in the lithosphere that have reasonable prospects for eventual economic extraction in the future, they are closely related to the mineralogical barrier, presumed acceptable depth of ore bodies, new explorations, extraction difficulties, projected changes of the ore grade, and borderline energy intensity. In all cases where there are different estimates, the higher values are entered in Table 5, such as 1 Gt of copper reserves instead of commonly cited 886 Mt, 1.74 Mt of silver resources instead of 1.3 Mt [20], and similar.
In column 4 of Table 5, the current annual demand is expressed in [Mt/year]. Based on available data on energy intensity in [MWh/t], energy W1Y is calculated, which represents the total energy expenditure for the annual production of considered minerals. For reference, the W1Y quantity is also presented as a share of annual global electricity consumption, as well as a share of global primary energy. The energy required to produce lithium carbonate from spodumene is over six times greater than the energy required to produce lithium from brine [23]. The total energy required to obtain the annual lithium consumption was calculated in two ways, first assuming that all lithium is obtained from spodumene and then assuming that all lithium is obtained from brine. Reserve and resource data are given for lithium content, while energy consumption calculations are based on equivalent lithium carbonate.
Recycling can reduce critical mineral supply problems [18]. The rate of recycling depends on the logistical problems in the collection of the worn-out devices, the energy required for recycling, extraction difficulties, mineral content in the waste, and the market price of recycled minerals. The recycling rate of gold, platinum, and silver exceeds 80, 60, and 50%, respectively. Recycling rates for Cu and Al exceed 40%, while Cr, Zn, and Co have recycling rates in excess of 30% [18]. Recycling requires significant amounts of energy, particularly when the devices to be recycled have not been designed to facilitate recycling. Therefore, recycling may reduce resource depletion problems but cannot eliminate the need to use significant amounts of energy to extract minerals [2,15,18]. According to predictions published in IEA [18] for 2040, recycling and reuse of EV and storage batteries could reduce the primary supply requirement for minerals by only 12%, while the share of recycled minerals could reach 8%, both figures being rather modest results. The current practice of designing and optimizing key devices also has a negative impact on the mineral recycling potential. As an example, solar panels are being designed to achieve higher efficiency, greater robustness and durability, and lower cost. The possibility of recycling used panels is not taken into account during design, which significantly reduces the chances of recycling with reasonable energy consumption. In the long run, it makes sense to focus development efforts on technologies and devices that use minerals abundantly available in geological structures.
4 Increased share of EV, solar & wind power: Case studies and minerals expenditure
About 97% of existing cars still use ICE engines. As part of the decarbonization of transport, it is planned to replace them with battery-powered electric cars (EV) that do not use fossil fuels. After replacing all ICE-engine cars with battery-powered EVs, they will continue to be produced to replace worn-out vehicles. The amount of key minerals needed to produce one typical battery-powered EV is given in Tables 2 and 3. Based on the estimate that there are about 1.47 billion cars in the world today, it is possible to estimate the amount of minerals needed for the “first generation” of battery-powered EV. The described calculation does not take into account later needs for minerals for the replacement of worn-out EVs and their batteries. The results of the calculations are given in Table 6. The necessary total quantities of Li, Co, graphite, and rare earths exceed the current annual production from 38 to 81 times, while the required amount of cobalt is 1.71 times larger than the assessed total available reserves.
Key materials for manufacturing battery-powered EV
| Required mineral | Required quantity (Q) [Mt] | Q as a share of global reserves | Q as a share of annual demand | Energy in TWh to produce Q |
|---|---|---|---|---|
| Li | 13.38 | 0.478 | 74.317 | 466 |
| Ni | 58.95 | 0.453 | 16.374 | 2,829 |
| Co | 18.82 | 1.711 | 81.809 | 4,610 |
| Mn | 35.28 | 0.019 | 1.764 | 282 |
| Cu | 77.91 | 0.078 | 2.783 | 795 |
| Graphite | 98.05 | 0.350 | 61.281 | 3,040 |
| Rare earths | 2.21 | 0.020 | 38.684 | 35 |
The calculation of the amount of minerals for the production of EVs can be estimated in an alternative way, starting from the specific amount for each battery minerals expressed in kg for each kWh of battery capacity. Based on the information published in [2,15,16,17,18,19] it is possible to estimate the necessary specific amounts expressed in [kg/kWh]. These data are given in the second column of Table 7. With an energy consumption of 1/6 [kWh/km] and with a required autonomy of 300 km, one EV would need a battery of 50 kWh. With the EV battery capacity of 50 kWh, it is possible to calculate the total amount of required minerals in [Mt], which is given in the third column. The calculation takes into account the “first generation” of battery-powered EVs, so the need to replace EVs that have reached the end of their useful life is not taken into account here. The data in first 3 columns of Table 7 do not take into account the amounts of copper and manganese required for the glider and the electric motor. These amounts are approximately, 28 kg of copper and 12 kg of manganese for each EV. In total, figure Q 1 in the fourth column of Table 7 includes 41.1 Mt of copper and 17.64 Mt of manganese. Notice that data in the last 3 columns of Table 7 consider quantity Q (battery only) and not Q 1 (the whole car). Required amounts of battery materials Li, Co, and graphite are more than 40 times larger than the actual annual production, the amount of cobalt is larger than the available reserves, and the main conclusions are similar to those derived from Table 6. Due to the significantly increased amount of material, the extrapolated effects of falling ore grade and the consequent increase in energy needed to obtain minerals should be taken into account, which was not done on this occasion.
Key materials for manufacturing battery-powered EV
| Required mineral | Specific [kg/kWh] | Required quantity (Q) for battery only [Mt] | Required quantity for the whole car (Q 1) [Mt] | Q as a share of global reserves | Q as a share of annual demand | Energy [TWh] to produce Q |
|---|---|---|---|---|---|---|
| Li | 0.1 | 7.35 | 7.35 | 0.263 | 40.833 | 256 |
| Ni | 1.2 | 88.20 | 88.20 | 0.678 | 24.500 | 4,234 |
| Co | 0.15 | 11.03 | 11.03 | 1.002 | 47.935 | 2,701 |
| Mn | 0.15 | 11.03 | 28.67 | 0.006 | 0.551 | 88 |
| Cu | 1 | 73.50 | 114.6 | 0.074 | 2.625 | 750 |
| Graphite | 1 | 73.50 | 73.50 | 0.263 | 45.938 | 2,279 |
| Nd | 0.5 kg/car | 0.74 | 0.092 | 12.895 | 11.76 |
It is also of interest to estimate the amount of critical materials required for the construction of grid-connected battery storage and to add such figures to the ones obtained for EV batteries (Table 6). In addition to batteries, utility storage also includes compressed air technology, reversible hydroelectric power plants, thermal storage, and other technologies. According to the estimate obtained for the year 2050, shown in Figures 1 and 2, the overall, cumulative capacity and power of all the utility storage technologies reach 6,147 TWh and 3.2 × 8,790 = 28,128 GW. Batteries represent only one part of these figures, most often dedicated to short-term storage, where the instantaneous power exchange (p STOR(t)) is significant, and it covers a considerable part of the peak power needs plotted in Figure 2.
The capacity (energy) of battery storage is planned to be relatively small compared to other technologies, much smaller than the total storage capacity required, because the most common battery-based storing and recovering processes are shorter than 2–4 h. In exceptional cases, such as in India, where solar energy makes a considerable contribution during the daytime, batteries would have to withstand charge (or discharge) times of up to 10 h [15]. To increase the durability of batteries and avoid too frequent replacement of modules or cells, it is beneficial to specify a higher capacity and thus reduce changes in the relative charge of the battery. To this aim, a good practice is to install a battery with a rated capacity between 1.5 and 2 times greater than the load variation under normal operating conditions.
Batteries are planned to provide up to one-third of the total short-term flexibility of the grid [2,15]. Forecasts for battery storage needed in 2050 are constantly increasing. According to the publication World Energy Outlook [2,15] for 2022, 2023, and 2024, the prognosis of battery power required in 2050 reached 3,860 GW in World Energy Outlook 2022, increased to 4,199 GW in 2023, and reached 5,512 GW in 2024 [15]. If we assume that the batteries will provide only one-third of the peak power required to integrate wind and solar power plants in 2050 (Figure 2) and that their rated discharge time will be specified as 8 h, then the required grid-connected battery storage capacity is calculated as 75 TWh. Data on the materials needed to manufacture such batteries are taken from column two of Table 7, where they are expressed in [kg/kWh]. Critical mineral resources required to manufacture utility-grade storage batteries, to be installed by 2050, are detailed in column 3 of Table 8, expressed in [Mt].
Key materials for utility-storage batteries and EV batteries in 2050
| Required mineral | Specific kg/kWh | [Mt] for utility batteries only | [Mt] for EV batteries only | Q [Mt] = EV++utility batteries | Q as a share of reserves | Q as a share of annual demand | Energy in TWh to produce Q |
|---|---|---|---|---|---|---|---|
| Li | 0.1 | 7.50 | 7.35 | 14.85 | 0.530 | 82.500 | 517 |
| Ni | 1.2 | 90.00 | 88.20 | 178.20 | 1.371 | 49.500 | 8,554 |
| Co | 0.15 | 11.25 | 11.03 | 22.28 | 2.025 | 96.848 | 5,457 |
| Mn | 0.15 | 11.25 | 11.03 | 22.28 | 0.012 | 1.114 | 178 |
| Cu | 1 | 75.00 | 73.50 | 148.50 | 0.149 | 5.304 | 1,515 |
| Graphite | 1 | 75.00 | 73.50 | 148.50 | 0.530 | 92.813 | 4,604 |
The results suggest that, for all materials except manganese, the quantities required exceed current annual production by an order of magnitude, up to 96 times. In the case of nickel and cobalt, the required quantities are significantly higher than estimated global reserves. Since the data in Table 8 represent an optimistic estimate that does not take into account the need for replacement of worn-out cells and batteries, nor does it consider the fact that ore grade will decline, the conclusion is that the planned decarbonization trajectory is unlikely to be achieved.
The data in Table 9 show the necessary quantities of critical minerals for the production of solar panels planned for 2050. According to the data given in Table 1, achieving net-zero emissions of CO2 by 2050 requires that the total installed power of solar power plants be increased by 26,296 GW. The specific quantities of key minerals for the construction of solar power plants are given in Table 4 and expressed in kg per each MW of installed power (kg/MW). The total amount of required materials is given in Table 9. As in the previous Table, the data presented do not take into account the need to replace solar panels that have reached the end-of-life. Implementing the current decarbonization plan would require a total amount of silver more than 40 times greater than the current annual demand, exceeding estimated global reserves by more than 1.7 times. The energy required to produce solar-grade silicon is nearly twice the current annual global electricity use.
Key materials for planned solar power plants
| Required mineral (element) | Required quantity (Q) [Mt] | Q as a share of global reserves | Q as a share of annual demand | Energy in TWh to produce Q |
|---|---|---|---|---|
| Copper | 74.00 | 0.074 | 2.643 | 754.8 |
| Silicon | 103.24 | Very low | Very low | 42,327 |
| Silver | 1.05 | 1.724 | 40.456 | 437.6 |
In order to achieve net-zero-emissions of CO2 by 2050, the plan we currently rely on (Table 1) requires that the total installed power of wind power plants be increased by 9,359 GW. The specific quantities of key minerals for the construction of wind power plants are given in Table 4 and expressed in [kg/MW]. The total amount of required materials is given in Table 10.
Key materials for planned wind power plants
| Required Mineral (element) | Specific [kg/MW] | Required quantity (Q) [Mt] | Q as a share of reserves | Q as a share of annual demand | Energy in TWh to produce Q |
|---|---|---|---|---|---|
| Cu-onshore | 2,889 | 27.04 | 0.027 | 0.966 | 276 |
| Cu-offshore | 7,852 | 73.49 | 0.073 | 2.625 | 750 |
| Nickel | 444 | 4.16 | 0.032 | 1.155 | 200 |
| Manganese | 741 | 6.93 | 0.004 | 0.347 | 55 |
| Chromium | 518 | 4.85 | 0.009 | 0.118 | 97 |
| Molibdenum | 111 | 1.04 | 0.069 | 3.661 | 21 |
| Zinc | 5,407 | 50.61 | 0.230 | 3.893 | 729 |
| Rare earths | 243 | 2.27 | 0.021 | 13.868 | 36 |
| Neodymium | 50 | 0.47 | 0.058 | 8.210 | 7 |
The first two rows in Table 10 show copper consumption first for the case when all new installations would be onshore, and then for the case when all new installations would be offshore. Currently, the ratio of the former and the latter is 12:1, but it is planned that it will change to around 2:1 by 2050. Therefore, the total consumption of copper will be higher than shown in the first row, and lower than shown in the second row of Table 10. Rare earths aside, the consumption of remaining minerals for onshore and offshore power plants is not too different. Rare earths and neodymium enable the construction of directly coupled light generators without gearboxes, so that high-power wind turbines can be manufactured with relatively low weight and without excessive investment in supports and construction. However, a significant number of existing onshore wind power plants still use traditional doubly-fed induction generators (DFIG) with gearboxes, which are still planned for low-power plants. Therefore, it should be noted that the total consumption of rare earths and neodymium in Table 10 will actually be lower than it is shown, to the extent that lower power turbines with gearboxes and DFIGs are retained.
Unlike the unattainable quantities of minerals required for the construction of solar power plants, electric vehicles, and batteries (Tables 6–9), the situation is somewhat more favourable for wind power plants. The need for molybdenum and zinc is less than four years’ current global production, while the energy consumption shown for obtaining the minerals is quite achievable. The need for rare earths is very significant, exceeding their current annual production by 13 times. If the needs for rare earths required for the production of EVs are added (Table 6), then the total needs would reach an amount 52 times higher than the current annual production.
From the presented results, it can be concluded that the planned production of key devices required for the green agenda will be faced with very serious problems in obtaining critical minerals. The needs for silver and cobalt significantly exceed the available global reserves, while the needs for other minerals are up to 60–70 times higher than the current annual production, which makes the possibility of obtaining them questionable due to logistical problems, problems of ore grade decline and the increasing energy consumption in the processes of extraction and refining. Over the past 12 years, considerable efforts have been devoted to studying the energy consumption of mining and refining as a function of the decline in ore quality [24]. Developed models [25], feasible solutions for sustainable resource management [26], and estimates of the energy intensity of critical minerals [27] prove that a drop in ore grade causes a significant increase in the energy intensity of critical minerals, which can create irresolvable problems in obtaining them in larger quantities. Current practices appear to be unsustainable, which would render our renewable devices non-renewable and could force us to divert our developments and technologies towards the use of abundant minerals. A viable solution for critical minerals could be [28] one where they are not sold, but rented or leased, with strict conditions regarding recycling.
5 Countries that supply mineral raw materials – current practices
Significantly increased quantities of critical minerals create the need to open numerous new mines. The EU economy requires critical raw materials for strategic sectors such as renewable energy, digital, aerospace, and defense. The Critical Raw Materials Act [29] (CRM Act) was created to ensure EU countries’ access to a sustainable supply of minerals. Mining activities aligned with strict environmental protection standards are still costly [30,31]. Therefore, the European Union comprehends the need to exploit mineral resources in countries over which it can exert influence, including countries seeking to become members of the Union. A comprehensive map of major EU suppliers of critical materials along with their level of governance is given in Figure 3.

Major EU suppliers of critical minerals and their level of governance. The map is obtained from https://rmis.jrc.ec.europa.eu/eu-critical-raw-materials.
Recent legislation in Serbia creates the possibility of opening more than 40 mines, mostly in areas with a vibrant rural population, profitable agriculture, and strategic water reserves. It is of interest to study the willingness and interest of the countries from which the mineral raw materials are sourced to agree to the opening of new mines. If there is resistance to mining, it may gradually subside or it may become stronger over time and threaten the security of mineral supplies. One way to make such an assessment is to look at past experiences.
5.1 The global situation
The distribution of critical mineral resources is very uneven. About 70% of the total amount of cobalt comes from Congo, while about 3/4 of lithium and rare earths are found in the three countries that are the richest in these resources. China refines about 35% of nickel, 54% of lithium, 72% of cobalt, and 90% of rare earths [2]. About 79% of the global production of equipment for solar power plants, 64% of equipment for wind power plants, 68% of batteries, 33% of electrolyzers, and about 30% of heat pumps are produced in China. China’s dominance in the field of obtaining mineral resources increasingly includes Africa and South America, which complicates the position of the industry in the West. A large part of minerals is found in third-world countries such as Botswana, Guinea, Suriname, Congo, Zambia, Mali, Guyana, Namibia, Peru, Kyrgyzstan, and others. It is of great importance to study the approach and manner in which China is steadily suppressing other companies and gradually taking over resources in third-world countries. There are indications that the vast majority of mining companies’ operations in the third-world countries offer unfavourable financial and environmental conditions to the local population. Although these phenomena are difficult to quantify, this section and the next one are dedicated to studying the problem.
The Democratic Republic of Congo (DRC) supplies the world with over 70% of cobalt and significant amounts of copper. Despite vast natural resources, the DRC is one of the poorest countries in the world, with a Gross domestic product (GDP) of 649 USD per capita. Already very small, the GDP is more an indication of the value of the minerals brought out of Congo than it is of tangible benefit to the people of the DRC. There are indications [32] that the manual work of people, and very often children, is used for the collection and separation of ore, which brings unprotected workers into contact with toxic substances, exposes them to the risks of landslides and rockfalls, and causes illness, loss of life and considerably shorter average human lifespan [32,33,34]. Disintegration of the national economy, dysfunctional transport, and unavailability of electricity are cited [33] as the main problems in maintaining reliable exploitation of mineral resources in the DRC. The expansion of industrial-scale cobalt and copper mines in the DRC has led to the forced eviction of entire communities and grievous human rights abuses including sexual assault, arson, and beatings [34].
It is necessary to study and understand the objectives of multinational mining companies that come to third-world countries to exploit critical minerals. Past experience shows that mining companies are interested in operating in countries with high corruption potential, dysfunctional democracy, and governments that abuse institutions and do not respect the separation of judicial, executive, and legislative affairs [32,33,34]. Stable institutions, functional democracy, and a high level of environmental protection largely prevent traditional and cheap mining. Traditional nineteenth-century mining involves the construction of tailings and process waste dumps, the use of large amounts of fossil fuels, insufficient electrification, and the practice of releasing often polluted waters and gasses into the environment. In most cases [30,31,32,33,34], mining is more profitable if mining operations do not comply with environmental standards, which is very likely in countries with high corruption capacity, where autocratic leaders can persuade the population to accept nineteenth-century mining with tailings deposits and release of toxic waters. In exchange for political support or for lucrative reasons, key autocratic leaders may be willing to enter into non-transparent contracts and agreements that are fundamentally unfavourable to the general population. The outcome is the exploitation of mineral resources for negligible compensation, but with the thorough devastation of water, land, air, and the living world. Unwanted effects of this approach are the rebellion of the local population, which can lead to a halt in exploitation, but also to armed conflicts and civil war [35]. What is not sufficiently appreciated is the fact that the traditional approach of companies from the West increases China’s room for expansion, which offers the local population of African countries somewhat more favourable financial conditions and, if necessary and convenient, a significantly higher level of environmental protection, thanks to which it gradually takes over key supplies of critical minerals.
Recourse to traditional, low-cost mining with landfills provides significant savings to the investor and makes mineral exploitation much more profitable. Namely, although new technologies enable mining without tailings dumps and without releasing problematic water and gases into the environment [36,37,38,39,40,41,42,43,44,45,46,47,48,49,50], they are, for the time being, considerably more expensive. Instead of implementing new technologies and accepting significant costs of remediation and crop recovery, an investor can choose a completely different way to do business in third-world countries. In countries with high corruption potential, investors could focus on establishing mutual understanding with local political leaders. By funding media campaigns, it is possible to try to persuade local people to accept harmful traditional mining without rebelling and without hurting the public image of local autocrats. The described approach prevails in plenty of cases [30,31,32,33,34,35]. In the long run, it can significantly threaten the security of the mineral supply. Despite political statements and promises that the EU will guarantee the environment, human rights, and health of people in the countries from which it sources minerals, and despite the EU’s commitment to a fair distribution of mining profits, leading European companies continue to use minerals from the Managem mine in Morocco, as well as from DRC, where there is environmental devastation, water pollution, child abuse and endangering of basic human rights [51]. The described practice could be more profitable, but it does not ensure the security of supply in the long term and it paves the way for Chinese investors. The Critical Raw Material Act of the EU [29] aims to reduce dependence on China and has paved the way for more mining, but there are no provisions that would prevent successful mining companies from selling their mines, concession, concentrate, or ore to China.
Chinese investors are ready to offer more advanced and environmentally friendly forms of mining wherever this approach gives them an advantage, puts them in a favourable position and allows them to acquire and control new mineral reserves. Moreover, Chinese Bank and Insurance Green Guidelines are rather strict and surpass in quality when compared with European practices. However, in cases where respect for the environment is not a requirement or does not bring them adequate benefits, they too resort to traditional mining with tailing dumps, and landfills, with the releasing of toxic waters and with thorough destruction of the environment.
5.2 The situation in Serbia (Bor and Majdanpek)
An example of the dire consequences of traditional mining is evident in eastern Serbia, in the towns of Bor and Majdanpek, where copper production began in 1903. Mining and smelting basin Bor (RTB) is the only producer of copper and precious metals (gold and silver) in Serbia. It produces cathode copper and high-quality precious metals. As of December 2018, operations are in the hands of a Chinese investor, who has opened a new underground mine Čukaru Peki and tripled production, and announces a further increase of up to 5 times compared to the initial. Increased production led to disastrous environmental and human rights violations, unprecedented levels of environmental pollution, and a significant increase in morbidity and mortality from non-infectious diseases.
The operations are accompanied by excessive emissions of toxic substances up to 40 times above the limit values. At the same time, the income of the host country is insignificant. Based on the market value of copper (currently 9188 EUR/t) and known quantities of copper obtained from Bor and Majdanpek mines on an annual basis (close to 240,000 t), the gross income from the sale of copper amounts to 2205 million EUR. Available data for 2021 show that Serbia received only 13,6 million euros in mining rent [10]. Due to the unavailability of reliable data, it is difficult to determine the exact total revenues of Serbia from RTB, which include direct and indirect taxes and allocations on other grounds, but the total revenues are estimated to be between 50 and 60 million EUR, i.e. 2.72% of the market value of copper obtained. If the calculation base also included the value of gold, other precious metals, and valuable minerals that the investor exports from Serbia in the form of concentrates, then the share of Serbia’s income in the value of the minerals obtained would be significantly lower than 2.72%.
The Chinese investor exports a significant part of the ore concentrate that is further processed outside of Serbia, so the total amount of precious metals and valuable minerals is not known, at least not to the general public. According to statements by leading officials made on several occasions on national TV channels (RTS, Radio Television of Serbia), Serbia has the possibility to buy gold mined on its own territory with a discount of 3% compared to the market price.
It is becoming increasingly common for smelters to process arsenic-rich concentrate. According to report 1411-24 dated May 15, 2024, made in the laboratories of the Institute of Mining and Metallurgy in Bor, the concentration of cadmium in PM10 particles exceeded the limit value 35 times, while the corresponding concentration of arsenic exceeded the limit value 23 times. Relevant (and alarming) data on the average annual concentrations of cadmium and arsenic can be found in the article [52]. The corresponding impact on the environment are shown in Figure 4.

Copper mining and processing in Bor and Majdanpek is carried out without land rehabilitation and reclamation, with pollution of watercourses to the extent that the Bor River is dead in every respect (a), and with the consent of the authorities that the investor carries out work with permanent pollution that exceeds the limits by several dozen times. (b) Abandoned open pit mine. The images are obtained from the private collection of Prof. Velizar Stankovic.
In 2022, about 4,000 records of oncology patients were counted in the health center in the city of Bor. The local doctors’ claims have not been officially confirmed by the Serbian government, but they are fully consistent with data on the number of new patients registered in Bor each year, as reported by Dr. Milan Jovanovic Batut, Serbia’s National Institute of Public Health. Data on the number of patients in 2023 and 2024 are not readily available, while the government-controlled media diminish the problem and state that the total number of oncology patients in Bor is five times smaller than it actually is. Despite the alarming levels of pollution, the operations in Bor do not stop, under the pretext that jobs would be lost. About 6,000 Serbian citizens and a significantly larger number of Chinese citizens, estimated at 22,000, currently work in Bor. The arrival of Chinese investors led to the closing of jobs in smaller companies and subcontractors that employed Serbian citizens and provided specialized services to the RTB complex.
Certain mines are partly supplied with technical water from the city’s water supply system, where they have priority, so that the population remains without water during the summer months. In addition to, there is clear evidence of enormous pollution of natural spring water in the foothills of Majdanpek’s hill, where the flotation lake is located [53]. There are also plans to build a new reservoir on the Crni Timok River and completely submerge and destroy the existing groundwater source “Bogovina” which provides high-quality potable water.
Moreover, a few years ago, a Chinese investor moved the Kriveljska River from its natural bed and directed it into a tunnel dug under the mountain. A detailed and well-founded study of the impact of mine waters on the Borska, Kriveljska and, consequently, Timok rivers is presented in [54] and [55].
Since a part of the Chinese workers come to work in Serbia under penalty, there is also a Chinese law enforcement group in Bor that controls parts of the territory. The Chinese workforce often comes to Serbia without the necessary qualifications, with the intention of obtaining basic training and learning from mistakes.
According to officially available population census data from 2011 and 2022, the number of Serbian citizens in Bor has decreased by 20% in 11 years, while according to predictions for the year 2050, it will be further halved. Despite the departure of Chinese citizens who complete their training at RTB, the number of Chinese citizens who live in Bor is constantly increasing. The overall picture of Bor and Majdanpek is changing in a very unfavorable way. Apart from the modification of natural landscape and environment, almost all economic activities except mining and mining-associated activities have been suspended. The remaining population is shrinking, and living without perspective and hope. There is also a lack of ability and will for the citizens of Bor to recognize, articulate, and defend their vital interests. Instead of being the subjects of social dynamics, they are reduced to mere objects and therefore victims. The population that remains passive in the face of mining practices such as those carried out in Bor is in line with the interests of investors and it meets the interests of the current Serbian autocratic government. Although in Europe, images from Bor and Majdanpek correspond in many ways to scenes from Congo, Morocco, or Papua New Guinea. This is an alarming sign that if Europe ignores the damage its extractive sector is causing in Africa, it will soon turn these practices against itself and its own citizens.
Most examples of mining in third-world countries imply a scenario similar to the experience in Bor. Big mining companies take the concentrate or minerals (Cu, Au, Ag, Pt, and rare earths) out of the country, leaving negligible income for the local population and the state. Traditional mining with landfills is used, which leads to devastating pollution of land, water, and air, destroys biocenoses, leads to serious diseases in the population, and leaves no room for a productive life of any kind other than mining. As a consequence, strong and negative reactions from the local population are frequent, threatening the security of global mineral supply.
6 Financial, environmental, social, and political implications of the Jadar project
The efforts of EU countries to reduce their dependence on imports of critical minerals were particularly articulated in 2024, with the adoption of the EU “Critical Raw Materials Act,” Regulation (EU) 2024/1252 of the European Parliament and of the Council [29]. Announcements that old mines could be reactivated and new ones opened in EU countries have met with considerable public resistance. In an attempt to reduce its dependence on minerals imported from China, the idea of relying on the opening of new mines in Serbia was raised. The following study of the Jadar project goes beyond a narrowly professional discussion, but nevertheless contains information and conclusions of importance for the main goals and messages of this article. In what follows, a brief discussion will ensue on (i) Newly adopted Serbian laws that favour mining companies at the expense of the interests of the population, (ii) Financial effects of jadarite mineral mining, (iii) Environmental risks of the Jadar project, (iv) Views, plans and attitudes of investors, (v) Threat to water supply, (vi) EU policy so far, followed by (vii) Adverse impacts of project Jadar on relations between Serbia and the EU. Jadar Valley is shown in Figure 5.

Jadar Valley: One of the rare examples where agricultural production enables the flourishing of a traditional village, schools filled to capacity, and a large number of young people who plan to stay in the village. The area shown lies on an aquifer system of crucial importance for the Republic of Serbia. (Foto – private collection of Dr Dragana Đorđević).
6.1 Laws favouring mineral exploitation
Over the past years, the laws of the Republic of Serbia have been changed to suit the international mining companies very well, but which does not suit the citizens of Serbia. In the context of the basic messages of this work, it is of interest to study the circumstances under which the Jadar project is being prepared. According to the current law on mining and geological research [56], national institutions are prevented from engaging in mineral research. This is only possible for them by order of the Government of Serbia, and since the law came into force, no such order has been issued even once. Mineral research and exploration are available to private companies, which are owned or controlled by international mining companies. The legal provisions of the same law grant the priority right of exploitation to companies that conduct research and find minerals, without the obligation of calling an international tender in order to obtain the most favourable offer. Since the current practice grants exploration rights exclusively to international mining companies, only they can obtain exploitation rights. Furthermore, these are exclusive rights, so no one can compete by offering more favourable terms. In short, Serbian laws have been changed so that the exploitation of mineral resources is entirely in the hands of foreign corporations or their subsidiaries, which have no competition. A discussion of the motives and interests of those responsible for introducing this law is beyond the scope of this article. The law was based on the corresponding legislation of Congo and Mongolia, which contains elements inappropriate for the EU, but its adoption was not opposed by EU representatives in charge of Serbia’s accession process.
There is a clearly expressed interest of international mining companies to, among other interests, exploit borates and nickel in Serbia. An excessive amount of boron in the soil prevents the growth of plants [57], while an excessive amount of nickel makes the water unsuitable for drinking. At the beginning of the twenty-first century, Serbia had regulations that limit the maximum amount of boron in the soil, which could oblige mining companies to apply modern mining technologies without landfills and without the risk of unwanted release of toxic water. However, the newly adopted regulation [58] excludes boron from the list of soil pollutants and abolishes all previous restrictions, so that investors are enabled to exploit boron and borates without fear of exceeding the limit values of soil pollution. Similarly, increased nickel concentrations in water will no longer be used to determine the chemical status of water [59], which could remove any need for big mining companies in Serbia to invest in equipment that would prevent or limit nickel pollution of water. In short, conditions have been created in Serbia for mining companies to work in a traditional way, with tailings and waste dumps, and with the release of toxic contents into the environment, without bearing any consequences, which is already happening in eastern Serbia, in Bor and Majdanpek. The image of Jadar Valley is given in Figure 6.

The photo was taken in the Jadar Valley, near exploratory wells where toxic groundwaters reach the surface. Due to the significant concentration of boron and other toxic content, the living world near the well is affected beyond repair and exterminated. (Foto - private collection of Dr Dragana Đorđević).
6.2 Financial effects of jadarite mining
This section will summarize the available information on the financial effects of the Jadar project. The conclusions that can be drawn are not favorable. Data related to the financial effects of the planned operations in the Jadar Valley are controversial, while all credible indicators indicate that the project could generate returns for investors, but would generate negligible gains for Serbian citizens, while causing unacceptable damage and permanently endangering their fundamental interests. Serbian laws and government actions related to priority exploitation rights are questionable; while data on the potential financial effects of the Jadar project from various sources differ widely. EU officials offer vague and unconvincing assurances, while credible experts point out that the EU’s intention to source critical minerals from Serbia is simply to shift environmental damage elsewhere, outside the EU. The bases for the aforementioned claims are provided within this chapter, separated by appropriate subheadings.
6.2.1 The priority right to exploit jadarite
Major investors who have arrived in western Serbia have expressed their intention to exploit boron. In the Jadar valley, deposits of the mineral jadarite have been identified, which, in addition to boron, also contains lithium. Although high concentrations of lithium and boron in the Jadar Valley were first discovered by Serbian scientists [60] in 1999, the state missed the opportunity to become the sole owner of exploitation rights. The mineral Jadarite was formally characterized in 2007 [61]. In the outcome, the priority right to exploit jadarite was not given to national institutions and companies.
6.2.2 The ruling regime’s claims
Leading Serbian politicians and promoters of the Jadar project claim that Serbia’s GDP will be increased by 10–12 billion euro [62], that lithium will primarily be used for the long-promised production of BEV in Serbia, that 20,000 new jobs will be created, and that exploitation will take place in accordance with the green agenda and with the “highest standards of life protection environment.” Serbian political leaders also stated that Serbian lithium reserves reach 10% of the global lithium reserves, although they actually represent only about 1% of global reserves [63].
6.2.3 Experts working on behalf of investor
Experts working on behalf of investors [64] claim that Serbia’s GDP will increase by 695 million instead of 10–12 billion (as the Government claims). Around 3,500 workers will be employed during the construction of the mine and plant, while 1,300 workers will be employed during the decades-long exploitation, instead of 20,000 (as Government claims). Only 40 million EUR will be collected annually in royalties when the incentive period expires, implying in this way unconfirmed information that Serbia will provide incentives to international mining companies.
6.2.4 Independent economic experts
A group of independent Serbian economic experts [65], including the former governor of the National Bank and renowned university professors, argue that the Jadar project is not economically justified and should be stopped. They state that Serbia would have negligible net income from that project on all grounds: 17,4 million euro per year, which represents 2,6 euro per capita. According to independent experts [66], endangered income from agricultural activities is estimated at 81,96 million euro per year, and it exceeds, by far, the potential effective revenues from mining activities. Under favourable conditions, raspberries from Western Serbia contribute to exports of more than 400 million euro a year. The subjective reluctance of potential buyers to opt for raspberries from the mining region can reduce sales and prices if the Jadar project is launched. Experts noted [65] that techniques of diminishing Serbia’s net income include unfounded indirect subsidies to companies linked to investors, transfers of assets and taxable flows to the tax jurisdiction of other countries, and purchase of goods, services, and often questionable consultancies almost exclusively from foreign suppliers. These are some of the reasons why mining in Serbia, on behalf of big international companies, generates insignificant revenues that do not benefit Serbia, something that can already be seen in Bor and Majdanpek and is predicted by independent experts [65] for Jadar. Moreover, foreign investors operating through a Serbia-based limited liability subsidiary give them the opportunity to earn income but avoid liability for damages, the cost of remediation and reclamation of contaminated land, and the cost of decommissioning. The damage caused in the Jadar Valley is illustrated in Figure 7.

In an effort to repair the damage shown in Figure 6, contaminated soil near the exploratory wells was removed and improperly disposed of next to a nearby pond. The water in the otherwise vibrant pond soon showed visible signs of serious contamination. (Foto – private collection of dr Dragana Đorđević).
6.2.5 Announcements, guarantees, and claims of EU representatives
Leading European representatives express the need to obtain raw materials from Serbia, thus denying claims by Serbian politicians that lithium will be used for EV manufacturing in Serbia. They also confirm that the EU is trying to obtain minerals from Serbia in order to free itself from dependence on minerals from China [67]. While EU politicians work on coercing Serbia into lithium mining, Prof. Claudia Kemfert [30,31], a German energy economist, confirms that EU countries have high environmental protection standards, which do not have to be respected in countries outside the European Union. This makes mining in the EU too expensive and introduces the tacit policy of sourcing critical minerals elsewhere. Her statements contradict the Serbian authorities’ claims that project Jadar will be carried out to the highest standards, they confirm that mining lithium in Serbia is problematic and that the potential environmental damage can be serious. Lithium mining can contaminate groundwater with heavy metals and pollute drinking water. It is confirmed [30,31] that Serbian environmental protection organizations have long rightly pointed out that the potential investors’ record of complying with environmental standards is not encouraging and that Germany’s intentions to obtain critical minerals in Serbia are simply shifting the potential environmental damage elsewhere.
6.3 Environmental risks of the Jadar project
Đorđević et al. [66] research contains fact-supported analyses that confirm the existence of an unacceptable eco‑chemical risk of jadarite mining and lithium extraction due to questionable technology solutions, and because of the specific terrain unsuitable for mining activities. The mentioned work was subjected to strict peer review, usually for reputable scientific publications. In addition, the article has resisted serious efforts to deny the facts presented and to have the article retracted. After double-checking, the published claims should be given the importance of scientifically confirmed facts. In the research Đorđević et al. [66] argue that the Jadar project threatens the water supply of 2.5 million people, it would occupy a territory where 20,000 people live, among which several thousands of farmers would lose their jobs. They state that, despite the proposed announced new technology, the company has been unable to meet legal limit values for boron in soil and water [68]. Unfortunately for the citizens of Serbia, the regulation [68] from 1994 was recently withdrawn, and according to the new one, the maximum content of boron in the soil is not registered at all, so it is possible to exploit jadarite and destroy large areas of land without violating the current Serbian regulation. Flooding in the Jadar Valley is illustrated in Figure 8.

The Jadar Valley is frequently exposed to flooding, which makes the idea of building landfills containing significant amounts of boron unacceptable due to the imminent risk of large-scale soil contamination. (Foto - private collection of Dr Dragana Đorđević).
Along with the data on the share of water-soluble boron and overall boron quantities toxic to the soil, it has been pointed out in research of Đorđević et al. [66] that the Jadar project would lead to degradation of the soil and desertification. In addition to toxins in the planned tailing dumps and landfills, toxic waters in the orebody zone bring boron, arsenic, and lithium to the surface. Đorđević et al. [66] indicate that the planned mine at Jadar, similar to nineteenth-century mines, will have tailings and waste dumps and landfills, and will discharge water into the environment. At the same time, modern technologies already in effect include zero liquid discharge solutions [69]. It is also possible to reinject water into geological layers of the ore body and deep aquifer layers containing mineralized or toxic waters, slightly away from the mine, or otherwise below the sealing layer [70]. Đorđević et al. [66] point to the already visible negative effects of land destruction around existing wells, and emphasize the mobility of boron, the high proportion of water-soluble boron, and the significant, visible effects of devastation on the surrounding land (Figure 6). Their conclusion is that the optimal solution for the Jadar project is its cancellation.
6.4 Views and plans of big investors
The investor’s attitude towards environmental issues can also be seen from public appearances of their representatives. During nationally broadcasted duel between managers of investors interested in the Jadar project, their engineers, concerned local residents and prominent representatives of the ruling regime [71], the investor’s engineers stated that the principle of engineering rationality prevents them from implementing the Jadar project in a way that would never release toxic water into the environment. They confirmed that some of the toxic water will be released under conditions of heavy, “accidental” rainfall that was characterized as “100-year waters” [71], which takes for granted that in the event of a 100-year flood, it is acceptable to expose the fertile land of western Serbia to toxic substances including boron, arsenic, and lithium. To make matters worse, the incidents described will occur much more often than once every 100 years. Due to climate change, there is a tendency for very significant amounts of precipitation to fall in an extremely short period of time. In recent years, the maximum monthly precipitation in Serbia exceeded 480 mm, the maximum daily precipitation exceeded 210 mm, and the three-day precipitation in the Jadar Valley basin exceeded 250 mm, in line with global changes [72], indicating significantly higher maximum hourly rainfall. Milutin Stefanović from the Jaroslav Černi Water Management Institute stated that 100-year floods have been occurring almost every year since 2014. Considering the intentions of investors [71], the same frequency would be observed in the spillage of toxic boron, arsenic, and lithium, diluted in water, onto the fertile soil of the Jadar Valley if the Jadar project is implemented.
Although it is cheaper and fits with “engineering rationality,” the aforementioned investors’ plan violates Article 19 of the Land Protection Law [73], which prohibits the discharge and disposal of polluting, harmful and hazardous substances and wastewater onto the land surface and into the soil. After any of these planned “accidental” spills of toxic water, Articles 20 and 21 of the same law require the immediate closure of the plant and the cessation of all mining and processing operations, while the costs of damage repairs, remediation, and recultivation would fall on the investor (“polluter pays” principle). Unfortunately, the state of Serbia does not regularly apply the aforementioned laws if the sanctions are directed at big investors. Previous experience suggests that the aforementioned closure will not occur, that remediation will not be undertaken, and that polluting mining will continue uninterrupted until the next storm.
The investors’ engineers justified [71] the “accidental” release of toxic water into the environment by the fact that, in conditions of heavy rainfall, the toxins would be diluted with large quantities of clean water brought in by precipitations. The intention of diluting hazardous and toxic substances with clean substances is contrary to environmental principles. Although inconsistently applied, even the Law on Waste Management of the Republic of Serbia [74] in its Articles 26, 38, 43, and 44 prohibits the mixing of hazardous substances with water and prohibits any dilution of hazardous substances. That is, as a principle, hazardous substances should not be diluted to reduce the concentration of toxins in an attempt to characterize the result as non-hazardous. Numerous experiences around the world indicate that insensitivity to environmental problems may be a sign that investors are inclined to cooperate closely with authoritarian regimes in order to avoid costly compliance with environmental rules, principles, and regulations.
The above-mentioned aspects are not the only and not the most important problems of the Jadar project. In their written communication with potential investors [75], prominent Serbian scientists claim that despite efforts to find an adequate interpretation of the articles of the Waste Management Act, the investors did not justify the proposal to open the processing plant, the mine and create the landfills on the aquifer ground such as the Jadar Valley, because Articles 3, 6, 44, and 65 of the Waste Management Act, as well as Article 18 (in conjunction with Articles 23 and 13) of Directive 2008/98/EC of the European Parliament and of the Council (19.11.2008, 18.02.2024) were not complied with that of Solaja [75]. The question arises as to why waste disposal is planned and designed in a manner that is contrary to the relevant laws of the Republic of Serbia and EU directives.
An illustrative and worrying example is the investors’ statements about their intention to learn from mistakes [71], as well as the statements of domestic collaborators that operations could be suspended if a major incident occurs. The promise to learn from mistakes suggests that a complete undertaking is an experiment with an uncertain outcome. Since the planned operation in the Jadar Valley would be the first example of jadarite mining, it would be carried out without previous experience in mines and plants of similar type, size, and purpose. Unfortunately, each of the mistakes that should be learned from would create permanent and irreparable damage [66] to people, living world, environment, and water supplies.
The Jadar project envisages transporting excavated materials over the top soil [76], using fossil fuels and releasing harmful dust with toxic content that would eventually settle on nearby fertile land. Combined with the considerable use of diesel fuel and natural gas in other operations, this will generate significant CO2 emissions and increase Serbia’s total emissions. According to Table 5, the energy intensity of lithium obtained from an underground ore deposit is more than six times greater than the energy required to obtain lithium from brine in salt lakes [23]. From publicly available data on the Jadar project [76], it is possible to estimate, directly or indirectly, related quantities of fossil fuels and other explicit and intrinsic energy inputs of the Jadar project. The outcome shows that the energy intensity of lithium extraction from underground jadarite ore would be, similar to the lithium obtained from spodumene, several times larger than the energy intensity of lithium extracted from salt lake brine.
Although the value of materials and goods is commonly expressed in terms of market price, long-term considerations are more reliable if values are based on energy invested and minerals consumed to produce relevant goods. The fact that much less energy is required to extract lithium from saltwater suggests that other methods of obtaining lithium are inferior. The above considerations are one of the reasons for the sevenfold drop in the price of lithium recorded since November 2022. This circumstance calls into question the prospects for earnings from the sale of lithium from Jadar Valley and emphasizes the importance of the original intentions of investors, which is the exploitation of boron and other critical minerals. This brings into focus the potential devastation of the soil and waters due to the release of rather mobile boron with a large proportion of water-soluble fraction, the risks which go unsanctioned in Serbia (Figures 6 and 7), while that would not be tolerated in the EU.
The attitude of big investors currently working in Serbia regarding environmental protection often reflects the belief in the cultural and civilizational inferiority of the local population. This attitude is reinforced by the fact that laws are enacted contrary to the interests of citizens and that even these laws are not respected when they act against the interests of big investors. There are about 250 mining landfills in Serbia, and none of them have been rehabilitated and recultivated, while violations of regulations by mining companies are controlled by a symbolic number of inspectors.
In addition to violating Serbian law, the planned and effective operation of mining companies in Serbia also violates EU environmental principles, in particular, the precautionary principle [77] (Treaty establishing the European Community, Article 174-2), the polluter pays principle (Article 174-2, as well as Article 22-1 of the German Federal Water Management Act), the principle of correction at source (former Article 130-r), the principle of sustainable development (Article 2 of the Treaty establishing the European Community, as well as the Fifth European Environmental Action Programme called “Towards Sustainability,” issued by the Commission of the European Communities in 1993), the principle of subsidiarity (the Maastricht Treaty implemented this principle in Article 3b, now defined in Article 5 of the Treaty establishing the European Community), the integration principle (Article 6) and the prevention principle (Article 174-2, former Article 130-r, also defined in the German Federal Water Management Act – Wasserhaushaltsgesetz).
6.5 Threat to water supply
In Đorđević et al. [66], the authors argue that the Jadar project would threaten the water supply of 2.5 million people. Of the three major water supply systems, the Mačva region, with which the Jadar Valley is closely connected, is the most important one. In this region, there is a unique configuration of sand and gravel deposits. They are located several tens of meters underground, with a high degree of porosity and large quantities of potable water. Deposits run along the Drina River and are directly connected to the entire terrain of the Mačva and Jadar regions. The greatest thickness of the deposit is found along the course of the Drina River, ranging from 50 to 75 m, while in the rest of Mačva, it ranges from 20 to 40 m. This area represents the most important groundwater reserve in western Serbia [78]. Đorđević et al. [66] predict that the Jadar project and its wastewater would pose a high risk of endangering water systems on a larger scale. The destruction of Serbia’s most important water system would put the water supply for a large part of the Serbian population at great risk. The impact of mining activities on water supply and groundwater resources is well studied [79,80,81,82,83,84]. The studies suggest that in aquifer systems and complex geological structures such as those in Mačva and Jadar, mineral extraction and exploration boreholes should not be carried out under any circumstances, while all drilling to significant depths may be permitted only for the purposes of monitoring groundwater quality. A similar conclusion was drawn by Serbian scientists in 2021, where it is suggested that mining should not be allowed in populated areas with fertile soil, strategic supplies of drinking water, profitable agriculture, and favorable demographics.
On 6–7 May 2021, the scientific conference “Jadar Project: What is Known” was held in the Serbian Academy of Sciences and Arts [85]. The conference brought together leading scientists, qualified experts, government representatives, experts, and managers of potential investors, as well as representatives of third parties cooperating with investors. The main results of the conference were sent to the Prime minister of the Republic of Serbia and published in the conference proceedings, with a conclusion section on pages 17 and 18 (translation in English available in [86]), stating in brief that, the Jadar project would lead to massive devastation of space, permanent changes in the character of the landscape, degradation of biodiversity, soil, forests, surface and groundwater, displacement of the local population, cessation of sustainable and profitable agricultural activities, and establishing a scenario of permanent risk to the health of residents of nearby villages and the city of Loznica. Scientists also conclude that the continuation of the uncontrolled realization of similar mining projects would lead to serious ecosystem disturbances, and environmental degradation and would be an indicator of the inability of the state, but also of the wider social community, to see the harm of such activities to the public interest. It is crucial that any form of economic development does not endanger the environment, does not lead to the displacement of population and does not deprive future generations of living space, drinking water, healthy food, fertile land, and preserved, clean, and diverse nature. Scientists have concluded that it is necessary to clean and recultivate the existing 250 landfills. They also stated that all the projects that envisage the construction of tailing dumps, waste landfills and water discharge should be banned in populated areas, as well as on fertile land, in zones of importance for water supply, and in places of importance for the preservation of wildlife. Activities similar to Project Jadar can only be allowed in uninhabited and barren deserts, far from the living world, far from people, and strategic water reserves. Given Serbia’s strategic interest in joining the European Union, mines with waste dumps, landfills, and mine water discharges should not be permitted. Implementation of the Jadar project and similar projects would leave Serbia outside the European Union. With a very high cost of environmental remediation in Serbia, the inclination and desire of EU member states to take Serbia under their umbrella of responsibility will be significantly lower.
6.6 EU policy so far
The encouragement of Serbia to become a raw material base for the EU is not accompanied by firm and unquestionable guarantees regarding environmental protection and financial gains. On the contrary, EU experts [30,31] point out that modern technologies that enable the acquisition of minerals with minimal environmental impact are currently too expensive. Therefore, they conclude that mining on EU territory is not profitable and that it takes too long to obtain the relevant permits. Given the circumstances, there is a preference and interest in acquiring minerals from countries where mining with dumps, landfills, and water discharges is permitted, and EU regulations do not apply. Responsible EU politicians point out that one should not expect their guarantees for mining operations abroad, and that the sole responsible for the environment in Serbia is the Serbian government. Serbian regulation has changed by removing upper limits for most critical pollutants [56,58,73,74], thus serving the interests of international mining companies and ignoring the interests of citizens. At the same time, despite verbal commitments from some EU politicians that mining outside the EU would not endanger the environment in other parts of the world, Europe continues to source minerals from Africa, where the environment is devastated and workers and the population are exposed to very harsh working and living conditions. The above circumstances are a reason for justified fear that the same could happen to the Jadar Valley.
Although the declared goal of the EU’s support for mining in Serbia is to free it from dependence on China, the choice of investors who should carry out such mining is not in line with the stated goal. The EU is pushing for the engagement of mining company Rio Tinto in Serbia, whose single biggest shareholder is a Chinese company [87,88,89], Chinese State Aluminium company Chinalco, while a smaller share is owned by the Chinese capital. At the same time, Rio Tinto is applying for strategic status under EU Critical Raw Materials Act in order to get funding for project Jadar from EU taxpayers. Instead of relaxing its dependence on Chinese minerals, the EU is strengthening Chinese investments in European markets.
6.7 Adverse impacts on relations between Serbia and the EU
The EU’s attempt to solve the mineral supply crisis through cheap, unsustainable mining in Serbia is questionable. The outline of the existing plan is to export the environmental hazards that accompany mining from the EU to Serbia, to the detriment of the citizens of Serbia, and to pay for it with political support from autocratic Serbian authorities. Public resistance to projects where narrow interest groups make profits at the expense of the environment is gradually growing, and therefore, the outlined plan may soon call into question the security of mineral supplies. Experiences from Papua New Guinea and Congo show that public resistance can be suppressed by the armed forces of an authoritarian government, but only in the short term. On the other hand, public unrest in Serbia and the EU’s concern for the supply of minerals, as well as the EU’s visible lack of concern for the environment and the health of citizens in Serbia, create the preconditions for the influence of non-European influential states and interest groups. In the long term, the described situation sharply conflicts with the interests of Serbia and the interests of the EU. The planned lithium mining in Serbia could threaten not only the ecosystem but also the stability of the EU itself. Controversial mining projects are fueling, among other things, a loss of confidence in the future of the EU, which is already taking political form in Hungary, Slovakia, and elsewhere, followed by a regression into local nationalisms. Even the Union’s biggest supporters are dismayed that EU taxpayers’ money could be used to fund a company whose largest shareholder is a Chinese company, to help it extract minerals cheaply on European soil, with devastating effects on the environment, while at the same time providing strong EU political support to local undemocratic authoritarian governments. The EU’s support for autocratic governments for the sake of cheap mining has fundamentally shaken the trust in the EU as the umbrella protector of the environment and democracy. Such support provides a rationale for extra-European narratives depicting a weak, divided, and manipulated Europe that compromises its fundamental values. This could lead to the marginalization of the entire continent, leaving peripheral areas at the mercy of Russia, China, and other non-European powers.
7 Discussion and recommendations
Efforts to suppress global warming, to curb the use of fossil fuels, to reach zero net CO2 emissions and to achieve climate neutrality, have been based on devices such as batteries, electric cars, solar power plants, wind farms, and grid energy storage. Manufacturing the above-mentioned devices requires very large quantities of critical minerals, which are scarcely present in the lithosphere. Their extraction requires considerable amounts of energy and fossil fuels. Recycling is often problematic, while cheap mining and processing pose considerable risks to the environment and the living world, particularly in countries sacrificed to become suppliers of raw materials. The current Green Agenda would require quantities of rare earths, graphite, silver, and cobalt exceeding their annual production by 38, 61, 40 and 81 times, respectively. The required quantities of silver and cobalt are 1,724 and 1,711 times greater than the corresponding estimated global reserves. The above arguments do not support the sustainability of the plans, primarily because the necessary devices and systems cannot be produced in the required quantities.
In this extremely complex situation that requires respect for the laws of physics rather than following cognitive shortcuts that lead to quick profits, the steps taken by the EU are quite unexpected. While the current green agenda is under threat from the centrist and nationalist right, an article [90] in a new EU plan reveals Brussels’ inclination to deregulate and thus meet the needs of big investors, rather than decarbonize and meet the long-term interests of the EU citizens. Instead of reducing excessive production, raising the goals of climate and energy justice, making the necessary adjustments for the sustainability of capitalism, and reducing the injustices of colonialism to a sustainable level that will not create conflicts, key decisions in Brussels are still made based on the profit thirst of large companies with significant influence from non-European powers.
Under these circumstances, the European green agenda and much of the current climate legislation are accelerating the infrastructural colonization of rural areas and deepening neoliberal control over the energy sector [91]. In practice, the energy transition is far from renewable, as it requires ever-increasing material and energy inputs. A viable alternative is to moderate growth to contain the ecological and climate disaster. Any further push for the green agenda risks fueling a new wave of mineral hunger [92], driven by the growing demand for mineral resources. Sustainability goals and efforts are often undermined by the profit motive of mining corporations, which remain firmly tied to permanent growth. Coupled with overly ambitious green goals, these developments could exacerbate, rather than resolve, ecological crises. Furthermore, it is also necessary to address global imbalances and decentralize industrial power concentrated in a few countries [93]. Changes are needed quickly. However, the required change is meeting resistance. Key steps must be taken by these countries, which must accept some short-term losses in order to achieve long-term objectives. The final outcome depends on the effectiveness of the scientific community and democratic processes, through which it is possible to direct the holders of executive power to suppress immediate profit motives and short-term goals for the sake of the long-term interests of the global population.
In the long term, the development and design of mass-produced devices and systems should be directed towards using minerals that are present in the geological structures and deposits at more than 0.1%, including silicon, aluminium, iron, calcium, magnesium, sodium, potassium, titanium, manganese, and phosphorus. Until then, it is important to keep in mind that the devices we currently use are not renewable due to the lack of minerals. They should therefore be designed to facilitate energy-efficient recycling, in order to reduce the extraction and processing of critical minerals.
For the sake of a secure and sustainable supply of minerals from third-world countries, it is necessary to end the current practice of cheap mining with tailings dumps, waste landfills, and massive environmental destruction. The ability of international mining companies to spot and exploit the corruption capacity of local authorities and to temporarily affect public opinion through media campaigns provides short-term results, but is not sustainable in the long term.
One of the key goals is to break China’s dominance in the supply of critical minerals. To this end, it is necessary to study the reasons for China’s growing influence in third-world countries that possess key minerals. The unrest in Congo and the civil war in Papua New Guinea have brought uncertainty in the supply of minerals, created problems on a global scale, and created a crisis of confidence in leading mining companies. To contain China and preserve the EU’s reputation and trust in third-world countries, the EU would have to preserve its reputation as a beacon of democracy, human rights, and environmental protection. China’s influence grows significantly in all cases where ephemeral and petty interests encourage the EU to provide support to autocratic regimes outside the Union. The EU’s reputation and influence decline in favor of China even in cases where competing political options within the Union are suppressed by undemocratic methods. There have also been adverse effects from recent attempts to amend the EU Corporate Sustainability Reporting Directive to shift the focus from environmental protection, climate action, and workers’ rights to competitiveness, which could reintroduce unacceptable anti-environmental attitudes and even tolerance of child and forced labor. It is of uttermost importance to contain and prevent such steps. Otherwise, this will create ample space for Chinese capital and further increase its dominance in the field of critical minerals.
To achieve long-term sustainability and regain the economic power of Europe on a global scale, it is necessary to offer fair conditions to the population of mining colonies. While traditional, environmentally unacceptable mining generates higher profits, it is not sustainable because it draws mineral suppliers into places where they expose the environment, wildlife and people to large-scale devastation that can be seen in Congo, Morocco, and the Serbian towns of Bor and Majdanpek. For the sake of long-term sustainable mineral supply, the project Jadar and all similar projects involving waste dumps, landfills, and mine water discharge into surface recipients should be forbidden. To achieve such a goal, it is necessary to assist the local population in targeted countries and to protect them from the harmful alliance of autocratic authorities and big companies.
In order to achieve a fair distribution of benefits and coherent environmental protection in line with EU standards, it is necessary to promote transparent and multilaterally controlled agreements between countries supplying raw materials and countries where minerals are used to manufacture final products. In countries aspiring to join the EU, existing dumps, landfills, and waters must be remediated and recultivated first. Furthermore, all projects with an environmental impact similar to that of the Jadar project should be banned, and all preparations for the construction of new non-European mines for the extraction of critical minerals must be suspended until the state of soil, water and air pollution in the host countries improves and is brought to the levels respected in Austria, Norway, and Luxembourg.
8 Conclusions
The main objective of this article is to use scientifically based considerations to identify the key issues of the title topic, to assess this complex and multidisciplinary subject, and to draw feasible conclusions and recommendations. The manuscript covers heterogeneous aspects, which lead to the following key insights.
Technological development should be directed towards solutions that rely primarily on minerals that are abundant in the lithosphere. Among the priorities in the design of devices and systems, it is necessary to include the possibility of recycling minerals with as little energy consumption as possible. For the purposes of long-term planning, it should be recognized that the value of raw materials, products, and services expressed in money cannot be measured only in money, but it is also necessary to take into account the associated energy consumption. In order to reliably and safely supply developed industrial countries with necessary minerals from the rest of the world, it is necessary to apply technologies, a degree of environmental protection and the share of the local population in the profits in the countries that provide minerals that would have to be applied if the exploitation were carried out in a developed country that uses minerals. According to previous experience and available estimates, deviation from the above recommendations creates significant uncertainty and serious problems.
Acknowledgement
The author dedicates this work to the students and teachers of Serbia who, since November 2024, firmly stand against corruption, partocracy, lawlessness, repression of scientists and teachers, and the intentional destruction of the education system by those in power.
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Funding information: The author thanks Serbian taxpayers for providing the necessary funding for science and education, even if only a small fraction of these funds reaches researchers and educators. This work was supported in part by the Ministry of the Serbian Government in charge of science, under Project TR33022, and in part by the Serbian Academy of Sciences and Arts under Project F143.
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Author contribution: This article is by a single author. All drafting and revisions were carried out by the sole author.
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Conflict of interest: The author has no affiliations with or involvement in any organization or entity with a financial or non-financial interest in the subject matter or materials discussed in this manuscript.
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- Comprehensive analysis of agricultural CEE: Efficiency assessment, mechanism identification, and policy response – A case study of Anhui Province
- Simulation study on the damage and failure mechanism of the surrounding rock in sanded dolomite tunnels
- Towards carbon neutrality: Spatiotemporal evolution and key influences on agricultural ecological efficiency in Northwest China
- High-frequency cycles drive the cyclical enrichment of oil in porous carbonate reservoirs: A case study of the Khasib Formation in E Oilfield, Mesopotamian Basin, Iraq
- Reconstruction of digital core models of granular rocks using mathematical morphology
- Spatial–temporal differentiation law of habitat quality and its driving mechanism in the typical plateau areas of the Loess Plateau in the recent 30 years
- A machine-learning-based approach to predict potential oil sites: Conceptual framework and experimental evaluation
- Effects of landscape pattern change on waterbird diversity in Xianghai Nature Reserve
- Research on intelligent classification method of highway tunnel surrounding rock classification based on parameters while drilling
- River morphology and tectono-sedimentary analysis of a shallow river delta: A case study of Putaohua oil layer in Saertu oilfield (L. Cretaceous), China
- Dynamic change in quarterly FVC of urban parks based on multi-spectral UAV images: A case study of people’s park and harmony park in Xinxiang, China
- Review Articles
- Humic substances influence on the distribution of dissolved iron in seawater: A review of electrochemical methods and other techniques
- Applications of physics-informed neural networks in geosciences: From basic seismology to comprehensive environmental studies
- Ore-controlling structures of granite-related uranium deposits in South China: A review
- Shallow geological structure features in Balikpapan Bay East Kalimantan Province – Indonesia
- A review on the tectonic affinity of microcontinents and evolution of the Proto-Tethys Ocean in Northeastern Tibet
- Advancements in machine learning applications for mineral prospecting and geophysical inversion: A review
- Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part II
- Depopulation in the Visok micro-region: Toward demographic and economic revitalization
- Special Issue: Geospatial and Environmental Dynamics - Part II
- Advancing urban sustainability: Applying GIS technologies to assess SDG indicators – a case study of Podgorica (Montenegro)
- Spatiotemporal and trend analysis of common cancers in men in Central Serbia (1999–2021)
- Minerals for the green agenda, implications, stalemates, and alternatives
- Spatiotemporal water quality analysis of Vrana Lake, Croatia
- Functional transformation of settlements in coal exploitation zones: A case study of the municipality of Stanari in Republic of Srpska (Bosnia and Herzegovina)
- Hypertension in AP Vojvodina (Northern Serbia): A spatio-temporal analysis of patients at the Institute for Cardiovascular Diseases of Vojvodina
- Regional patterns in cause-specific mortality in Montenegro, 1991–2019
- Spatio-temporal analysis of flood events using GIS and remote sensing-based approach in the Ukrina River Basin, Bosnia and Herzegovina
- Flash flood susceptibility mapping using LiDAR-Derived DEM and machine learning algorithms: Ljuboviđa case study, Serbia
- Geocultural heritage as a basis for geotourism development: Banjska Monastery, Zvečan (Serbia)
- Assessment of groundwater potential zones using GIS and AHP techniques – A case study of the zone of influence of Kolubara Mining Basin
- Impact of the agri-geographical transformation of rural settlements on the geospatial dynamics of soil erosion intensity in municipalities of Central Serbia
- Where faith meets geomorphology: The cultural and religious significance of geodiversity explored through geospatial technologies
- Applications of local climate zone classification in European cities: A review of in situ and mobile monitoring methods in urban climate studies
- Complex multivariate water quality impact assessment on Krivaja River
- Ionization hotspots near waterfalls in Eastern Serbia’s Stara Planina Mountain
- Shift in landscape use strategies during the transition from the Bronze age to Iron age in Northwest Serbia
- Assessing the geotourism potential of glacial lakes in Plav, Montenegro: A multi-criteria assessment by using the M-GAM model
- Flash flood potential index at national scale: Susceptibility assessment within catchments
- SWAT modelling and MCDM for spatial valuation in small hydropower planning
- Disaster risk perception and local resilience near the “Duboko” landfill: Challenges of governance, management, trust, and environmental communication in Serbia
Articles in the same Issue
- Research Articles
- Seismic response and damage model analysis of rocky slopes with weak interlayers
- Multi-scenario simulation and eco-environmental effect analysis of “Production–Living–Ecological space” based on PLUS model: A case study of Anyang City
- Remote sensing estimation of chlorophyll content in rape leaves in Weibei dryland region of China
- GIS-based frequency ratio and Shannon entropy modeling for landslide susceptibility mapping: A case study in Kundah Taluk, Nilgiris District, India
- Natural gas origin and accumulation of the Changxing–Feixianguan Formation in the Puguang area, China
- Spatial variations of shear-wave velocity anomaly derived from Love wave ambient noise seismic tomography along Lembang Fault (West Java, Indonesia)
- Evaluation of cumulative rainfall and rainfall event–duration threshold based on triggering and non-triggering rainfalls: Northern Thailand case
- Pixel and region-oriented classification of Sentinel-2 imagery to assess LULC dynamics and their climate impact in Nowshera, Pakistan
- The use of radar-optical remote sensing data and geographic information system–analytical hierarchy process–multicriteria decision analysis techniques for revealing groundwater recharge prospective zones in arid-semi arid lands
- Effect of pore throats on the reservoir quality of tight sandstone: A case study of the Yanchang Formation in the Zhidan area, Ordos Basin
- Hydroelectric simulation of the phreatic water response of mining cracked soil based on microbial solidification
- Spatial-temporal evolution of habitat quality in tropical monsoon climate region based on “pattern–process–quality” – a case study of Cambodia
- Early Permian to Middle Triassic Formation petroleum potentials of Sydney Basin, Australia: A geochemical analysis
- Micro-mechanism analysis of Zhongchuan loess liquefaction disaster induced by Jishishan M6.2 earthquake in 2023
- Prediction method of S-wave velocities in tight sandstone reservoirs – a case study of CO2 geological storage area in Ordos Basin
- Ecological restoration in valley area of semiarid region damaged by shallow buried coal seam mining
- Hydrocarbon-generating characteristics of Xujiahe coal-bearing source rocks in the continuous sedimentary environment of the Southwest Sichuan
- Hazard analysis of future surface displacements on active faults based on the recurrence interval of strong earthquakes
- Structural characterization of the Zalm district, West Saudi Arabia, using aeromagnetic data: An approach for gold mineral exploration
- Research on the variation in the Shields curve of silt initiation
- Reuse of agricultural drainage water and wastewater for crop irrigation in southeastern Algeria
- Assessing the effectiveness of utilizing low-cost inertial measurement unit sensors for producing as-built plans
- Analysis of the formation process of a natural fertilizer in the loess area
- Machine learning methods for landslide mapping studies: A comparative study of SVM and RF algorithms in the Oued Aoulai watershed (Morocco)
- Chemical dissolution and the source of salt efflorescence in weathering of sandstone cultural relics
- Molecular simulation of methane adsorption capacity in transitional shale – a case study of Longtan Formation shale in Southern Sichuan Basin, SW China
- Evolution characteristics of extreme maximum temperature events in Central China and adaptation strategies under different future warming scenarios
- Estimating Bowen ratio in local environment based on satellite imagery
- 3D fusion modeling of multi-scale geological structures based on subdivision-NURBS surfaces and stratigraphic sequence formalization
- Comparative analysis of machine learning algorithms in Google Earth Engine for urban land use dynamics in rapidly urbanizing South Asian cities
- Study on the mechanism of plant root influence on soil properties in expansive soil areas
- Simulation of seismic hazard parameters and earthquakes source mechanisms along the Red Sea rift, western Saudi Arabia
- Tectonics vs sedimentation in foredeep basins: A tale from the Oligo-Miocene Monte Falterona Formation (Northern Apennines, Italy)
- Investigation of landslide areas in Tokat-Almus road between Bakımlı-Almus by the PS-InSAR method (Türkiye)
- Predicting coastal variations in non-storm conditions with machine learning
- Cross-dimensional adaptivity research on a 3D earth observation data cube model
- Geochronology and geochemistry of late Paleozoic volcanic rocks in eastern Inner Mongolia and their geological significance
- Spatial and temporal evolution of land use and habitat quality in arid regions – a case of Northwest China
- Ground-penetrating radar imaging of subsurface karst features controlling water leakage across Wadi Namar dam, south Riyadh, Saudi Arabia
- Rayleigh wave dispersion inversion via modified sine cosine algorithm: Application to Hangzhou, China passive surface wave data
- Fractal insights into permeability control by pore structure in tight sandstone reservoirs, Heshui area, Ordos Basin
- Debris flow hazard characteristic and mitigation in Yusitong Gully, Hengduan Mountainous Region
- Research on community characteristics of vegetation restoration in hilly power engineering based on multi temporal remote sensing technology
- Identification of radial drainage networks based on topographic and geometric features
- Trace elements and melt inclusion in zircon within the Qunji porphyry Cu deposit: Application to the metallogenic potential of the reduced magma-hydrothermal system
- Pore, fracture characteristics and diagenetic evolution of medium-maturity marine shales from the Silurian Longmaxi Formation, NE Sichuan Basin, China
- Study of the earthquakes source parameters, site response, and path attenuation using P and S-waves spectral inversion, Aswan region, south Egypt
- Source of contamination and assessment of potential health risks of potentially toxic metal(loid)s in agricultural soil from Al Lith, Saudi Arabia
- Regional spatiotemporal evolution and influencing factors of rural construction areas in the Nanxi River Basin via GIS
- An efficient network for object detection in scale-imbalanced remote sensing images
- Effect of microscopic pore–throat structure heterogeneity on waterflooding seepage characteristics of tight sandstone reservoirs
- Environmental health risk assessment of Zn, Cd, Pb, Fe, and Co in coastal sediments of the southeastern Gulf of Aqaba
- A modified Hoek–Brown model considering softening effects and its applications
- Evaluation of engineering properties of soil for sustainable urban development
- The spatio-temporal characteristics and influencing factors of sustainable development in China’s provincial areas
- Application of a mixed additive and multiplicative random error model to generate DTM products from LiDAR data
- Gold vein mineralogy and oxygen isotopes of Wadi Abu Khusheiba, Jordan
- Prediction of surface deformation time series in closed mines based on LSTM and optimization algorithms
- 2D–3D Geological features collaborative identification of surrounding rock structural planes in hydraulic adit based on OC-AINet
- Spatiotemporal patterns and drivers of Chl-a in Chinese lakes between 1986 and 2023
- Land use classification through fusion of remote sensing images and multi-source data
- Nexus between renewable energy, technological innovation, and carbon dioxide emissions in Saudi Arabia
- Analysis of the spillover effects of green organic transformation on sustainable development in ethnic regions’ agriculture and animal husbandry
- Factors impacting spatial distribution of black and odorous water bodies in Hebei
- Large-scale shaking table tests on the liquefaction and deformation responses of an ultra-deep overburden
- Impacts of climate change and sea-level rise on the coastal geological environment of Quang Nam province, Vietnam
- Reservoir characterization and exploration potential of shale reservoir near denudation area: A case study of Ordovician–Silurian marine shale, China
- Seismic prediction of Permian volcanic rock reservoirs in Southwest Sichuan Basin
- Application of CBERS-04 IRS data to land surface temperature inversion: A case study based on Minqin arid area
- Geological characteristics and prospecting direction of Sanjiaoding gold mine in Saishiteng area
- Research on the deformation prediction model of surrounding rock based on SSA-VMD-GRU
- Geochronology, geochemical characteristics, and tectonic significance of the granites, Menghewula, Southern Great Xing’an range
- Hazard classification of active faults in Yunnan base on probabilistic seismic hazard assessment
- Characteristics analysis of hydrate reservoirs with different geological structures developed by vertical well depressurization
- Estimating the travel distance of channelized rock avalanches using genetic programming method
- Landscape preferences of hikers in Three Parallel Rivers Region and its adjacent regions by content analysis of user-generated photography
- New age constraints of the LGM onset in the Bohemian Forest – Central Europe
- Characteristics of geological evolution based on the multifractal singularity theory: A case study of Heyu granite and Mesozoic tectonics
- Soil water content and longitudinal microbiota distribution in disturbed areas of tower foundations of power transmission and transformation projects
- Oil accumulation process of the Kongdian reservoir in the deep subsag zone of the Cangdong Sag, Bohai Bay Basin, China
- Investigation of velocity profile in rock–ice avalanche by particle image velocimetry measurement
- Optimizing 3D seismic survey geometries using ray tracing and illumination modeling: A case study from Penobscot field
- Sedimentology of the Phra That and Pha Daeng Formations: A preliminary evaluation of geological CO2 storage potential in the Lampang Basin, Thailand
- Improved classification algorithm for hyperspectral remote sensing images based on the hybrid spectral network model
- Map analysis of soil erodibility rates and gully erosion sites in Anambra State, South Eastern Nigeria
- Identification and driving mechanism of land use conflict in China’s South-North transition zone: A case study of Huaihe River Basin
- Evaluation of the impact of land-use change on earthquake risk distribution in different periods: An empirical analysis from Sichuan Province
- A test site case study on the long-term behavior of geotextile tubes
- An experimental investigation into carbon dioxide flooding and rock dissolution in low-permeability reservoirs of the South China Sea
- Detection and semi-quantitative analysis of naphthenic acids in coal and gangue from mining areas in China
- Comparative effects of olivine and sand on KOH-treated clayey soil
- YOLO-MC: An algorithm for early forest fire recognition based on drone image
- Earthquake building damage classification based on full suite of Sentinel-1 features
- Potential landslide detection and influencing factors analysis in the upper Yellow River based on SBAS-InSAR technology
- Assessing green area changes in Najran City, Saudi Arabia (2013–2022) using hybrid deep learning techniques
- An advanced approach integrating methods to estimate hydraulic conductivity of different soil types supported by a machine learning model
- Hybrid methods for land use and land cover classification using remote sensing and combined spectral feature extraction: A case study of Najran City, KSA
- Streamlining digital elevation model construction from historical aerial photographs: The impact of reference elevation data on spatial accuracy
- Analysis of urban expansion patterns in the Yangtze River Delta based on the fusion impervious surfaces dataset
- A metaverse-based visual analysis approach for 3D reservoir models
- Late Quaternary record of 100 ka depositional cycles on the Larache shelf (NW Morocco)
- Integrated well-seismic analysis of sedimentary facies distribution: A case study from the Mesoproterozoic, Ordos Basin, China
- Study on the spatial equilibrium of cultural and tourism resources in Macao, China
- Urban road surface condition detecting and integrating based on the mobile sensing framework with multi-modal sensors
- Application of improved sine cosine algorithm with chaotic mapping and novel updating methods for joint inversion of resistivity and surface wave data
- The synergistic use of AHP and GIS to assess factors driving forest fire potential in a peat swamp forest in Thailand
- Dynamic response analysis and comprehensive evaluation of cement-improved aeolian sand roadbed
- Rock control on evolution of Khorat Cuesta, Khorat UNESCO Geopark, Northeastern Thailand
- Gradient response mechanism of carbon storage: Spatiotemporal analysis of economic-ecological dimensions based on hybrid machine learning
- Comparison of several seismic active earth pressure calculation methods for retaining structures
- Mantle dynamics and petrogenesis of Gomer basalts in the Northwestern Ethiopia: A geochemical perspective
- Study on ground deformation monitoring in Xiong’an New Area from 2021 to 2023 based on DS-InSAR
- Paleoenvironmental characteristics of continental shale and its significance to organic matter enrichment: Taking the fifth member of Xujiahe Formation in Tianfu area of Sichuan Basin as an example
- Equipping the integral approach with generalized least squares to reconstruct relict channel profile and its usage in the Shanxi Rift, northern China
- InSAR-driven landslide hazard assessment along highways in hilly regions: A case-based validation approach
- Attribution analysis of multi-temporal scale surface streamflow changes in the Ganjiang River based on a multi-temporal Budyko framework
- Maps analysis of Najran City, Saudi Arabia to enhance agricultural development using hybrid system of ANN and multi-CNN models
- Hybrid deep learning with a random forest system for sustainable agricultural land cover classification using DEM in Najran, Saudi Arabia
- Long-term evolution patterns of groundwater depth and lagged response to precipitation in a complex aquifer system: Insights from Huaibei Region, China
- Remote sensing and machine learning for lithology and mineral detection in NW, Pakistan
- Spatial–temporal variations of NO2 pollution in Shandong Province based on Sentinel-5P satellite data and influencing factors
- Numerical modeling of geothermal energy piles with sensitivity and parameter variation analysis of a case study
- Stability analysis of valley-type upstream tailings dams using a 3D model
- Variation characteristics and attribution analysis of actual evaporation at monthly time scale from 1982 to 2019 in Jialing River Basin, China
- Investigating machine learning and statistical approaches for landslide susceptibility mapping in Minfeng County, Xinjiang
- Investigating spatiotemporal patterns for comprehensive accessibility of service facilities by location-based service data in Nanjing (2016–2022)
- A pre-treatment method for particle size analysis of fine-grained sedimentary rocks, Bohai Bay Basin, China
- Study on the formation mechanism of the hard-shell layer of liquefied silty soil
- Comprehensive analysis of agricultural CEE: Efficiency assessment, mechanism identification, and policy response – A case study of Anhui Province
- Simulation study on the damage and failure mechanism of the surrounding rock in sanded dolomite tunnels
- Towards carbon neutrality: Spatiotemporal evolution and key influences on agricultural ecological efficiency in Northwest China
- High-frequency cycles drive the cyclical enrichment of oil in porous carbonate reservoirs: A case study of the Khasib Formation in E Oilfield, Mesopotamian Basin, Iraq
- Reconstruction of digital core models of granular rocks using mathematical morphology
- Spatial–temporal differentiation law of habitat quality and its driving mechanism in the typical plateau areas of the Loess Plateau in the recent 30 years
- A machine-learning-based approach to predict potential oil sites: Conceptual framework and experimental evaluation
- Effects of landscape pattern change on waterbird diversity in Xianghai Nature Reserve
- Research on intelligent classification method of highway tunnel surrounding rock classification based on parameters while drilling
- River morphology and tectono-sedimentary analysis of a shallow river delta: A case study of Putaohua oil layer in Saertu oilfield (L. Cretaceous), China
- Dynamic change in quarterly FVC of urban parks based on multi-spectral UAV images: A case study of people’s park and harmony park in Xinxiang, China
- Review Articles
- Humic substances influence on the distribution of dissolved iron in seawater: A review of electrochemical methods and other techniques
- Applications of physics-informed neural networks in geosciences: From basic seismology to comprehensive environmental studies
- Ore-controlling structures of granite-related uranium deposits in South China: A review
- Shallow geological structure features in Balikpapan Bay East Kalimantan Province – Indonesia
- A review on the tectonic affinity of microcontinents and evolution of the Proto-Tethys Ocean in Northeastern Tibet
- Advancements in machine learning applications for mineral prospecting and geophysical inversion: A review
- Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part II
- Depopulation in the Visok micro-region: Toward demographic and economic revitalization
- Special Issue: Geospatial and Environmental Dynamics - Part II
- Advancing urban sustainability: Applying GIS technologies to assess SDG indicators – a case study of Podgorica (Montenegro)
- Spatiotemporal and trend analysis of common cancers in men in Central Serbia (1999–2021)
- Minerals for the green agenda, implications, stalemates, and alternatives
- Spatiotemporal water quality analysis of Vrana Lake, Croatia
- Functional transformation of settlements in coal exploitation zones: A case study of the municipality of Stanari in Republic of Srpska (Bosnia and Herzegovina)
- Hypertension in AP Vojvodina (Northern Serbia): A spatio-temporal analysis of patients at the Institute for Cardiovascular Diseases of Vojvodina
- Regional patterns in cause-specific mortality in Montenegro, 1991–2019
- Spatio-temporal analysis of flood events using GIS and remote sensing-based approach in the Ukrina River Basin, Bosnia and Herzegovina
- Flash flood susceptibility mapping using LiDAR-Derived DEM and machine learning algorithms: Ljuboviđa case study, Serbia
- Geocultural heritage as a basis for geotourism development: Banjska Monastery, Zvečan (Serbia)
- Assessment of groundwater potential zones using GIS and AHP techniques – A case study of the zone of influence of Kolubara Mining Basin
- Impact of the agri-geographical transformation of rural settlements on the geospatial dynamics of soil erosion intensity in municipalities of Central Serbia
- Where faith meets geomorphology: The cultural and religious significance of geodiversity explored through geospatial technologies
- Applications of local climate zone classification in European cities: A review of in situ and mobile monitoring methods in urban climate studies
- Complex multivariate water quality impact assessment on Krivaja River
- Ionization hotspots near waterfalls in Eastern Serbia’s Stara Planina Mountain
- Shift in landscape use strategies during the transition from the Bronze age to Iron age in Northwest Serbia
- Assessing the geotourism potential of glacial lakes in Plav, Montenegro: A multi-criteria assessment by using the M-GAM model
- Flash flood potential index at national scale: Susceptibility assessment within catchments
- SWAT modelling and MCDM for spatial valuation in small hydropower planning
- Disaster risk perception and local resilience near the “Duboko” landfill: Challenges of governance, management, trust, and environmental communication in Serbia