Abstract
Airports are among the constructions that must meet international standards and specifications established by the International Civil Aviation Organization (ICAO). Some of these parameters and criteria include topography, environmental, and operating circumstances. Navigation operations are also affected by terrain and human barriers, while noise, infrastructure, and weather factors affect the environment around airports. This article investigates using the interpretative structure model (ISM) and analytical network process (ANP) together as a new technique to select and determine the optimum site selection for constructing new international airports in the Nile Delta, Egypt. The criteria used (16 international criteria) are selected depending on the standards of the ICAO, field surveys, and previous studies. Nile Delta, Egypt, is chosen as a case study because it suffers from the lack of international airports and has a population of approximately 23 million. Therefore, new international airports must be established to serve this region, boost tourism, improve transportation, and stimulate commercial traffic. The results using the suggested new technique are compared with the traditional used methods for site selection, such as fuzzy-analytic hierarchy process. Landsat 8 images are used in this research. A quality test using the area under the curve and the receiver operating characteristic curve was applied to evaluate the new technique for site selection of international airports, depending on calculating the highest suitability index for each proposed site. From the quality tests, it is deduced that the suggested method (ISM–ANP) for airport site selection is more accurate than any other traditional method. ArcGIS 10.5 software is used to draw the final digital maps containing the proposed resulted sites. As a result, three new locations for the construction of international airports were found and selected throughout the research region (Delta Nile, Egypt) based on the used mathematical models. Therefore, the proposed novel method for determining the locations of international airports is thought to be effective and feasible, and it can be used to determine the locations of any development projects in general, particularly in developing countries, which benefits the decision-makers in making the right decisions.
1 Introduction
Airports are the main pillars of the economy of any country because they are very important and prominent. It is an important infrastructure project and contributes to communications [1]. It plays an important role as a catalyst for local growth and in effective plans in this field and can greatly affect and enhance the local logistics services on the social and economic levels. Infrastructure projects in Egypt are currently progressing rapidly in all fields and in all regions, especially the Nile Delta. The establishment of new international airports has now become an important destination for decision makers in Egypt.
Egypt is located in the north of the African continent, surrounded by the Mediterranean Sea in its north, with a coastline of 995 km. Egypt is considered the main hub of communication and constantly welcomes visitors and investments between European and African countries [2]. Due to tourism, production, service industries, and other fields, those who do not have access to airport services will benefit from developing a new airport in the chosen research area (Nile Delta, Egypt). This article focuses on determining the optimum locations for constructing new international airports, which are essential to be chosen properly. The residents of the study area face difficulty in accessing the nearby airport services; the residents of the selected study area will also benefit from the construction of a new international airport [3]. These changes can simultaneously enhance regional well-being and prosperity through a stable transportation system and a suitable location to address the problem of geographic integration of airport location selection using multi-criteria decision-making (MCDM) deepening on remote sensing and geographic information system (GIS) technology.
GIS technology allows for the storage, organization, and analysis of all forms of geographic data required to establish an international airport. The article combines two models, which are the interpretative structure model (ISM) and analytical network process (ANP) together ISM–ANP methods. The results are compared with traditional methods in site selection such as analytic hierarchy process (AHP) and weighted overly tool (WOA). ISM is used to determine the relationships between the criteria and standards, but ANP is a way to derive the weights of each standard, but the WOA method implements several stages in one modular tool.
One of the best-paired comparisons for determining weights for choice criteria is the AHP approach, which is used to derive ratio measures and is employed in many different sectors of decision-making procedures. Then, the resulted weights were used for ArcGIS input layers (standard maps). The techniques of the ANP, the AHP, and the overweight method are some examples of MCDM used to calculate the weights of criteria [4,5,6].
Beshr et al. used fuzzy-AHP to detect the optimum site selection for isolation hospitals for coronavirus patients in the Nile Delta, Egypt [7]. Mallick et al. [8] used GIS and ANP for wind farm site selection in East Azerbaijan Province, Iran. Exposure of the Anambra state to floods was modeled using the Interval value fuzzy rough number–decision making trial and evaluation laboratory–ANP model in a GIS environment. The location of the general bread factory in Turkey was chosen in an unknown area and their results showed the efficiency of the method and its application to the bread sector [8]. Using the AHP method and application of GIS to landslides in the watershed of Abha, Saudi Arabia, has been investigated. The results showed the feasibility of the strategy to understand how to preserve watersheds in terms of landslides, according to El Jazouli et al. [9].
AHP by Balusa and Gorai [10] helped to create a digital map with important details regarding current and upcoming landslides to enable them to occur. The results showed that the methodology succeeded in selecting the mining method using the GIS-based AHP model and was compared by Balusa and Gorai [10]. Parizi et al. [11] used the two methods of receiver operating characteristic curve (ROC) and AHP to find the best location for the construction of the airport in Libya. According to Erkan and Elsharida [12], a GIS-based approach to the selection of rainwater harvesting sites. Sayl et al. [13] chose the optimal location for groundwater wells by integrating GIS and water geophysical data. Integration of maps of the groundwater potential area using GIS and WOA of northeastern Iraq [14,15]. Multi-criteria GIS resolution analysis by Feizizadeh and Blaschke [16] for landslide sensitivity mapping: comparison of three methods for the Urmia Lake Basin, Iran. Chen [17] has used ISM and artificial neural networks techniques in developing the user expected command location predicting approach.
To help decision-makers identify the most suitable areas for new construction projects, numerous researchers have employed a wide range of techniques to identify the best, or even optimal, locations for particular projects [18,20,21,22,23,24,25,26].
Therefore, this article aims to achieve the following goals:
The possibility of using the ISM–ANP method as a new technique in selecting the airports location in the Nile Delta, Egypt;
Comparing the results of site selection using the proposed technique with traditional site selection techniques; and
Evaluating the ISM–ANP method by applying an accuracy test using the ROC and the area under the curve (AUC).
2 Study area (Nile Delta, Egypt) and airport services
The study area for this study is Nile Delta, Egypt, which is one of the nation’s densely populated regions. The Delta region is situated between the longitudes 30°20′ 0′′E and 32° 0′ 0′′ and the two latitudes 31°30′ 0′′ N and 30°30′ 0′′ N. The Mediterranean Sea, the Suez Canal, Cairo, and Alexandria form this region’s northern, eastern, southern, and western borders, respectively. According to Figure 1, the Nile Delta lies in the Arab Republic of Egypt’s northern region. There are five governorates in Egypt’s Nile Delta: Dakahlia, Kafr El-Sheikh, Damietta, Gharbia, and Menoufia. These governorates are situated between the two branches of the Nile River (Damietta and Rashid). Some governorates, like Dakahlia and Menoufia, may have centers that extend beyond these two branches (Figure 1). Together, these five provinces account for 16735.61 km2 or 1.22% of Egypt’s total land area. Table 1 displays the population, area, and density of Nile Delta governorates. The study area has a total population of 22,223,211, they account for 22.1% of Egypt’s total population (Source: Central Agency for Public Mobilization and Statistics, Egypt 2022). Agriculture, fishing, and the furniture business are the main employers in this community. One of the most significant agricultural and industrial areas is the study area the closest to the Mediterranean coast is considered the main location, so the area must be supported by an air transport network to serve the citizens of Delta and to promote international trade. The total number of Egyptian airports is 19, including 12 international airports with a total capacity of 29,020,100 people/hour and 7 airports National with a total capacity of 1,980 people/h (Source: Egyptian Ministry of Civil Aviation, 2022) (Figure 2).

Study area map (Nile Delta, Egypt).
Areas and populations for Egypt’s Nile Delta governorates in 2022
Governorate | Population (people) 2022 | Area (km2) | Density (population/km2) |
---|---|---|---|
El-Dakhlia | 7,008,548 | 5383.36 | 1301.891 |
El-Gharbia | 5,403,727 | 2648.10 | 2040.605 |
Menoufia | 4,703,192 | 3125.41 | 1504.824 |
Damietta | 1,608,847 | 1225.51 | 1312.798 |
Kafr El-sheikh | 3,682,824 | 4353.23 | 845.998 |
Total | 22,407,138 | 16735.61 | 7006.116 |
Source: Central Agency for Public Mobilization and Statistics, Egypt 2022.

Types and distribution of the existing airports in Egypt.
3 Methodologies and applied analysis models
In this section, the new approach method is presented and described as follows.
3.1 ISM
ISM is a way of figuring out how the parts of a complex system relate to each other. It is used to organize and arrange the connections among the system’s components and establish their relative order. ISM is a technique for structural analysis that is built on an interpretive paradigm [17]. It can be used to investigate the relationships between the various underlying factors of a complex and multidimensional event, as well as the effects of each variable on the others. Different kinds of relationships between variables are possible, including mathematical, chronological, geographical, comparative, and definitive ones [17]. This approach, which is a subset of the multi-criteria approaches, aims to elucidate these connections using the opinions of subject matter experts and a graph theory foundation. The actions in this are explained in the following steps [11]:
Step 1: Structural self-interaction matrix (SSIM)
The experts are first given a square matrix with the size of the number of indications. They are required to use symbols in the matrix that correspond to the different types of relationships between the indicators to represent the paired relationships between them. The following lists these symbols along with what they mean [17].
V: When element I has an impact on element j, but element j has no bearing on element I.
A: When element j impacts element I while element I has no effect on element j.
X: When both components interact.
O: When there is no interaction between the two factors.
To determine the sort of relationship, various management strategies are offered, including brainstorming and nominal groups.
Step 2: Initial reachability matrix (IRM)
The IRM is created using the structural self-interaction matrix (SSIM), with zeros and ones in place of symbols. The SSIM matrix’s zero and one can be switched, provided that (i, j) is the component (i, j) of the SSIM matrix and R(i, j) is the component (i, j) of the reachability matrix.
If $(i, j) = V, then R(i, j) = 1 and R(i, j) = 0.
If $(i, j) = A, then R(i, j) = 0 and R(i, j) = 1.
If $(i, j) = X, then R(i, j) = 1 and R(i, j) = 1.
If $(i, j) = O, then R(i, j) = 0 and R(i, j) = 0.
Step 3: Completing the final reachability matrix (FRM)
According to equation (1), transitivity and Euler’s theorem are used to determine whether the IRM is consistent in order to determine the FRM.
The Boolean rule should be followed when exponentiations A + I
Step 4: Establishing the importance and amount of indicators
This stage uses the FRM to determine two sets of reachability set and antecedent set as follows.
The variables that the element I affect, as well as element I itself, are included in the reachability set for each variable I. As a result, the variables in the row corresponding to variable I that are members of this set are all equal to 1.
The variables that impact element I as well as an element I itself are both included in the antecedent set for each variable I. As a result, the variables in the column corresponding to variable I, which is part of this set, are all equal to 1. The intersection set, which is the set of all variables from both sets, must be identified after these two sets have been established. These data can be used to determine the variables’ level of relevance in the following step. As a result, the variable at the highest level will be one whose reachability is set and intersection sets are equal. The next table is created using the remaining variables once this variable is eliminated from the previous one. The second-level variables are determined by this table. This process keeps going until the levels of all the variables are established. It is easier to understand the function of each indicator and how they interact when indicators are divided into many levels, and their levels are determined [19].
Step 5: Interpretive structure model digraph construction and model evaluation: In this stage, a panel of experts evaluates the connections between the variables at various levels that were derived from the final reachability matrix in the preceding step. They are then requested to rank the relationship in order of minimal to largest influence on a scale of one to five. Next, the levels, the final reachability matrix, the results of the model evaluation, and the elimination of transitivity from the original model are used to build the final model [19].
3.2 ANP method
The ANP approach is a generalization of the AHP method and one of the multi-criteria decision-making (MCDM) methods. In reality, the ANP technique supports interdependence between criteria and sub-criteria, whereas the AHP method does not [20].
When the criteria or sub-criteria are tied to each other internally, the problem is not hierarchical; instead, it has a network state. The ANP approach is used in this instance to resolve the issue. The analytical network approach offers a thorough and effective way to make informed decisions using the empirical data or individual opinions of each decision-maker [13]. In the ANP, sub-criteria are arranged in clusters, and factors and indicators form a network of criteria. It is crucial to establish the connections between the clusters and sub-criteria because of their dependencies.
Step 1: Creating the model and network diagram
A network of criteria and sub-criteria are joined together in clusters to form the elements and indicators in ANP. Finding the linkages between the various criteria and sub-criteria of the system is a crucial stage in this process because these criteria and sub-criteria are related to one another. Methods like ISM can be used to find these connections [21]. Through this, the accessibility matrix M is transformed into an ANP network architecture, and Super Decisions software is used to generate the model.
Step 2: In the entire network, benchmarks are compared using the amazing decisions program.
Using pairwise comparisons to create an unweighted super matrix, such as AHP decision-makers now compare the two components. Scores, which range from 1 to 9, are used for pairwise comparisons [22]. To express an inverse comparison, one uses the reciprocal of each integer. The comparison matrix, which is formed from the eigenvector, and the local priority vector contain the values for pairwise comparisons. Matrix consistency as measured by AHP ought to be less than 0.1 [17]. However, if the consistency ratio is more than 0.1, experts must respond to queries. Progressively more cautious, the consistency ratio is calculated using opinions using the former (AGIS MUITI CERTIRIA) equation (2), and high degrees of inconsistency reveal conflicts in expert opinion
where n is the number of components compared in the matrix, max is its maximum eigenvalue, CR is its consistency ratio, CI is its consistency index, and RI is its random index (matrix dimensions). The geometric mean method was then used to integrate the paired comparison matrices. The eigenvector approach is then used to calculate the weight vectors (equation (3)):
where λ max is the largest eigenvalue of the matrix, W is the normalized weight vector, while A is the paired comparison matrix, which
Step 3: Super matrices, both weighted and unweighted
The weights obtained in the first stage of the ANP model are used in the third step.
Based on the problem’s structure, they are all grouped together in an array called improbable. Matrix super. To compute all the priorities and the cumulative impact of each component on the other components with which it interacts, the supermatrix can limit the coefficients. The effects of clusters or groupings of elements on one another are represented by the supermatrix. The sum of each special column vector that makes up an unweighted super matrix’s columns is one. Consequently, more than one can result from the addition of all primary or unweighted supermatrix columns (corresponding to the columns’ respective vectors). The initial supermatrix is referred to in this stage as the supermatrix. The general form of the super matrix is seen in equation (2) [21].
Step 4: In order to weight the initial supermatrix, compute the cluster weights in this step. Once the cluster weight matrix has been generated, the initial supermatrix can be weighted by multiplying the cluster weights matrix by an initial super matrix [6].
The weighted supermatrix is the name of the newly obtained matrix. To output a column, each array column needs to be standardized. The elements must add up to one and be proportional to their respective weights. As a result, a new matrix is created with each column’s sum equaling 1. That’s its super-weighted matrix is the name of the matrix by itself to the maximum super matrix size has been attained. The supermatrix is weighted until its linear values are equal and the array’s elements converge. In light of equation (4):
where WI is the limit supermatrix with one number on each line. These numbers show the indicators’ weight [4,23].
4 Research methodology and procedure steps
Figure 3 depicts a rough summary and methodology of the research, explaining the techniques used to determine the optimum locations for constructing new international airports in the study area and the stages involved in each method.

Flow chart of the research methodology.
5 Selection of criteria for international airport site selection
The selected applied criteria were chosen depending on the Federal Aviation Administration, the International Civil Aviation Organization, the literature review of prior studies, expert opinion through actual field visits to existing airports and asking their specialists, and the availability of the data including maps, documents, etc.
The five primary categories of choice criteria to select new international airport locations are environmental concerns, topographical characteristics, climatic aspects, infrastructure facilities, and operating requirements. There are sub-criteria for each of the primary criteria, and each sub-criterion is also categorized. All of these criteria and sub-criteria have been collected into a comprehensive set of elements (parameters) that are summarized in Table 2. Thus, there are a total of 16 applicable criteria in this study, as shown in Table 2.
Applied criteria for the study zone (Nile Delta, Egypt)
Parameter (criteria) code | Parameter description |
---|---|
SC1 | Topographical altitude |
SC2 | Earth tilt |
SC3 | Soil type |
SC4 | Major roads |
SC5 | Water resource |
SC6 | Power station |
SC7 | Communication station |
SC8 | Gas and oil station |
SC9 | Center of cities |
SC10 | Land use and land cover |
SC11 | Notice pollution |
SC12 | Rainfall |
SC13 | Temperature |
Sc14 | Wind speed |
SC15 | Pressure |
SC16 | Relative% |
6 Data collection for the research
The input data for this study came from a wide range of sources: Landsat images, topographic maps, and official, and governmental data required for research. All of the images were created by digitizing, scanning, and geocoding the pertinent data after they were gathered at different resolutions and sizes. In addition, GIS methods such as intersection, union, buffering, interpolation, map algebra, and overlay were used to construct the topographic maps.
The studied area (Nile Delta, Egypt) was categorized into five soil types (sand, loam, clay, clay loam, and sand loam) based on geological governmental data and soil stratification. Soil type, elevation above sea level, and other criteria outlined in Tables 2 and 3 were considered to ensure alignment with international standards. Upon examining the study area, the geological composition was found to have remained largely unchanged for over 20 years, depending on the official reports.
Used criteria, sources, format, and the scale factor
Factor | Source | Format | Resolution or scale | Used to build a layer |
---|---|---|---|---|
Slope, elevation, water stream | United States Geological Survey (USGS) | Digital | 30 × 30 | Slope (%), elevation (m), distance from water stream |
Roads, power line, waterbodies, River Nile | Diva GIS | Vector data | Shape file | The proximity of roads, the proximity of water resource |
Communication state, gas, and oil well | Google Map | Vector data | The shape file download is then prepared by the author | The proximity of communication state, the proximity of gas and oil well |
Land use/land cover | USGS | Digital | Unsupervised classification | Selecting appropriate land |
Soil | Soil and Water Assessment (SWAT 2012) | Table | Code type of Soil | Selecting appropriate Soil |
Precipitation, temperature, wind, atmospheric pressure, humidity | Climate Research Unit (CRU) | Digital | Drown by author entering in GIS software to implement interpolation between points Location using the tool Kriging | The proper wind speed (m/s), the proper temperature (°C), and the value of the atmospheric pressure (kPa) |
Because the input data utilized by different organizations are typically created and compiled for applications, they have distinct formats, scales, and projection systems. All of those data (United States Geological Survey) were georeferenced using the Transverse Mercator projection system within the GIS environment. Syntaxinthe final needed layers were then obtained through a series of GIS steps (including extract, proximity, buffer, overlay, convert, and clip) and, ultimately, rasterizing those vector maps (shape files).
For infrastructure data, the Esri firm created the ArcGIS Editor OSM tool, which makes the possibility to download directly to the program, starting with version 10. It is straightforward to download shape files of infrastructure for the necessary study zone using this program. Shape files can be downloaded directly from the website as well. Preparing the layers is done as follows.
The meteorological information, which included temperature, wind, humidity, air pressure, precipitation, and clearness index, was obtained from the NASA Imagery Satellite at (power.larc.nasa.gov):
A point grid was created for every study area (22 points).
The necessary data were obtained as an Excel file from the NASA satellite.
The required data’s average was determined for each point in the grid and then entered.
Apply the command from the Arc toolbox (3D analyst tools – Raster interpolation – Kriging) while pointing the GIS program at a grid point.
Creation of a raster layer and land cover layer through:
The source from which the layer of land cover for Egypt was downloaded.
Using the study zone’s mask layer and the extract-clip from Arc Toolbox function.
Using Egyptian datum to geocode the layer of land cover.
7 Reclassifying and redistributing the criteria and sub-criteria
Every criterion layer has a different unit from the others. Therefore, in order to implement a weighted overlay process, they must typically be in the same units. As a result, standardization is necessary to make the dimension units uniform, but in doing so, the scores typically lose both their dimensions and their measurement unit [24]. To create the appropriateness index map, all input layers were transformed into raster layers and categorized before being added to the weighted overlay (Figures 4–7). Assigning rating values from 1 to 9 (from the least to the most) based on the data from the literature research, the opinions of experts, and specifics on the safe distances and buffering zones to an airport site define the reclassifying task suitableness, as shown in Table 4. Note that, in Figures 4–7, the number 9 indicates the highest effect. The lower the number indicates the gradation of the effect from the highest, which is 9, to the lowest, which is 1.

Reclassification of the topographical map.

Reclassification of the infrastructure map.

Reclassification of operational and environment condition map.

Reclassification of the climatic factor map.
Reclassification of the input layers
Main criteria | Sub-criteria | Reclassification | Score | Source |
---|---|---|---|---|
Topographical | Elevation (m) | ≤122 | 9 | USGS |
38.6–58.6 | 8 | |||
18.6–38.6 | 7 | |||
4.6–18.6 | 6 | |||
4.666≥ | 5 | |||
Slope% | 0–0.49 | 9 | ||
0.49–1.55 | 9 | |||
1.55–2.9 | 8 | |||
2.99–5.7 | 7 | |||
≥48.1 | 3 | |||
Soil type | Sand | 10 | Soil and Water Assessment (SWAT 2012) | |
Loam | 6 | |||
Clay | 4 | |||
Clay Loam | 6 | |||
Sandy Loam | 7 | |||
Infrastructure | Major roads (m) | 0–1758.6 | 9 | Diva GIS |
1758.6–3976 | 8 | |||
3976.2–7187.5 | 7 | |||
≥19574.5 | 3 | |||
Water streams (m) | 0–3054.8 | 9 | Diva GIS/digital elevation model | |
≥18547.4 | 1 | |||
Water body (m) | 6.979≥ | 9 | ||
6.979–16.517 | 8 | |||
16.517–27.450 | 5 | |||
≤27.450 | 3 | |||
River Nile (m) | 0–10,020 | 9 | ||
10,020–21,630 | 7 | |||
21,630–34,530 | 5 | |||
≥62046.5 | 3 | |||
Proximity from power station (m) | 0–16808.3 | 9 | Google Map | |
16808.3–29628.2 | 7 | |||
29628.2–29628.7 | 5 | |||
≥72646.2 | 2 | |||
Proximity from communication station (km) | 0–0.2734 | 9 | Google Map | |
0.2734–0.4876 | 7 | |||
0.4876–0.7656 | 5 | |||
≥1.1576 | 3 | |||
Operational conditions | Proximity from gas and oil station | 0–0.5915 | 9 | Google Map |
0.5915–1.3642 | 8 | |||
Center of cities (km) | 0–0.1970 | 9 | Diva GIS | |
0.1970–0.3472 | 8 | |||
0.3472–0.4917 | 6 | |||
0.4917–0.6494 | 5 | |||
≥0.9546 | 3 | |||
Environment considerations | Land use and land cover | Herbaceous or shrub cover | 1 | United States Geological Survey (USGS) |
Cultivated area | 1 | |||
Bare land | 10 | |||
Water bodies | 10 | |||
Associated area | 6 | |||
Density of population (m) | 0–1627.5 | 1 | World Pop | |
1627.5–13563.2 | 7 | |||
13563.2–45030.1 | 8 | |||
138345.5≤ | 9 | |||
Climatic factors | Rainfall (mm/day) | ≥2.666671 | 3 | CRU |
6.383662–9.547059 | 2 | |||
≤12.749999 | 1 | |||
Temperature (°C) | ≥22.05 | 9 | CRU | |
≤23.225 | 8 | |||
Wind speed (m/s) | 4.9477–5.47 | 9 | CRU | |
5.42–5.75 | 8 | |||
≥6.4571 | 7 | |||
Pressure (kPa) | 101.4–101.4 | 7 | CRU | |
101.40–101.40 | 8 | |||
≥101.4099 | 9 | |||
Relative% | 1.323–1.837 | 9 | CRU | |
1.837–2.3918 | 8 | |||
≥3.0699 | 7 |
8 Implementation and outcomes of ISM
Finding the problem-related variables is the first step in this method of structuring the problem indicators. The contextual links between the indicators are then established utilizing specialists’ experience, theoretical knowledge, and practical expertise.
The provision of a multi-level structural model comes last. Fifteen university professors who are specialists in crisis management, urban planning, and seismic engineering collaborated in this study and answered a questionnaire on this method. The following were the steps in the implementation: formation of the SSIM.
Step 1: The experts received the pertinent questionnaire in the form of a square matrix with the same rows and columns as the urban physical indicators. The final structural self-interaction matrix is obtained after compiling all the finished opinions and matrices according to the outcomes of paired comparisons. Therefore, a relationship between the two components is considered if it is supported by the majority of the expert group (N/2 + 1 votes); otherwise, there is no relationship between the two components. This matrix is shown in Table 5.
Resulted SSIM
Variables | 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | 11 | 12 | 13 | 14 | 15 | 16 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
SC1 | X | O | O | V | O | O | O | O | V | O | V | V | V | V | O | |
SC2 | O | V | V | O | O | O | O | V | O | V | O | V | V | O | ||
SC3 | O | A | O | O | V | O | A | O | A | A | A | O | A | |||
SC4 | O | O | O | O | O | A | O | O | O | O | O | O | ||||
SC5 | O | O | O | O | V | V | A | V | A | A | V | |||||
SC6 | O | A | O | A | O | A | O | A | O | O | ||||||
SC7 | O | A | A | O | O | O | O | O | O | |||||||
SC8 | O | V | V | A | A | O | O | O | ||||||||
SC9 | V | X | O | O | O | O | O | |||||||||
SC10 | X | O | O | O | O | O | ||||||||||
SC11 | O | O | O | O | O | |||||||||||
SC12 | X | X | A | A | ||||||||||||
SC13 | V | A | A | |||||||||||||
SC14 | A | V | ||||||||||||||
SC15 | O | |||||||||||||||
SC16 |
Step 2: Creation of the IRM
The SSIM and the symbol substitution method are used to create the IRM.
Step 3: Creation of the FRM
The equation is then used to determine the consistency of the initial reachability matrix and produce the final reachability matrix (1).
Step 4: Grouping and ordering indicators according to the importance
This stage uses the final reachability matrix to determine two sets of reachability set and antecedent set. The level partitioning (LP) of the indicators used in the current study is shown in Table 6.
LP of the indicators
Elements (MI) | Reachability set R (MI) | Antecedent set A (Ni) | Intersection set R(MI) ∩ A(Ni) | Level |
---|---|---|---|---|
1 | 1,2 | 1,2 | 1,2 | 5 |
2 | 1,2 | 1,2 | 1,2 | 5 |
3 | 3,8,9,10,11 | 1,2,3,5,8,9,10,11,12,13,14,15,16 | 3,8,9,10,11 | 2 |
4 | 4, | 1,2,3,5,8,9,10,11,12,13,14,15,16 | 4 | 1 |
5 | 5,12,13,14,16 | 1,2,5,12,13,14,15,16 | 5,12,13,14,16 | 3 |
6 | 6, | 1,2,3,5,6,8,9,10,11,12,13,14,15,16 | 6 | 1 |
7 | 7, | 1,2,3,5,6,8,9,10,11,12,13,14,15,16 | 7 | 1 |
8 | 3,8,9,10,11 | 1,2,3,5,8,9,10,11,12,13,14,15,16 | 3,8,9,10,11 | 2 |
9 | 3,8,9,10,11 | 1,2,3,5,8,9,10,11,12,13,14,15,16 | 3,8,9,10,11 | 2 |
10 | 3,8,9,10,11 | 1,2,3,5,8,9,10,11,12,13,14,15,16 | 3,8,9,10,11 | 2 |
11 | 3,8,9,10,11 | 1,2,3,5,8,9,10,11,12,13,14,15,16 | 3,8,9,10,11 | 2 |
12 | 5,12,13,14,16 | 1,2,5,12,13,14,15,16 | 5,12,13,14,16 | 3 |
13 | 5,12,13,14,16 | 1,2,5,12,13,14,15,16 | 5,12,13,14,16 | 3 |
14 | 5,12,13,14,16 | 1,2,5,12,13,14,15,16 | 5,12,13,14,16 | 3 |
15 | 15, | 1,2,15 | 15 | 4 |
16 | 5,12,13,14,16 | 1,2,5,12,13,14,15,16 | 5,12,13,14,16 | 3 |
Step 5: Model assessment and the creation of the interpretive structure model digraph
Using the relationships taken from the final reachability matrix and the preceding stage, a group of seven experts assessed the model. Subsequently, the ultimate model is created based on the outcomes of the fourth phase and the model assessment findings. In the ISM model, an indicator will be at a lower level if it has an impact on others. On the other hand, an indicator will be of higher quality if it is strongly influenced by other indications. The ISM model displays an effect from bottom to top. There are five levels in the final model this study created (Figure 8). This model shows the most significant relationships. The directions of the arrows indicate how each factor affects the others.

The diamgraph of ISM-based model.
9 Implementation of ANP
Determining the importance of each urban physical indicator using this methodology is done.
Physical toughness: This model’s calculations were carried out using Super Decision and MATLAB software. The model’s phases for implementation are as follows:
Step 1: The network diagram and creation of the ANP model
Three clusters of urban physical indicators are identified in this study.
Inside each cluster, there are multiple linked signs. The ISM model produces clusters (Figure 9).

The procedure used to calculate the weight vectors.
Step 2: Forming the unweighted and weighted super matrices
The unweighted super matrix was created in this stage using the weights gained in the preceding step. The weighted supermatrix has dimensions (16 rows × 16 columns) and was created by standardizing the columns of the unweighted supermatrix table.
The unweighted super matrix was created in this stage using the weights gained in the preceding step. The weighted super matrix was created by standardizing the columns of the unweighted supermatrix. Limit Super matrix generation is specified in Step 4 (Figures 10 and 11).

The weight of the applied indicators.

Output map of applying ANP method.
10 AHP application
Based on the opinions of the experts, the analytic hierarchy technique was used in this study to evaluate the factors that influence and characterize urban physical resilience. The same set of experts from the ANP model offered their input and advised importance ratings in paired comparisons for this reason (Table 7) [6]. According to Table 7, professionals use paired comparison matrices to express their viewpoints.
Relative importance values in paired comparisons
Rank of importance | Definition | Description |
---|---|---|
1 | Equal importance | To accomplish the goal, two components are equally crucial |
3 | Some more important | There is one that is marginally more significant than the other |
5 | Much more important | There is a more significant aspect than the other |
7 | Very much important | One component is far more crucial than the other |
9 | Extremely important | One component is far more significant than the other |
2,4,6,8 | Values in the middle of adjacent values | Comparison times are required |
Reciprocals above | Equivalent in terms of inverse comparison | When comparing in reverse, the inverse number needs to be taken into account |
The weight of each attribute is established by creating paired comparison matrices and figuring out the consistency ratio. Based on the judgments of the experts, Table 8 displays the relative relevance of several features in relation to one another (the weight of the main criteria) (Figures 12–14) (Table 9).
Main criteria, sub-criteria, and their relative weight were computed by using the AHP method
Main criteria | Sub-criteria | Weights |
---|---|---|
Topographical | Topographical altitude | 0.090404 |
Earth tilt | 0.022601 | |
Soil type | 0.045202 | |
Infrastructure | Major roads | 0.222222 |
Water resource | 0.444444 | |
Power station | 0.222222 | |
Communication station | 0.111111 | |
Environment considerations | Gas and oil station | 0.064312 |
Center of cities | 0.128624 | |
Operational conditions | Land use and land cover | 0.138518 |
Notice pollution | 0.277036 | |
Climatic factors | Rainfall | 0.028455 |
Temperature | 0.028455 | |
Wind speed | 0.022401 | |
Pressure | 0.016814 | |
Relative% | 0.062083 | |
Total | 1.00 |

Output map of applying the AHP method.

Weighted overlay tool model for the study’s requirements.

Resulted map of applying the WOA method.
Airport output location areas and percentages resulting from the ANP, AHP, and WOA methods
Rank area | Areas of optimum location airports from ANP | Percentage | Areas of optimum location airports from AHP | Percentage | Areas of optimum location airports from WOA | Percentage |
---|---|---|---|---|---|---|
Average to good | 89.9 | 0.005 | 786.5 | 0.047 | 708.8 | 0.042 |
Good | 3655.5 | 0.218 | 3631.5 | 0.217 | 3628.8 | 0.217 |
Very good | 11959 | 0.715 | 11045.1 | 0.66 | 10826.4 | 0.647 |
Excellent | 1011.6 | 0.060 | 1171.5 | 0.07 | 1434.6 | 0.086 |
Optimum | 19 | 0.002 | 100.4 | 0.006 | 136.4 | 0.008 |
Total | 16,735 | 1.00 | 16,735 | 1.00 | 16,735 | 1.00 |
Five categories emerged from the use of the three methods: optimum suitability, excellent suitability, very good suitability, good suitability, and average to good suitability. By comparing the results obtained with the three methods, it was found that there was some convergence in the analysis of the results obtained.
11 Suitability assessment of the suggested resulted airport sites
After the application process in the three methods, three candidate sites were selected to satisfy all site requirements and are located at different locations within the highest suitability index regions (suitability index 7–9). Each of the suggested site will have assigned letter – A, B, C – and each cover about 50 km2 (5,000 ha); max (Figure 15) in order to determine the optimum suitable site (Figures 16 and 17).

Optimum location map, using the ANP method.

Optimum location map, using the AHP method.

Optimum location map, using the WOA method.
12 Analysis and results
The ROC curve is a graphical representation of the performance of a binary classifier mode. Plotting the true positive rate vs the false positive rate at various categorization criteria is how it is made. The AUC/ROC is a measure of the classifier’s ability to discriminate. The curve is important because it provides a single number that summarizes the performance of the classifier across all possible thresholds. It is also insensitive to unbalanced class distribution. This curve is a useful measure for evaluating binary classification models. By calculating the area under the ROC curve, a single number can be obtained that summarizes the classifier’s ability to distinguish between classes, which makes it easy to evaluate the performance of classification models.
AUC is a synthetic measure created for ROC curves that defines the probability that an event categorized as positive by the test will occur in reality given all potential positive test results. The quantitative and qualitative relationships between the American University of Cairo and the prediction rate are expressed as follows: unsatisfactory (0.5–0.6), satisfactory (0.6–0.7), good (0.7–0.8), very good (0.8–0.9), and excellent (0.9–1). The ISM–ANP model is validated using AUC/ROC. The research region was gathered and used as a validation dataset. These locations were imported into the GIS Environment and validated using the ROC tool (Figures 18–21).

Steps to determine the AUC.

Test quality for AHP using the AUC/ROC curve.

Test quality for ANP using the AUC/ROC curve.

Test quality for WOA using the AUC/ROC curve.
According to the verification results, the ISM–ANP approach obtained outstanding validation accuracy with an AUC value of 0.990, while the AHP method achieved 0.936, as did the WOA method. This indicates that the ISM–ANP model is the most successful at evaluating airport site selection.
13 Conclusion
This article presents a combination of two techniques, ANP and ISM models, integrating GIS to detect the optimum site selection of new international airports in Nile Delta, Egypt. The suggested technique is compared with traditional methods using an accuracy test. Using suggested models integrating with GIS technology and multiple environmental and scientific standards followed in developed countries represents an efficient and elaborate technique in the selection of appropriate sites for airports in Egypt and makes the vision clear for decision-makers to choose the best places to establish new international airports or any other national project. Therefore, the following conclusions can be drawn.
Three new locations for the construction of international airports were found and selected throughout three governorates in the research region (Delta Nile, Egypt) based on the used mathematical models: Kafr El Sheikh, El Dakahlia, and El Menoufia. We were able to identify the most important zones for additional investigation using these models. Using ArcGIS 10.5, 16 input criteria (layers) were added to an overlay analysis process with GIS to solve the issue of where to locate the airport in the suggested area, a technological advancement that has the capacity to handle massive amounts of data from several sources. The following parameters were considered in this analysis: distance from residential areas (noise and pollution), land cover type, precipitation, temperature, wind speed, atmospheric pressure, relative humidity, altitude above sea level, land slope percentage, soil properties, ease of access to roads, water resources, power lines, communication stations, oil and gas lines, and urban centers.
Using ANP methodologies, the weights of the standards were established based on the geographical features of the study area (Nile Delta, Egypt), relevant laws and regulations, a review of the literature on previous research, and expert opinion. The finished map contained five different types of suitability indications, ranging from modest to very efficient.
The ISM–ANP approach was compared to the usual methods (AHP), and the three generated maps were compared. Three sites have been proposed for airport sites out of numerous locations with the greatest suitability index according to the approach map used.
The quality of result test was carried out for the chosen method using ROC_AUC with the usual methods for evaluating the reliability of the method employed, and the ranking of the suggested resulted sites. The obtained findings demonstrate the approach adopted. Despite variances in decision weights within the domain, it entirely outperformed the other potential sites.
Field investigations and satellite imagery analysis show that the indicated sites are consistent with the form’s results. The results of this study show that the performance is accurate. The model used to locate Egypt’s airport is quite precise. As a result, it can be customized as a decision-support tool for decision-makers and planners.
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Funding information: Funding information is not applicable/No funding was received.
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Author contributions: Conceptualization, Ashraf A. A. Beshr; methodology, Ashraf A. A. Beshr; software, Ali M. Basha; formal analysis, Nourhan Lofty; investigation, Nourhan Lofty; field works and resources, Ashraf A. A. Beshr; data curation, Nourhan Lofty; writing – original draft preparation, Magda H. Farhan; writing – review and editing, Magda H. Farhan; supervision, all authors have read and agreed to the published version of the manuscript.
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Conflict of interest: On behalf of all authors, the corresponding author states that there is no conflict of interest.
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Data availability statement: All data, models, and code generated or used during the study appear in the submitted article.
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- Modification of dolomitization on reservoir spaces in reef–shoal complex: A case study of Permian Changxing Formation, Sichuan Basin, SW China
- Geological characteristics of the Daduhe gold belt, western Sichuan, China: Implications for exploration
- Rock physics model for deep coal-bed methane reservoir based on equivalent medium theory: A case study of Carboniferous-Permian in Eastern Ordos Basin
- Enhancing the total-field magnetic anomaly using the normalized source strength
- Shear wave velocity profiling of Riyadh City, Saudi Arabia, utilizing the multi-channel analysis of surface waves method
- Effect of coal facies on pore structure heterogeneity of coal measures: Quantitative characterization and comparative study
- Inversion method of organic matter content of different types of soils in black soil area based on hyperspectral indices
- Detection of seepage zones in artificial levees: A case study at the Körös River, Hungary
- Tight sandstone fluid detection technology based on multi-wave seismic data
- Characteristics and control techniques of soft rock tunnel lining cracks in high geo-stress environments: Case study of Wushaoling tunnel group
- Influence of pore structure characteristics on the Permian Shan-1 reservoir in Longdong, Southwest Ordos Basin, China
- Study on sedimentary model of Shanxi Formation – Lower Shihezi Formation in Da 17 well area of Daniudi gas field, Ordos Basin
- Multi-scenario territorial spatial simulation and dynamic changes: A case study of Jilin Province in China from 1985 to 2030
- Review Articles
- Major ascidian species with negative impacts on bivalve aquaculture: Current knowledge and future research aims
- Prediction and assessment of meteorological drought in southwest China using long short-term memory model
- Communication
- Essential questions in earth and geosciences according to large language models
- Erratum
- Erratum to “Random forest and artificial neural network-based tsunami forests classification using data fusion of Sentinel-2 and Airbus Vision-1 satellites: A case study of Garhi Chandan, Pakistan”
- Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part I
- Spatial-temporal and trend analysis of traffic accidents in AP Vojvodina (North Serbia)
- Exploring environmental awareness, knowledge, and safety: A comparative study among students in Montenegro and North Macedonia
- Determinants influencing tourists’ willingness to visit Türkiye – Impact of earthquake hazards on Serbian visitors’ preferences
- Application of remote sensing in monitoring land degradation: A case study of Stanari municipality (Bosnia and Herzegovina)
- Optimizing agricultural land use: A GIS-based assessment of suitability in the Sana River Basin, Bosnia and Herzegovina
- Assessing risk-prone areas in the Kratovska Reka catchment (North Macedonia) by integrating advanced geospatial analytics and flash flood potential index
- Analysis of the intensity of erosive processes and state of vegetation cover in the zone of influence of the Kolubara Mining Basin
- GIS-based spatial modeling of landslide susceptibility using BWM-LSI: A case study – city of Smederevo (Serbia)
- Geospatial modeling of wildfire susceptibility on a national scale in Montenegro: A comparative evaluation of F-AHP and FR methodologies
- Geosite assessment as the first step for the development of canyoning activities in North Montenegro
- Urban geoheritage and degradation risk assessment of the Sokograd fortress (Sokobanja, Eastern Serbia)
- Multi-hazard modeling of erosion and landslide susceptibility at the national scale in the example of North Macedonia
- Understanding seismic hazard resilience in Montenegro: A qualitative analysis of community preparedness and response capabilities
- Forest soil CO2 emission in Quercus robur level II monitoring site
- Characterization of glomalin proteins in soil: A potential indicator of erosion intensity
- Power of Terroir: Case study of Grašac at the Fruška Gora wine region (North Serbia)
- Special Issue: Geospatial and Environmental Dynamics - Part I
- Qualitative insights into cultural heritage protection in Serbia: Addressing legal and institutional gaps for disaster risk resilience
Articles in the same Issue
- Regular Articles
- Theoretical magnetotelluric response of stratiform earth consisting of alternative homogeneous and transitional layers
- The research of common drought indexes for the application to the drought monitoring in the region of Jin Sha river
- Evolutionary game analysis of government, businesses, and consumers in high-standard farmland low-carbon construction
- On the use of low-frequency passive seismic as a direct hydrocarbon indicator: A case study at Banyubang oil field, Indonesia
- Water transportation planning in connection with extreme weather conditions; case study – Port of Novi Sad, Serbia
- Zircon U–Pb ages of the Paleozoic volcaniclastic strata in the Junggar Basin, NW China
- Monitoring of mangrove forests vegetation based on optical versus microwave data: A case study western coast of Saudi Arabia
- Microfacies analysis of marine shale: A case study of the shales of the Wufeng–Longmaxi formation in the western Chongqing, Sichuan Basin, China
- Multisource remote sensing image fusion processing in plateau seismic region feature information extraction and application analysis – An example of the Menyuan Ms6.9 earthquake on January 8, 2022
- Identification of magnetic mineralogy and paleo-flow direction of the Miocene-quaternary volcanic products in the north of Lake Van, Eastern Turkey
- Impact of fully rotating steel casing bored pile on adjacent tunnels
- Adolescents’ consumption intentions toward leisure tourism in high-risk leisure environments in riverine areas
- Petrogenesis of Jurassic granitic rocks in South China Block: Implications for events related to subduction of Paleo-Pacific plate
- Differences in urban daytime and night block vitality based on mobile phone signaling data: A case study of Kunming’s urban district
- Random forest and artificial neural network-based tsunami forests classification using data fusion of Sentinel-2 and Airbus Vision-1 satellites: A case study of Garhi Chandan, Pakistan
- Integrated geophysical approach for detection and size-geometry characterization of a multiscale karst system in carbonate units, semiarid Brazil
- Spatial and temporal changes in ecosystem services value and analysis of driving factors in the Yangtze River Delta Region
- Deep fault sliding rates for Ka-Ping block of Xinjiang based on repeating earthquakes
- Improved deep learning segmentation of outdoor point clouds with different sampling strategies and using intensities
- Platform margin belt structure and sedimentation characteristics of Changxing Formation reefs on both sides of the Kaijiang-Liangping trough, eastern Sichuan Basin, China
- Enhancing attapulgite and cement-modified loess for effective landfill lining: A study on seepage prevention and Cu/Pb ion adsorption
- Flood risk assessment, a case study in an arid environment of Southeast Morocco
- Lower limits of physical properties and classification evaluation criteria of the tight reservoir in the Ahe Formation in the Dibei Area of the Kuqa depression
- Evaluation of Viaducts’ contribution to road network accessibility in the Yunnan–Guizhou area based on the node deletion method
- Permian tectonic switch of the southern Central Asian Orogenic Belt: Constraints from magmatism in the southern Alxa region, NW China
- Element geochemical differences in lower Cambrian black shales with hydrothermal sedimentation in the Yangtze block, South China
- Three-dimensional finite-memory quasi-Newton inversion of the magnetotelluric based on unstructured grids
- Obliquity-paced summer monsoon from the Shilou red clay section on the eastern Chinese Loess Plateau
- Classification and logging identification of reservoir space near the upper Ordovician pinch-out line in Tahe Oilfield
- Ultra-deep channel sand body target recognition method based on improved deep learning under UAV cluster
- New formula to determine flyrock distance on sedimentary rocks with low strength
- Assessing the ecological security of tourism in Northeast China
- Effective reservoir identification and sweet spot prediction in Chang 8 Member tight oil reservoirs in Huanjiang area, Ordos Basin
- Detecting heterogeneity of spatial accessibility to sports facilities for adolescents at fine scale: A case study in Changsha, China
- Effects of freeze–thaw cycles on soil nutrients by soft rock and sand remodeling
- Vibration prediction with a method based on the absorption property of blast-induced seismic waves: A case study
- A new look at the geodynamic development of the Ediacaran–early Cambrian forearc basalts of the Tannuola-Khamsara Island Arc (Central Asia, Russia): Conclusions from geological, geochemical, and Nd-isotope data
- Spatio-temporal analysis of the driving factors of urban land use expansion in China: A study of the Yangtze River Delta region
- Selection of Euler deconvolution solutions using the enhanced horizontal gradient and stable vertical differentiation
- Phase change of the Ordovician hydrocarbon in the Tarim Basin: A case study from the Halahatang–Shunbei area
- Using interpretative structure model and analytical network process for optimum site selection of airport locations in Delta Egypt
- Geochemistry of magnetite from Fe-skarn deposits along the central Loei Fold Belt, Thailand
- Functional typology of settlements in the Srem region, Serbia
- Hunger Games Search for the elucidation of gravity anomalies with application to geothermal energy investigations and volcanic activity studies
- Addressing incomplete tile phenomena in image tiling: Introducing the grid six-intersection model
- Evaluation and control model for resilience of water resource building system based on fuzzy comprehensive evaluation method and its application
- MIF and AHP methods for delineation of groundwater potential zones using remote sensing and GIS techniques in Tirunelveli, Tenkasi District, India
- New database for the estimation of dynamic coefficient of friction of snow
- Measuring urban growth dynamics: A study in Hue city, Vietnam
- Comparative models of support-vector machine, multilayer perceptron, and decision tree predication approaches for landslide susceptibility analysis
- Experimental study on the influence of clay content on the shear strength of silty soil and mechanism analysis
- Geosite assessment as a contribution to the sustainable development of Babušnica, Serbia
- Using fuzzy analytical hierarchy process for road transportation services management based on remote sensing and GIS technology
- Accumulation mechanism of multi-type unconventional oil and gas reservoirs in Northern China: Taking Hari Sag of the Yin’e Basin as an example
- TOC prediction of source rocks based on the convolutional neural network and logging curves – A case study of Pinghu Formation in Xihu Sag
- A method for fast detection of wind farms from remote sensing images using deep learning and geospatial analysis
- Spatial distribution and driving factors of karst rocky desertification in Southwest China based on GIS and geodetector
- Physicochemical and mineralogical composition studies of clays from Share and Tshonga areas, Northern Bida Basin, Nigeria: Implications for Geophagia
- Geochemical sedimentary records of eutrophication and environmental change in Chaohu Lake, East China
- Research progress of freeze–thaw rock using bibliometric analysis
- Mixed irrigation affects the composition and diversity of the soil bacterial community
- Examining the swelling potential of cohesive soils with high plasticity according to their index properties using GIS
- Geological genesis and identification of high-porosity and low-permeability sandstones in the Cretaceous Bashkirchik Formation, northern Tarim Basin
- Usability of PPGIS tools exemplified by geodiscussion – a tool for public participation in shaping public space
- Efficient development technology of Upper Paleozoic Lower Shihezi tight sandstone gas reservoir in northeastern Ordos Basin
- Assessment of soil resources of agricultural landscapes in Turkestan region of the Republic of Kazakhstan based on agrochemical indexes
- Evaluating the impact of DEM interpolation algorithms on relief index for soil resource management
- Petrogenetic relationship between plutonic and subvolcanic rocks in the Jurassic Shuikoushan complex, South China
- A novel workflow for shale lithology identification – A case study in the Gulong Depression, Songliao Basin, China
- Characteristics and main controlling factors of dolomite reservoirs in Fei-3 Member of Feixianguan Formation of Lower Triassic, Puguang area
- Impact of high-speed railway network on county-level accessibility and economic linkage in Jiangxi Province, China: A spatio-temporal data analysis
- Estimation model of wild fractional vegetation cover based on RGB vegetation index and its application
- Lithofacies, petrography, and geochemistry of the Lamphun oceanic plate stratigraphy: As a record of the subduction history of Paleo-Tethys in Chiang Mai-Chiang Rai Suture Zone of Thailand
- Structural features and tectonic activity of the Weihe Fault, central China
- Application of the wavelet transform and Hilbert–Huang transform in stratigraphic sequence division of Jurassic Shaximiao Formation in Southwest Sichuan Basin
- Structural detachment influences the shale gas preservation in the Wufeng-Longmaxi Formation, Northern Guizhou Province
- Distribution law of Chang 7 Member tight oil in the western Ordos Basin based on geological, logging and numerical simulation techniques
- Evaluation of alteration in the geothermal province west of Cappadocia, Türkiye: Mineralogical, petrographical, geochemical, and remote sensing data
- Numerical modeling of site response at large strains with simplified nonlinear models: Application to Lotung seismic array
- Quantitative characterization of granite failure intensity under dynamic disturbance from energy standpoint
- Characteristics of debris flow dynamics and prediction of the hazardous area in Bangou Village, Yanqing District, Beijing, China
- Rockfall mapping and susceptibility evaluation based on UAV high-resolution imagery and support vector machine method
- Statistical comparison analysis of different real-time kinematic methods for the development of photogrammetric products: CORS-RTK, CORS-RTK + PPK, RTK-DRTK2, and RTK + DRTK2 + GCP
- Hydrogeological mapping of fracture networks using earth observation data to improve rainfall–runoff modeling in arid mountains, Saudi Arabia
- Petrography and geochemistry of pegmatite and leucogranite of Ntega-Marangara area, Burundi, in relation to rare metal mineralisation
- Prediction of formation fracture pressure based on reinforcement learning and XGBoost
- Hazard zonation for potential earthquake-induced landslide in the eastern East Kunlun fault zone
- Monitoring water infiltration in multiple layers of sandstone coal mining model with cracks using ERT
- Study of the patterns of ice lake variation and the factors influencing these changes in the western Nyingchi area
- Productive conservation at the landslide prone area under the threat of rapid land cover changes
- Sedimentary processes and patterns in deposits corresponding to freshwater lake-facies of hyperpycnal flow – An experimental study based on flume depositional simulations
- Study on time-dependent injectability evaluation of mudstone considering the self-healing effect
- Detection of objects with diverse geometric shapes in GPR images using deep-learning methods
- Behavior of trace metals in sedimentary cores from marine and lacustrine environments in Algeria
- Spatiotemporal variation pattern and spatial coupling relationship between NDVI and LST in Mu Us Sandy Land
- Formation mechanism and oil-bearing properties of gravity flow sand body of Chang 63 sub-member of Yanchang Formation in Huaqing area, Ordos Basin
- Diagenesis of marine-continental transitional shale from the Upper Permian Longtan Formation in southern Sichuan Basin, China
- Vertical high-velocity structures and seismic activity in western Shandong Rise, China: Case study inspired by double-difference seismic tomography
- Spatial coupling relationship between metamorphic core complex and gold deposits: Constraints from geophysical electromagnetics
- Disparities in the geospatial allocation of public facilities from the perspective of living circles
- Research on spatial correlation structure of war heritage based on field theory. A case study of Jinzhai County, China
- Formation mechanisms of Qiaoba-Zhongdu Danxia landforms in southwestern Sichuan Province, China
- Magnetic data interpretation: Implication for structure and hydrocarbon potentiality at Delta Wadi Diit, Southeastern Egypt
- Deeply buried clastic rock diagenesis evolution mechanism of Dongdaohaizi sag in the center of Junggar fault basin, Northwest China
- Application of LS-RAPID to simulate the motion of two contrasting landslides triggered by earthquakes
- The new insight of tectonic setting in Sunda–Banda transition zone using tomography seismic. Case study: 7.1 M deep earthquake 29 August 2023
- The critical role of c and φ in ensuring stability: A study on rockfill dams
- Evidence of late quaternary activity of the Weining-Shuicheng Fault in Guizhou, China
- Extreme hydroclimatic events and response of vegetation in the eastern QTP since 10 ka
- Spatial–temporal effect of sea–land gradient on landscape pattern and ecological risk in the coastal zone: A case study of Dalian City
- Study on the influence mechanism of land use on carbon storage under multiple scenarios: A case study of Wenzhou
- A new method for identifying reservoir fluid properties based on well logging data: A case study from PL block of Bohai Bay Basin, North China
- Comparison between thermal models across the Middle Magdalena Valley, Eastern Cordillera, and Eastern Llanos basins in Colombia
- Mineralogical and elemental analysis of Kazakh coals from three mines: Preliminary insights from mode of occurrence to environmental impacts
- Chlorite-induced porosity evolution in multi-source tight sandstone reservoirs: A case study of the Shaximiao Formation in western Sichuan Basin
- Predicting stability factors for rotational failures in earth slopes and embankments using artificial intelligence techniques
- Origin of Late Cretaceous A-type granitoids in South China: Response to the rollback and retreat of the Paleo-Pacific plate
- Modification of dolomitization on reservoir spaces in reef–shoal complex: A case study of Permian Changxing Formation, Sichuan Basin, SW China
- Geological characteristics of the Daduhe gold belt, western Sichuan, China: Implications for exploration
- Rock physics model for deep coal-bed methane reservoir based on equivalent medium theory: A case study of Carboniferous-Permian in Eastern Ordos Basin
- Enhancing the total-field magnetic anomaly using the normalized source strength
- Shear wave velocity profiling of Riyadh City, Saudi Arabia, utilizing the multi-channel analysis of surface waves method
- Effect of coal facies on pore structure heterogeneity of coal measures: Quantitative characterization and comparative study
- Inversion method of organic matter content of different types of soils in black soil area based on hyperspectral indices
- Detection of seepage zones in artificial levees: A case study at the Körös River, Hungary
- Tight sandstone fluid detection technology based on multi-wave seismic data
- Characteristics and control techniques of soft rock tunnel lining cracks in high geo-stress environments: Case study of Wushaoling tunnel group
- Influence of pore structure characteristics on the Permian Shan-1 reservoir in Longdong, Southwest Ordos Basin, China
- Study on sedimentary model of Shanxi Formation – Lower Shihezi Formation in Da 17 well area of Daniudi gas field, Ordos Basin
- Multi-scenario territorial spatial simulation and dynamic changes: A case study of Jilin Province in China from 1985 to 2030
- Review Articles
- Major ascidian species with negative impacts on bivalve aquaculture: Current knowledge and future research aims
- Prediction and assessment of meteorological drought in southwest China using long short-term memory model
- Communication
- Essential questions in earth and geosciences according to large language models
- Erratum
- Erratum to “Random forest and artificial neural network-based tsunami forests classification using data fusion of Sentinel-2 and Airbus Vision-1 satellites: A case study of Garhi Chandan, Pakistan”
- Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part I
- Spatial-temporal and trend analysis of traffic accidents in AP Vojvodina (North Serbia)
- Exploring environmental awareness, knowledge, and safety: A comparative study among students in Montenegro and North Macedonia
- Determinants influencing tourists’ willingness to visit Türkiye – Impact of earthquake hazards on Serbian visitors’ preferences
- Application of remote sensing in monitoring land degradation: A case study of Stanari municipality (Bosnia and Herzegovina)
- Optimizing agricultural land use: A GIS-based assessment of suitability in the Sana River Basin, Bosnia and Herzegovina
- Assessing risk-prone areas in the Kratovska Reka catchment (North Macedonia) by integrating advanced geospatial analytics and flash flood potential index
- Analysis of the intensity of erosive processes and state of vegetation cover in the zone of influence of the Kolubara Mining Basin
- GIS-based spatial modeling of landslide susceptibility using BWM-LSI: A case study – city of Smederevo (Serbia)
- Geospatial modeling of wildfire susceptibility on a national scale in Montenegro: A comparative evaluation of F-AHP and FR methodologies
- Geosite assessment as the first step for the development of canyoning activities in North Montenegro
- Urban geoheritage and degradation risk assessment of the Sokograd fortress (Sokobanja, Eastern Serbia)
- Multi-hazard modeling of erosion and landslide susceptibility at the national scale in the example of North Macedonia
- Understanding seismic hazard resilience in Montenegro: A qualitative analysis of community preparedness and response capabilities
- Forest soil CO2 emission in Quercus robur level II monitoring site
- Characterization of glomalin proteins in soil: A potential indicator of erosion intensity
- Power of Terroir: Case study of Grašac at the Fruška Gora wine region (North Serbia)
- Special Issue: Geospatial and Environmental Dynamics - Part I
- Qualitative insights into cultural heritage protection in Serbia: Addressing legal and institutional gaps for disaster risk resilience