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Research on pore structures of fine-grained carbonate reservoirs and their influence on waterflood development

  • Chichen Yang EMAIL logo and Hongming Tang EMAIL logo
Published/Copyright: May 24, 2023
Become an author with De Gruyter Brill

Abstract

Carbonate reservoir has complex pore structures. At present, the influence of pore structure on water flooding mechanism of carbonate reservoirs is insufficient. In this article, a systematic workflow was designed in combination with scanning electron microscope, particle size, physical properties, and water flooding experiments to study the effect of pore structure on water flooding mechanism of fine-grained carbonate rocks. Due to the small particle size and strong heterogeneity, the acid fracturing operations, rather than hydraulic fracturing alone, are necessary to achieve increased production and reservoir reconstruction of carbonate reservoirs. Through this study, the mathematical model of reservoir physical parameters (permeability and porosity) was proposed, and the accuracy of the model was verified by comparing the simulated oil recovery with the experimental results. According to the comparison results, the experimental results are consistent with the simulation results, and their oil recovery efficiency is 33.62 and 31.87%, respectively. Finally, the effect of injection rate on oil production was discussed. It is shown that with the increase in injection rate, the output of displaced oil increases significantly. The cumulative oil production increases from 62.5 to 256.31 mL when the injection rate increases from 100 to 400 mL/min. The findings of this study can help for better understanding of the influencing factors and mechanisms of the development efficiency of carbonate reservoirs.

1 Introduction

With the rapid development of the global economy, the energy crisis has become increasingly prominent. However, at present, new energy such as solar energy cannot completely replace fossil fuels [1,2,3]. Development and utilization of conventional fossil fuels are still the focus of future energy-related investigations [4]. Conventional oil and gas resources are often in a state of continuous production reduction after long-term of production cycle [5,6]. Therefore, the exploration and development of unconventional oil and gas resources are of great significance in maintaining the security of global energy [7,8]. Among them, carbonate reservoirs are important unconventional resources, whose estimated resource reserves are 1.6 × 1012 tons [9]. Therefore, effective development of oil and gas resources from carbonate reservoirs can help ease the tense situation of global energy.

Nevertheless, the bedrock minerals of carbonate rocks are extremely vulnerable to corrosion and become carbonate solutions, resulting in complex pore structures that differ from other reservoirs [10]. It is dominated by short and wide pores, and there may be small karst caves [11,12,13]. Figure 1 shows a comparison of the pore structures of carbonate and sandstone reservoirs [14]. As observed in Figure 1a, distribution of pores within carbonate reservoir is discrete, and the existence of some microfissures communicates different pore clusters. However, the pores in sandstone distribute uniformly (Figure 1b). [15] Therefore, the heterogeneity of pore structure in carbonate reservoir is stronger than that of sandstone. Therefore, it is very necessary to simulate the process of water flooding in carbonate reservoirs.

Figure 1 
               Schematic diagram of the pore structure of carbonate (a) and sandstone (b) reservoirs (modified after ref. [14]); (c) difference in fluid flow in carbonate and sandstone reservoirs.
Figure 1

Schematic diagram of the pore structure of carbonate (a) and sandstone (b) reservoirs (modified after ref. [14]); (c) difference in fluid flow in carbonate and sandstone reservoirs.

At present, some researchers have carried out relevant studies on the pore structures of carbonate reservoir, and some progress has been made. Li et al. [16] systematically studied the characteristics of pore structures in four types of carbonate reservoirs, and the main influencing factors of difference in pore structures were also investigated. It was found that the random distribution of various pores is an important factor affecting the pore structures of reservoirs. He et al. [17] studied the relationship between permeability and porosity in carbonate reservoirs. It was found that high permeability of the reservoir is related to the development of microfractures and caves. Wang and Fan [18] evaluated the variation characteristics of porosity and permeability of carbonate reservoirs caused by diagenesis. Rezaee et al. [19] established the relationship between permeability, porosity, and pore size through an artificial neural network approach. This study indirectly proved that the artificial neural network is effective in predicting the permeability of carbonate reservoirs.

Undoubtedly, these studies are of significance for the efficient development of oil and gas resources in carbonate reservoirs. Nevertheless, there are still two defects that exist in these investigations. First of all, most of the research studies on pore structures of carbonate reservoirs are qualitative studies, and it is difficult to establish relationships with development indexes. There are few research studies on water flooding mechanism based on a systematic workflow construction and microperspective. Second, there are few reports about the effect of pore structures of carbonate rocks on oil and gas production behavior. In this study, a systematic experimental workflow was established to characterize the microscopic pore structures (including mathematical modeling) of carbonate reservoirs and their effect on productivity. This study can facilitate subsequent productivity calculation and reservoir simulation of carbonate reservoirs.

In this study, the pore structures of carbonate reservoirs were analyzed by macroscopic and microscopic experiments. The effect of water injection operation on oil and gas development was explored through oil displacement experiments. At the same time, the effect of injection rate on oil production was also investigated. This work can provide reference for the efficient extraction and production of oil and gas resources in carbonate reservoirs.

The workflow of the investigation is shown in Figure 2. In Section 2, both the self-developed experimental system and experimental method were introduced. In Section 3, the rock properties were investigated, and modeling of porosity and permeability was carried out. Furthermore, the applicability of the proposed model was verified by the oil displacement experiments, and the influence of injection rate on oil displacement effect was analyzed.

Figure 2 
               Workflow of the study.
Figure 2

Workflow of the study.

2 Experiments and methods

The particle size distribution of mineral particles was analyzed using a BT-9300ST laser particle size analyzer (purchased from Dandong Baxter Instruments Co.). This particle size analyzer can accurately measure the size of particle in the range of 0.1–1,000 μm. Moreover, the accuracy of the particle size analyzer is 1%, which can fully meet the requirements of particle size distribution measurement of most minerals.

In addition, the experiment system for simultaneous measurement of porosity and permeability was performed as shown in Figure 3.

Figure 3 
               (a) Experimental equipment for simultaneous measurement of porosity and permeability of rock samples and (b) diagram of the applied stress states.
Figure 3

(a) Experimental equipment for simultaneous measurement of porosity and permeability of rock samples and (b) diagram of the applied stress states.

Step-by-step measurements of porosity and permeability can lead to the deviation in experimental results. This is because the permeability and porosity measurement process will pose a threat to the integrity of the pore structures of rock samples. For this reason, the permeability and porosity should be measured simultaneously by placing the rock samples directly into the autoclave. The porosity and permeability were measured with the gas method to avoid pollution caused by the mercury-pressure method [20]. During the experiment, the airtightness of the device needs to be tested first. Then, the samples were placed into the autoclave and sealed with a rubber sleeve. At the same time, the porosity and permeability measurement system was activated, and the nitrogen was filled into the experiment system. The permeability and porosity can be measured simultaneously. Notably, the measurement accuracy of porosity and permeability is as high as 0.25% and 0.20 mD, respectively.

The principle of this experimental system for porosity measurement can be expressed as follows:

(1) φ = V p V t × 100 % ,

where φ is the porosity, %; V p is the pore volume of rock sample, m3; V t is the total apparent volume of rock sample, m3.

Similarly, the gas percolation during the measurement of permeability follows Darcy’s law exactly, and the Klinkenberg effect is neglected. Darcy’s law, which is the principle of the experimental system for permeability measurement, can be expressed as:

(2) Q = KA Δ P l ,

where Q is the infiltration rate per unit time; K is the permeability, mD; A is the effective cross-sectional area of rock sample, m2; ΔP is the pressure difference, MPa; l is the length of the rock sample, m.

3 Results

3.1 Experimental materials and mineral fractions

The six samples used in the experiments were taken from the AH-1 well in the AH Oil Field, and the sampling depth interval was between 1,325 and 1,342 m. Notably, particle size analysis of mineral grains needs to be performed after the simultaneous permeability and porosity measurement experiments. This is because particle size analysis will destroy the physical structure of the rock samples. Meanwhile, the nitrogen gas (99.9% purity) used in the experiments was purchased from Qingdao Southwest Drainage Gas Co. The physical characteristics of the six samples are shown in Table 1.

Table 1

Rock sample characteristics and results of mineral analysis

No. Diameter (mm) Density (g/cm3) Height (mm) Mineral composition (%)
Quartz Potassium feldspar Plagioclase Calcite Dolomite Clay
1 48.84 2.54 98.37 39 10 7 25 2 14
2 49.16 2.58 100.39 36 14 6 24 2 16
3 50.12 2.61 101.62 25 2 5 48 2 14
4 49.29 2.55 99.68 32 23 4 27 4 7
5 50.67 2.60 101.03 47 26 4 11 1 7
6 50.32 2.59 98.92 34 20 5 31 8

In addition, the experimental results of mineral analysis are given in Table 1. Only the percent contents of the main mineral components are given in Table 1. From Table 1, it is found that quartz, calcite, and potassium feldspar make up the major part of the mineral composition of the six rock samples. The proportion of the above three minerals is distributed between 70 and 90%. Plagioclase, dolomite, and clay are less in the six rock samples. The content of these three minerals only accounts for about 10% of the total mineral composition. It can be inferred from the experimental results that the cementation of the carbonate reservoir is achieved by the compaction of the surrounding rocks.

3.2 Characterization of particle size distribution and pore structure

Fine characterization of rock pore structure is a prerequisite for studying reservoir seepage mechanism [21,22,23]. The D50 and D90 data of the particle size distribution of the six rock samples are given in Table 2. From Table 2, we can find that the median particle sizes are between 30 and 50 μm, and the mineral particle is extremely fine. This is mainly due to the serious compaction of this layer during its geological formation process. Moreover, there were no violent plate tectonic movement and metamorphism in this process, and the mineral grains did not recrystallize [24]. The D90 of the six rock samples is mostly between 80 and 100 μm, which is also at a fine level.

Table 2

Results of particle size analysis

No. D50 (μm) D90 (μm) Porosity (%) Permeability (mD)
1 49.94 98.59 13.2 8.56
2 34.55 87.75 12.6 7.98
3 33.83 84.65 11.1 7.52
4 34.91 95.57 12.8 8.84
5 34.88 88.84 16.3 10.61
6 33.11 91.70 15.2 10.39

Notes: D50: Particle size when the cumulative particle size distribution percentage reaches 50%. D90: Particle size when the cumulative particle size distribution percentage reaches 90%.

Finer carbonate mineral grains are not conducive to the formation of pores with high hydraulic conductivity, resulting in the poor property of carbonate reservoirs. The scanning electron microscope images of rock samples No. 3 and No. 5 are shown in Figure 4. From Figure 4(a), it can be found that the poor physical properties of rock sample No. 3 can be attributed to the fact that the pores are filled with dense cements. The porosity of the rock sample No. 3 is only 11.1%, which is the worst among the six rock samples. As a comparison, the clay content of the rock sample No. 5 in Figure 4(b) is only 7%, while the quartz content reaches 47%. The weak cement filling leads to the development of pores in this rock sample, which can be used as the seepage channel and storage space for oil and gas [25].

Figure 4 
                  Microscopic pore structures of rock samples No. 3 (a) and No. 5 (b).
Figure 4

Microscopic pore structures of rock samples No. 3 (a) and No. 5 (b).

In a word, stimulation measures such as hydraulic fracturing are still required for the efficient development of carbonate reservoirs. To be precise, acid-fracturing technology is more suitable for reservoir stimulation of carbonate reservoirs [13].

3.3 Physical parameter modeling

It is of engineering significance to propose a mathematical model of the porosity and permeability of rock samples obtained from carbonate reservoirs. Based on the experimental results, the porosity of carbonate reservoir can be fitted as:

(3) φ ( C Q , C c ) = φ 0 ( 1 C Q ) ( a exp ( b C c ) ) ,

where φ 0 is the porosity in reservoir conditions, %. C Q and C c are the quartz and clay content in rock samples, respectively, %. a and b are the fitting constants, which are 0.324 and 2.631, respectively.

Similarly, rock permeability can be expressed as:

(4) k ( C Q , C c ) = c φ 2 + d φ + e ,

where c, d, and e are all the fitting coefficients (c is 0.023, d is 0.387, and e is 1.075). From equation (4), we can find that permeability can be expressed as a function of porosity. In this way, it was indirectly expressed as a function of the clay and quartz contents. The models shown in equations (3) and (4) can be used in the productivity analysis of carbonate reservoirs.

4 Discussion

Water injection and oil displacement experiments for carbonate reservoirs were carried out to verify the accuracy of the aforementioned fitted models (equations (3) and (4)). At the same time, the effect of injection rate on oil and gas production in carbonate reservoirs was explored in this section.

4.1 Experimental system for water injection and repulsion

As shown in Figure 5, the experimental system used for oil displacement in carbonate reservoirs mainly consists of a core holder, an air compressor, a water injection system, and a waste water treatment system. Among them, the core holder is a cylinder made of 316 L stainless steel, whose wall thickness is 5.0 mm. The core holder can withstand pressure up to 100 MPa, which fully meets the experimental requirements herein. In addition, the role of the air compressor is to restore the subsurface environment in reservoir. The air compressor can achieve a maximum confining pressure of 30 MPa on the sample with an accuracy of 0.10 MPa. The water injection system is realized by an advection pump, and the injection medium is clear water with a certain amount of surface activator added. Notably, the surface activator used in the experiment is sodium dodecyl sulfate (SDS). The advection pump is capable of injecting the displacing fluid at a constant flow rate of up to 2 L/min with an adjustment accuracy of 10 mL/min. The waste water treatment system consists of a beaker and an oil–water separator. Among them, the beaker is used to receive the waste displacing fluid in experiment. However, the oil–water separator is a hydrocyclone used in the separation of oil–water mixture.

Figure 5 
                  Experimental system of carbonate injection and replacement.
Figure 5

Experimental system of carbonate injection and replacement.

The natural carbonate cores are first prepared as the standard samples (50 mm in diameter and 100 mm in height). Then, the core samples are placed in a core holder and loaded with surrounding pressure. At the same time, water with a certain concentration of surface activator is injected into the system. Finally, the waste displacement fluid is collected, and oil–water separation is performed for production (capacity) calculation. It should be noted that the injection rate is 200 mL/min, and the SDS concentration in the displacement fluid is 50 ppm. These are only the default data, and they should be adjusted when sensitivity analysis is performed.

4.2 Displacement effect of water injection and productivity

Figure 6 displays the evolution curves of oil production and oil–water ratio in the experiments. As observed in Figure 6, the oil production gradually increases as the displacement experiment continues. However, the production rate of oil is gradually decreasing. The oil production in the first 12 h was 75.25 mL. However, it was only about 20 mL in the last 12 h, which was about one-fourth of the oil production in the first 12 h. This is mainly due to the fact that the oil saturation in the core decreases as the experiment continues [12,26,27]. Moreover, the oil displaced by water at the beginning of the experiment was in well-flowing pores and throats, and it was easily displaced. However, as the experiment continues, the oil and gas in the core gradually become some crude oil sealed in pores with poor conductivity. It can also be seen in Figure 6 that the oil–water ratio decreases as the experiment continues. This indicates that the proportion of crude oil in produced mixture is gradually decreasing during the experiment, while this proportion of water is gradually increasing. At the beginning of the experiment, the ratio between oil and water was as high as 17.9, indicating that the majority of the produced fluid was crude oil. However, as the experiment continues, oil saturation in pore space within the reservoir gradually decreases. The Klinkenberg effect appears, and the fingering phenomenon becomes prominent. By the end of the experiment, the ratio between oil and water in the produced fluid was only 4.81, which was 26.87% of that at the beginning of the experiment.

Figure 6 
                  Evolution curves of oil production and oil–water ratio during water injection and replacement experiments.
Figure 6

Evolution curves of oil production and oil–water ratio during water injection and replacement experiments.

Another purpose of this experiment is to verify the applicability and accuracy of the porosity and permeability models proposed herein (see equations (3) and (4)). The recovery value of crude oil was then obtained from the productivity simulation by taking equations (3) and (4) into account. The comparison with the experimental results (oil recovery) is shown in Table 3. Notably, all simulation conditions are all same with the experimental results.

Table 3

Comparison of simulation and experimental results

Category Time (h)
4.0 8.0 12.0 24.0
Simulation 12.23 22.31 30.22 33.62
Experiment 11.34 21.08 29.11 31.87

We can see from Table 3 that although the oil recovery obtained from the simulations at any moment is all slightly higher than that of the experiments, the difference is small. All these results indicate that the influence of mineral composition on pore structures should be considered when the productivity for carbonate reservoir was calculated. As a comparison, the productivity of carbonate reservoirs was also analyzed without considering the influence of mineral composition on pore structures. It was found that the final crude oil recovery was only about 27%, which was much lower than the experimental results. The comparison results shown in Table 3 indicate that the influence of mineral composition on pore structures needs to be considered when the productivity of carbonate reservoir was calculated.

4.3 Influence of injection flow rate on capacity

Based on the proposed pore structure (i.e. porosity and permeability) model, an analysis was conducted for the effect of injection rate on the productivity calculation of carbonate reservoirs. The results are shown in Figure 7. In this section, the injection rate was assumed as 100, 200, 300, and 400 mL/min, respectively. As observed in Figure 6, both the cumulative oil production and production rate increase significantly with the increasing injection rate. The cumulative oil production is only 62.71 mL when the injection flow rate is 100 mL/min. However, the final cumulative oil production increased to 75.25, 136.96, and 256.31 mL when the injection rate was 200, 300, and 400 mL/min, respectively. Therefore, it can be concluded that the oil recovery of water flooding in carbonate reservoir can be improved by properly increasing the injection rate.

Figure 7 
                  Histogram of productivity analysis when injection rate is different.
Figure 7

Histogram of productivity analysis when injection rate is different.

However, it is not always possible to achieve a better displacement effect by simply increasing the injection rate. The schematic diagram of oil washing effect in porous media when injection rate is different is displayed in Figure 8. From Figure 8(a), we can see that the crude oil droplets in pores between the sediment particles are less impacted by the injected water when the injection rate is small. The oil droplets cannot be effectively stripped from the surface of the matrix particles. In this case, the recovery of crude oil is certainly lower and the cumulative crude oil production is not high. However, when the injection rate is high, the drag force of injected water on crude oil is extremely strong. In this case, the crude oil in the pores of porous media will be effectively flushed, which is manifested as higher crude oil production and recovery. Of course, the fingering effect will gradually appear and be strengthened with the increase in injection rate, and it will result in a poor oil displacement [28]. Therefore, there must be a limit injection rate value, which maximizes the water flooding efficiency. For this purpose, we expanded the injection rate to three groups: 500, 600, and 700 mL/min. Furthermore, it was found that when the water injection rate reached 400 mL/min under experimental conditions, the oil displacement effect reached the limit value.

Figure 8 
                  Schematic diagram of oil washing effect under different water injection rates: (a) low water injection rate and (b) high water injection rate.
Figure 8

Schematic diagram of oil washing effect under different water injection rates: (a) low water injection rate and (b) high water injection rate.

Through this study, the mathematical models of permeability and porosity are constructed on the basis of quantitative analysis. Moreover, a systematic experimental system of oil displacement in carbonate reservoirs associated with development dynamics has been established. However, this study also has some disadvantages: (1) The core represents a one-dimensional condition, which cannot restore the true reservoir state (3D), and (2) the factors affecting the water flooding effect of carbonate reservoir are complex, but due to the limitation of experimental conditions, the factors have not been fully considered. These shortcomings also need to be improved in the follow-up study.

5 Summary and conclusions

The main conclusions in this work are as follows:

  1. In this study, the main mineral components in the carbonate samples are quartz, calcite, and potassium feldspar, the total content of which is more than 70%. However, the proportion of clay minerals is about 10%. The strong cementation of the carbonate reservoirs is related to the strong compaction of the surrounding rocks. Carbonate reservoir has poor percolation characteristics, and acidizing fracturing is an effective reservoir reconstruction measure to effectively extract oil and gas from carbonate reservoir.

  2. Through this study, a model of reservoir physical parameters (permeability and porosity) was proposed, and the accuracy of the model was verified by comparing the simulated oil recovery with the experimental results. According to the comparison results, the experimental results are consistent with the simulation results, and the oil recovery efficiency is 33.62 and 31.87%, respectively.

  3. The effect of injection rate on oil production was discussed. It is shown that with the increase in injection rate, the output of displaced oil increases significantly. The cumulative oil production increases from 62.5 to 256.31 mL when the injection rate increases from 100 to 400 mL/min.

In order to provide further support for efficient oil recovery in carbonate reservoirs, further studies will need to be carried out, such as the influence of other factors, such as displacement fluid properties, on oil displacement.

Nomenclature

SDS

sodium dodecyl sulfate

P z

axial pressure

P c

confining pressure

P p

pore pressure

φ

porosity

V p

pore volume of rock sample

V t

total apparent volume of rock sample

Q

infiltration rate per unit time

K

permeability

A

effective cross-sectional area of rock sample

P

pressure

ΔP

pressure difference

l

length of the rock sample

D50

particle size when the cumulative particle size distribution percentage reaches 50%

D90

particle size when the cumulative particle size distribution percentage reaches 90%

φ 0

porosity in reservoir conditions

C Q

quartz content

C C

clay content

ae

constants

Acknowledgement

This study was supported by the National Major Oil and Gas Projects of China “Key technologies for the development of large carbonate reservoirs in the Silk Road Economic Belt” (Item No.: 2017ZX05030).

  1. Conflict of interest: This study was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

  2. Data availability statement: The data that support the findings of this study are available from the corresponding author upon a reasonable request.

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Received: 2023-02-11
Revised: 2023-03-27
Accepted: 2023-03-30
Published Online: 2023-05-24

© 2023 the author(s), published by De Gruyter

This work is licensed under the Creative Commons Attribution 4.0 International License.

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  17. Reconstruction of paleoglacial equilibrium-line altitudes during the Last Glacial Maximum in the Diancang Massif, Northwest Yunnan Province, China
  18. A prediction model for Xiangyang Neolithic sites based on a random forest algorithm
  19. Determining the long-term impact area of coastal thermal discharge based on a harmonic model of sea surface temperature
  20. Origin of block accumulations based on the near-surface geophysics
  21. Investigating the limestone quarries as geoheritage sites: Case of Mardin ancient quarry
  22. Population genetics and pedigree geography of Trionychia japonica in the four mountains of Henan Province and the Taihang Mountains
  23. Performance audit evaluation of marine development projects based on SPA and BP neural network model
  24. Study on the Early Cretaceous fluvial-desert sedimentary paleogeography in the Northwest of Ordos Basin
  25. Detecting window line using an improved stacked hourglass network based on new real-world building façade dataset
  26. Automated identification and mapping of geological folds in cross sections
  27. Silicate and carbonate mixed shelf formation and its controlling factors, a case study from the Cambrian Canglangpu formation in Sichuan basin, China
  28. Ground penetrating radar and magnetic gradient distribution approach for subsurface investigation of solution pipes in post-glacial settings
  29. Research on pore structures of fine-grained carbonate reservoirs and their influence on waterflood development
  30. Risk assessment of rain-induced debris flow in the lower reaches of Yajiang River based on GIS and CF coupling models
  31. Multifractal analysis of temporal and spatial characteristics of earthquakes in Eurasian seismic belt
  32. Surface deformation and damage of 2022 (M 6.8) Luding earthquake in China and its tectonic implications
  33. Differential analysis of landscape patterns of land cover products in tropical marine climate zones – A case study in Malaysia
  34. DEM-based analysis of tectonic geomorphologic characteristics and tectonic activity intensity of the Dabanghe River Basin in South China Karst
  35. Distribution, pollution levels, and health risk assessment of heavy metals in groundwater in the main pepper production area of China
  36. Study on soil quality effect of reconstructing by Pisha sandstone and sand soil
  37. Understanding the characteristics of loess strata and quaternary climate changes in Luochuan, Shaanxi Province, China, through core analysis
  38. Dynamic variation of groundwater level and its influencing factors in typical oasis irrigated areas in Northwest China
  39. Creating digital maps for geotechnical characteristics of soil based on GIS technology and remote sensing
  40. Changes in the course of constant loading consolidation in soil with modeled granulometric composition contaminated with petroleum substances
  41. Correlation between the deformation of mineral crystal structures and fault activity: A case study of the Yingxiu-Beichuan fault and the Milin fault
  42. Cognitive characteristics of the Qiang religious culture and its influencing factors in Southwest China
  43. Spatiotemporal variation characteristics analysis of infrastructure iron stock in China based on nighttime light data
  44. Interpretation of aeromagnetic and remote sensing data of Auchi and Idah sheets of the Benin-arm Anambra basin: Implication of mineral resources
  45. Building element recognition with MTL-AINet considering view perspectives
  46. Characteristics of the present crustal deformation in the Tibetan Plateau and its relationship with strong earthquakes
  47. Influence of fractures in tight sandstone oil reservoir on hydrocarbon accumulation: A case study of Yanchang Formation in southeastern Ordos Basin
  48. Nutrient assessment and land reclamation in the Loess hills and Gulch region in the context of gully control
  49. Handling imbalanced data in supervised machine learning for lithological mapping using remote sensing and airborne geophysical data
  50. Spatial variation of soil nutrients and evaluation of cultivated land quality based on field scale
  51. Lignin analysis of sediments from around 2,000 to 1,000 years ago (Jiulong River estuary, southeast China)
  52. Assessing OpenStreetMap roads fitness-for-use for disaster risk assessment in developing countries: The case of Burundi
  53. Transforming text into knowledge graph: Extracting and structuring information from spatial development plans
  54. A symmetrical exponential model of soil temperature in temperate steppe regions of China
  55. A landslide susceptibility assessment method based on auto-encoder improved deep belief network
  56. Numerical simulation analysis of ecological monitoring of small reservoir dam based on maximum entropy algorithm
  57. Morphometry of the cold-climate Bory Stobrawskie Dune Field (SW Poland): Evidence for multi-phase Lateglacial aeolian activity within the European Sand Belt
  58. Adopting a new approach for finding missing people using GIS techniques: A case study in Saudi Arabia’s desert area
  59. Geological earthquake simulations generated by kinematic heterogeneous energy-based method: Self-arrested ruptures and asperity criterion
  60. Semi-automated classification of layered rock slopes using digital elevation model and geological map
  61. Geochemical characteristics of arc fractionated I-type granitoids of eastern Tak Batholith, Thailand
  62. Lithology classification of igneous rocks using C-band and L-band dual-polarization SAR data
  63. Analysis of artificial intelligence approaches to predict the wall deflection induced by deep excavation
  64. Evaluation of the current in situ stress in the middle Permian Maokou Formation in the Longnüsi area of the central Sichuan Basin, China
  65. Utilizing microresistivity image logs to recognize conglomeratic channel architectural elements of Baikouquan Formation in slope of Mahu Sag
  66. Resistivity cutoff of low-resistivity and low-contrast pays in sandstone reservoirs from conventional well logs: A case of Paleogene Enping Formation in A-Oilfield, Pearl River Mouth Basin, South China Sea
  67. Examining the evacuation routes of the sister village program by using the ant colony optimization algorithm
  68. Spatial objects classification using machine learning and spatial walk algorithm
  69. Study on the stabilization mechanism of aeolian sandy soil formation by adding a natural soft rock
  70. Bump feature detection of the road surface based on the Bi-LSTM
  71. The origin and evolution of the ore-forming fluids at the Manondo-Choma gold prospect, Kirk range, southern Malawi
  72. A retrieval model of surface geochemistry composition based on remotely sensed data
  73. Exploring the spatial dynamics of cultural facilities based on multi-source data: A case study of Nanjing’s art institutions
  74. Study of pore-throat structure characteristics and fluid mobility of Chang 7 tight sandstone reservoir in Jiyuan area, Ordos Basin
  75. Study of fracturing fluid re-discharge based on percolation experiments and sampling tests – An example of Fuling shale gas Jiangdong block, China
  76. Impacts of marine cloud brightening scheme on climatic extremes in the Tibetan Plateau
  77. Ecological protection on the West Coast of Taiwan Strait under economic zone construction: A case study of land use in Yueqing
  78. The time-dependent deformation and damage constitutive model of rock based on dynamic disturbance tests
  79. Evaluation of spatial form of rural ecological landscape and vulnerability of water ecological environment based on analytic hierarchy process
  80. Fingerprint of magma mixture in the leucogranites: Spectroscopic and petrochemical approach, Kalebalta-Central Anatolia, Türkiye
  81. Principles of self-calibration and visual effects for digital camera distortion
  82. UAV-based doline mapping in Brazilian karst: A cave heritage protection reconnaissance
  83. Evaluation and low carbon ecological urban–rural planning and construction based on energy planning mechanism
  84. Modified non-local means: A novel denoising approach to process gravity field data
  85. A novel travel route planning method based on an ant colony optimization algorithm
  86. Effect of time-variant NDVI on landside susceptibility: A case study in Quang Ngai province, Vietnam
  87. Regional tectonic uplift indicated by geomorphological parameters in the Bahe River Basin, central China
  88. Computer information technology-based green excavation of tunnels in complex strata and technical decision of deformation control
  89. Spatial evolution of coastal environmental enterprises: An exploration of driving factors in Jiangsu Province
  90. A comparative assessment and geospatial simulation of three hydrological models in urban basins
  91. Aquaculture industry under the blue transformation in Jiangsu, China: Structure evolution and spatial agglomeration
  92. Quantitative and qualitative interpretation of community partitions by map overlaying and calculating the distribution of related geographical features
  93. Numerical investigation of gravity-grouted soil-nail pullout capacity in sand
  94. Analysis of heavy pollution weather in Shenyang City and numerical simulation of main pollutants
  95. Road cut slope stability analysis for static and dynamic (pseudo-static analysis) loading conditions
  96. Forest biomass assessment combining field inventorying and remote sensing data
  97. Late Jurassic Haobugao granites from the southern Great Xing’an Range, NE China: Implications for postcollision extension of the Mongol–Okhotsk Ocean
  98. Petrogenesis of the Sukadana Basalt based on petrology and whole rock geochemistry, Lampung, Indonesia: Geodynamic significances
  99. Numerical study on the group wall effect of nodular diaphragm wall foundation in high-rise buildings
  100. Water resources utilization and tourism environment assessment based on water footprint
  101. Geochemical evaluation of the carbonaceous shale associated with the Permian Mikambeni Formation of the Tuli Basin for potential gas generation, South Africa
  102. Detection and characterization of lineaments using gravity data in the south-west Cameroon zone: Hydrogeological implications
  103. Study on spatial pattern of tourism landscape resources in county cities of Yangtze River Economic Belt
  104. The effect of weathering on drillability of dolomites
  105. Noise masking of near-surface scattering (heterogeneities) on subsurface seismic reflectivity
  106. Query optimization-oriented lateral expansion method of distributed geological borehole database
  107. Petrogenesis of the Morobe Granodiorite and their shoshonitic mafic microgranular enclaves in Maramuni arc, Papua New Guinea
  108. Environmental health risk assessment of urban water sources based on fuzzy set theory
  109. Spatial distribution of urban basic education resources in Shanghai: Accessibility and supply-demand matching evaluation
  110. Spatiotemporal changes in land use and residential satisfaction in the Huai River-Gaoyou Lake Rim area
  111. Walkaway vertical seismic profiling first-arrival traveltime tomography with velocity structure constraints
  112. Study on the evaluation system and risk factor traceability of receiving water body
  113. Predicting copper-polymetallic deposits in Kalatag using the weight of evidence model and novel data sources
  114. Temporal dynamics of green urban areas in Romania. A comparison between spatial and statistical data
  115. Passenger flow forecast of tourist attraction based on MACBL in LBS big data environment
  116. Varying particle size selectivity of soil erosion along a cultivated catena
  117. Relationship between annual soil erosion and surface runoff in Wadi Hanifa sub-basins
  118. Influence of nappe structure on the Carboniferous volcanic reservoir in the middle of the Hongche Fault Zone, Junggar Basin, China
  119. Dynamic analysis of MSE wall subjected to surface vibration loading
  120. Pre-collisional architecture of the European distal margin: Inferences from the high-pressure continental units of central Corsica (France)
  121. The interrelation of natural diversity with tourism in Kosovo
  122. Assessment of geosites as a basis for geotourism development: A case study of the Toplica District, Serbia
  123. IG-YOLOv5-based underwater biological recognition and detection for marine protection
  124. Monitoring drought dynamics using remote sensing-based combined drought index in Ergene Basin, Türkiye
  125. Review Articles
  126. The actual state of the geodetic and cartographic resources and legislation in Poland
  127. Evaluation studies of the new mining projects
  128. Comparison and significance of grain size parameters of the Menyuan loess calculated using different methods
  129. Scientometric analysis of flood forecasting for Asia region and discussion on machine learning methods
  130. Rainfall-induced transportation embankment failure: A review
  131. Rapid Communication
  132. Branch fault discovered in Tangshan fault zone on the Kaiping-Guye boundary, North China
  133. Technical Note
  134. Introducing an intelligent multi-level retrieval method for mineral resource potential evaluation result data
  135. Erratum
  136. Erratum to “Forest cover assessment using remote-sensing techniques in Crete Island, Greece”
  137. Addendum
  138. The relationship between heat flow and seismicity in global tectonically active zones
  139. Commentary
  140. Improved entropy weight methods and their comparisons in evaluating the high-quality development of Qinghai, China
  141. Special Issue: Geoethics 2022 - Part II
  142. Loess and geotourism potential of the Braničevo District (NE Serbia): From overexploitation to paleoclimate interpretation
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