Startseite Analysis of urban expansion patterns in the Yangtze River Delta based on the fusion impervious surfaces dataset
Artikel Open Access

Analysis of urban expansion patterns in the Yangtze River Delta based on the fusion impervious surfaces dataset

  • Cuiheng Ye , Jie Jiang EMAIL logo , Lei Li und Yan Jin
Veröffentlicht/Copyright: 12. September 2025
Veröffentlichen auch Sie bei De Gruyter Brill

Abstract

The Yangtze River Delta (YRD) is a highly urbanized region. Understanding the spatial and temporal dynamics of urban land expansion in the YRD is essential for optimizing the distribution of urban clusters and promoting balanced regional development. Existing 30 m global impervious surfaces (IS) datasets are hampered by significant accuracy discrepancies and uncertainties stemming from inconsistent methodologies. Therefore, the Dempster–Shafer (D-S) evidence theory was used to fuse three datasets of the China Land Cover Dataset, Global Land Cover product with Fine Classification System at 30 m, and Global Impervious Surface Area, to analyze the urban land expansion in the YRD from 1985 to 2020. The results indicate that: (1) The fused dataset achieved an overall accuracy of 98.26% and a kappa coefficient of 0.965, notably higher than those of the individual datasets. (2) Urban land expansion in the YRD exhibited distinct phases: slow growth, rapid growth, and rapid decline. The early expansion was more intense in the southern YRD. Later, the northern region expansion accelerated, shifting the development center northward. (3) The urban development pattern of the YRD was predominantly characterized by edge expansion, with the proportion of infilling gradually increasing. Long-term and high-precision data on IS provide a comprehensive understanding of the development patterns of regional urban clusters. The D-S evidence theory enhances the accuracy of IS dataset, serving as a foundation for planning and promoting high-quality urban development.

1 Introduction

The spatial expansion of impervious surfaces (IS) is a critical indicator of urbanization and changes in land use patterns [1,2]. Since the initiation of reform and opening up, China’s urbanization has proceeded at an unprecedented rate, with its urban growth significantly outpacing that of other nations [3,4]. This rapid extension of urban land use has stimulated population migration, capital inflow, and industrial agglomeration [5,6]. However, it has also resulted in uncontrolled land use growth, urban sprawl, inefficient utilization of land resources [7,8], severe traffic congestion, and ecological degradation [9,10,11,12]. As a primary material manifestation of urbanization processes, understanding the spatiotemporal characteristics of urban land expansion is essential for grasping the overall trajectory of urbanization and formulating effective regional development policies [13].

Most research on the pattern and characteristics of urban spatial expansion has primarily focused on spatial morphology, structure, and configuration [14,15,16]. Metrics such as the morphological compactness index [17,18], global and local spatial autocorrelation [19,20,21], landscape expansion index [22,23,24], landscape pattern index [25,26,27,28,29], along with orientation comparison and grid cell analysis methods [30], have been employed to evaluate the spatial concentration, diffusion, and expansion patterns of urban areas. Spanning scales from metropolitan areas to urban agglomerations, these studies typically employ remote sensing to analyze land cover change and IS dynamics [31,32]. Since its launch in 1972, the Landsat satellite has provided high temporal and spatial resolution imagery, serving as an ideal platform for monitoring extensive land cover changes and IS data [33,34,35,36].

In recent years, China has released several sets of 30 m land cover products, such as China’s National Land Use and Cover Change dataset produced by the Center for Geoscience and Resources of the Chinese Academy of Sciences [37], Global Land Cover Mapping at 30 m Resolution (GlobeLand30) from the National Center for Basic Geographic Information, the Finer Resolution Observation and Monitoring of Global Land Cover by Tsinghua University, the China Land Cover Dataset (CLCD) by Wuhan University, and the Global 30 m Land Cover Classification with a Fine Classification System (GLC_FCS30) by the Institute of Innovative Research in Air and Space Information of the Chinese Academy of Sciences [38]. These land cover datasets have significantly enhanced the understanding of urban spatial expansion patterns. In 2015, the Joint Research Center (JRC) published the Global Human Settlement Layer (GHSL), which is one of the earliest high-resolution (30 m) global IS products based on Landsat imagery and covers the years 1975, 1990, 2000, and 2014. Subsequently, the Global Annual Urban Dynamics dataset was developed to map urban changes at a 30 m resolution from 1985 to 2015 [39], and the Global Artificial Impervious Areas dataset was created to assess annual dynamics of urban IS from 1985 to 2018 [40]. Recently, the JRC issued an updated GHSL dataset that provides a probabilistic imperviousness grid for 2018 [41]. Additionally, the Global Impervious Surface Area (GISA) dataset divided the global land surface into 1,221 cells, and a unique random forest model was trained for each one to produce annual products from 1985 onward [42].

Despite the availability of numerous 30 m resolution global IS datasets, substantial discrepancies in their accuracy stem from inconsistencies in training samples, classification methodologies, post-processing techniques, and accuracy evaluations. This study employed the D-S evidence theory to integrate the CLCD, GLC_FCS30, and GISA datasets, thereby generating high-precision IS data for the YRD spanning 1985–2020. Subsequent analysis revealed the intensity, differences, and patterns of urban land expansion within the YRD region.

2 Materials and methods

2.1 Study area

The YRD region is a pivotal intersection of the Belt and Road Initiative and the Yangtze River Economic Belt (Figure 1), playing a critical strategic role in China’s national modernization and development [43]. It is distinguished by a high level of urbanization, densely populated built-up areas, a vibrant economy, efficient transportation networks, and advanced infrastructure [44]. As the largest and most developed urban cluster in China, the YRD not only propels economic and social progress but also functions as a vital platform for international cooperation. Geographically, the YRD is characterized by a typical river-mouth alluvial plain topography, with predominantly flat terrain covering approximately 83.7% of the total area. North of the Yangtze River, the terrain is primarily plain, while south of the river, it is predominantly hilly. Notably, Zhejiang Province exhibits complex topography, with over 70% of its land classified as mountainous or hilly. In contrast, Shanghai consists entirely of the alluvial plain formed by the YRD. Climatically, the YRD experiences a subtropical monsoon climate, marked by hot and humid summers, as well as mild and rainy winters.

Figure 1 
                  Map of land cover and urban expansion in the YRD. The YRD includes Jiangsu Province, Zhejiang Province, Anhui Province, and Shanghai Municipality, with Jiangsu Province including Nanjing, Wuxi, Xuzhou, Changzhou, Suzhou, Nantong, Lianyungang, Huai’an, Yancheng, Yangzhou, Zhenjiang, Taizhou, and Suqian; Zhejiang Province includes Hangzhou, Ningbo, Wenzhou, Jiaxing, Huzhou, Shaoxing, Jinhua, Quzhou, Zhoushan, Taizhou, and Lishui; Anhui Province includes Hefei, Huaibei, Bozhou, Susong, Bengbu, Fuyang, Huainan, Chuzhou, Lu’an, Anqing, and Huangshan.
Figure 1

Map of land cover and urban expansion in the YRD. The YRD includes Jiangsu Province, Zhejiang Province, Anhui Province, and Shanghai Municipality, with Jiangsu Province including Nanjing, Wuxi, Xuzhou, Changzhou, Suzhou, Nantong, Lianyungang, Huai’an, Yancheng, Yangzhou, Zhenjiang, Taizhou, and Suqian; Zhejiang Province includes Hangzhou, Ningbo, Wenzhou, Jiaxing, Huzhou, Shaoxing, Jinhua, Quzhou, Zhoushan, Taizhou, and Lishui; Anhui Province includes Hefei, Huaibei, Bozhou, Susong, Bengbu, Fuyang, Huainan, Chuzhou, Lu’an, Anqing, and Huangshan.

2.2 Land cover and IS dataset

The IS datasets utilized in the study include CLCD, GLC_FCS30, and GISA. The CLCD is an annual land cover dataset derived from Landsat imagery, offering 30 m land use analysis specific to China over a three-decade time series. GLC_FCS30 represents the first global fine-scale land cover dataset at 30 m resolution generated through continuous change detection methods, encompassing 35 refined classifications spanning from 1985 to 2022. This dataset integrates a dense time series produced from Landsat imagery via continuous change detection, local adaptive update models, and spatiotemporal optimization algorithms, achieving an accuracy of approximately 80%. GISA provides global IS maps dating back to 1985, characterized by both a long temporal span and high accuracy due to its extensive set of randomly selected validation samples obtained from third-party data. Furthermore, it introduces a novel global IS mapping method that combines semi-automatic sample collection, local adaptive classification strategies, and spatiotemporal post-processing procedures to effectively extract IS.

The validation dataset adopted the multi-temporal IS validation dataset in YRD [45]. This dataset collects 3,845 validation samples based on high-resolution images on Google Earth, including 2,160 non-impervious surfaces (NIS) samples and 1,685 IS samples spanning from 1985 to 2020.

2.3 Data fusion method

The fusion problems in the D-S evidence theory are tackled within the recognition framework U, which is a non-empty set comprising a series of mutually exclusive elements A, and the power set of this recognition framework contains a total of 2U elements. All objectives in the problem domain involve set functions m: 2U → [0, 1] that satisfy

(1) m ( ) = 0 ,

(2) A U m ( A ) = 1 ,

where m represents the Basic probability assignment (BPA) function for the recognition framework U. m(A) denotes the BPA for the proposition A, reflecting the degree of support for its occurrence. Equation (1) specifies that the BPA for the empty set is zero. Equation (2) indicates that the total confidence assigned to all propositions within the recognition framework sums to 1, despite each proposition having its distinct level of confidence.

Different sources of evidence m 1 , m 2 , m n have distinct BPA functions. The D-S synthesis formula utilizes orthogonal sums to combine these individual BPA functions into a new function. This formula is expressed as follows:

(3) m ( A ) = 1 1 k A 1 A 2 A 3 = A m 1 ( A ) m 2 ( A ) m n ( A ) ,

(4) k = A 1 A 2 A 3 = m 1 ( A ) m 2 ( A ) m n ( A ) ,

where k is defined as the conflict coefficient. A conflict coefficient (k) nearing 1 indicates higher degree of conflict among the evidence sources, while k tending toward 0 signifies greater consistency among them. The term 1 1 K serves as a normalization factor, ensuring that data fusion does not assign confidence to the empty set.

In the study, the BPA values for the classification of IS vs NIS were first determined by calculating the confusion matrix for each dataset. Then, equation (3) was implemented to fuse the evidence from the three datasets at a pixel level, which generated a composite belief for the classification of each pixel. Prior to fusion, a consistency analysis of the three types of land cover data was performed. Based on the spatial consistency analysis results, if the land cover types from all three datasets or two of them are consistent, the land cover type of the pixel was defined accordingly. In contrast, if each dataset suggests a different type of land cover for the same pixel, a standard fusion process was applied. When the belief assigned to the “impervious surfaces” class for a given pixel was maximal, it was designated as an impervious pixel, facilitating the final extraction of urban regions.

2.4 Urban expansion intensity index (UEII)and urban expansion differentiation index (UEDI)

UEII indicates the rate of change in urban land area over a specified period, reflecting both the speed and magnitude of increases or decreases in urban land extent. Its calculation formula is presented in equation (5).

(5) UE I I i = U i t 2 U i t 1 U i t 1 × Δ t ,

where U i t 2 and U i t 1 are the urban land area of the city i at time t 2 and t 1 , Δ t is the period of the study. The urban area was extracted based on IS data following the methodology [24,46].

The UEDI represents the ratio of a city’s urban land expansion rate to the overall urban land expansion rate within the study area. This index quantifies the relative dynamics of urban land development in a specific city compared to the entire study region. By providing a standardized quantitative measure, UEDI enables more precise and comparable assessments of urban land expansion rates across different cities. Furthermore, it reflects the coordinated development and relative progress of urban expansion among cities within the region, which is essential for analyzing spatial distribution and dynamic evolution patterns. The calculation formula for UEDI is presented in equation (6).

(6) UEDI i = | U i t 2 U i t 1 | × U t 1 | U t 2 U t 1 | × U i t 1 ,

where U t 2 and U t 1 are the urban land areas of the study area at times t 2 and t 1 .

2.5 Type of urban expansion

The urban expansion type is classified into three forms: enclave expansion, infilling expansion, and edge expansion [47]. Enclave expansion represents a prevalent form of urban growth during the urbanization process, characterized by the transformation of rural and other non-urban areas into urban land through development activities. In contrast, infilling expansion primarily occurs in contexts of intensive land use, where previously developed but underutilized areas within the city are redeveloped. Edge expansion refers to the outward growth of urban areas as cities expand their boundaries. The formula [48] for calculating urban expansion type T is presented as follows:

(7) T = C L P ,

where L P represents the perimeter of a newly developed urban patch, and C is the length of the common boundary of this newly developed urban patch and the existing urban land. The urban expansion type is identified as enclave expansion when T = 0, as edge expansion when 0 < T ≤ 0.5, and as infilling expansion when T > 0.5. The steps of the study are shown in Figure 2.

Figure 2 
                  The flowchart of the study.
Figure 2

The flowchart of the study.

3 Results

3.1 Accuracy of fused IS datasets

The accuracy of the fusion dataset and the three datasets of the CLCD, GLC_FCS30, and GISA in the YRD are presented in Table 1. Among the 3,845 randomly sampled points, 2,160 were classified as NIS, and 1,685 as IS. For the CLCD dataset, 38 NIS points were incorrectly classified as impervious, resulting in a misclassification rate of 1.76%. Conversely, there were 374 instances where IS were misclassified, leading to a significantly higher misclassification rate of 22.2%. For GLC_FCS30, only 11 NIS points were incorrectly classified as impervious, with a misclassification rate of 0.51%, whereas 249 IS points were misclassified, yielding a rate of 14.78%. Although this was lower than that observed in CLCD, it remained considerably higher than the misclassification rate for NIS. By contrast, GISA demonstrated superior performance with only 9 instances of NIS being misclassified as impervious (a rate of 0.41%) and a total of 77 IS points misclassified, corresponding to a misclassification rate of 4.57%. Among the three datasets analyzed, GISA exhibited the lowest proportion of misclassified IS compared to the CLCD and GLC_FCS30 datasets.

Table 1

Confusion matrix of CLCD, GLC_FCS30, GISA, and fusion data

CLCD GLC_FCS30 GISA Fusion data
/ NIS IS UA (%) NIS IS UA (%) NIS IS UA (%) NIS IS UA (%)
NIS 2,122 38 98.2 2,149 11 99.4 2,151 9 99.58 2,148 12 99.44
IS 374 1,311 77.8 249 1,436 85.2 77 1,608 95.43 55 1,630 96.74
PA (%) 85.02 97.18 89.62 99.24 96.54 99.44 97.5 99.27 98.261

Note: NIS is non-impervious surfaces, IS is impervious surfaces, PA is producer’s accuracy, UA is user’s accuracy. 1 is the OA of the fusion dataset.

The fusion dataset revealed that 12 NIS points had been inaccurately classified (0.56%), while 55 IS points were misclassified at a rate of 3.26%, which was notably lower than other datasets. Table 2 illustrates the overall accuracy (OA) and kappa coefficient for all datasets. Specifically, CLCD demonstrated the lowest classification efficacy, attaining an OA of 0.893 and a kappa coefficient of 0.777. In contrast, GLC_FCS30 exhibited moderate improvement with an OA of 0.932. Notably, GISA outperformed all initial datasets, achieving an OA of 0.978 and a kappa coefficient of 0.954. The fusion dataset realized the highest results, reaching an OA of 0.983 and a kappa coefficient of 0.965.

Table 2

Overall accuracy and kappa coefficient of CLCD, GLC_FCS30, GISA, and fusion data

OA (%) Kappa
CLCD 89.28 0.777
GLC_FCS30 93.24 0.860
GISA 97.76 0.954
Fusion data 98.26 0.965

Among the 374 misclassified sample points in the CLCD dataset, 362 were identified as cropland, 6 as grassland, 5 as woodland, and 1 as waterbody. Similarly, among the 249 misclassified points in the GLC_FCS30, 236 were categorized as cropland. The complexity of land use types, the diversity of crop species, and variations in crop growth stages result in significant variability in the spectral characteristics of cropland observed in remote sensing imagery, leading to pronounced hetero spectral phenomena that complicate feature extraction. Furthermore, urbanization transitions from natural to artificial surfaces often involve complex surface compositions, further exacerbating classification uncertainty. The fusion of multiple datasets can substantially improve the accuracy of IS classification.

To investigate and elucidate the performance advantages of D-S evidence theory in data fusion, the study conducted a comparative analysis of several mainstream fusion strategies (Table 3) [49,50,51,52]. The D-S evidence theory significantly outperformed alternative fusion methods, yielding an outstanding OA of 98.26% even when relying on lower-resolution data.

Table 3

Comparison of the accuracy of different fusion methods

Method Datasets Resolution (m) OA (%)
D-S evidence theory (our study) CLCD, GLC_FCS30, and GISA 30 98.26
D-S evidence theory [49] GF-1 and SAR (Sentinel-1A) 16 95.33
Random forest [50] SPOT-5 and SAR (TerraSAR-X) 10 98.44
Random forest [50] Landsat ETM + and SAR (ASAR) 30 93.72
Object-based fuzzy classification [51] IKONOS 1 94.50
Adaptive reweighting and combining [52] RapidEye 5 95.32

3.2 Temporal evolution in urban land expansion intensity

The intensity of urban land expansion in the YRD exhibited distinct stages (Figure 3), following a trend characterized by Slow Growth, Rapid Growth, and subsequent Rapid Decline. The UEII gradually increased from 0.065 to 0.091 between 1985 and 2000, peaking at 0.132 during the period from 2000 to 2005. Subsequently, it declined to 0.041 from 2015 to 2020, indicating that the YRD urban agglomeration is progressively transitioning towards more coordinated and synergistic development.

Figure 3 
                  The overall UEII in the YRD from 1985 to 2020.
Figure 3

The overall UEII in the YRD from 1985 to 2020.

Between 1985 and 2020, urban land areas in various cities exhibited continuous growth, though expansion intensity varied significantly across development stages. The temporal trend of the UEII for most regions in Zhejiang Province and Suzhou, Wuxi, and Changzhou in Jiangsu Province, as well as Shanghai, aligned with the overall trajectory of the YRD, peaking between 2000 and 2005. Notably, Jinhua recorded a UEII of 0.323, while Suzhou approached 0.3. In contrast, the UEII growth rate in northern Jiangsu and much of Anhui was relatively subdued, reaching its maximum value between 2005 and 2010. Xuancheng (Anhui) recorded a peak UEII of 0.522 during this period. Additionally, Yancheng, Bengbu, Chuzhou, and Fuyang attained their highest values between 2010 and 2015, while Wenzhou peaked earlier from 1995 to 2000. Overall, Jinhua demonstrated the highest expansion intensity at an impressive rate of 1.404%, followed by Shaoxing, Huzhou, and Suzhou.

The southern YRD, particularly the southeastern region, has demonstrated a higher rate of development compared to the northern area (Figure 4). Over time, the development rate in the north has begun to increase, gradually shifting the center of regional growth northward. Between 1985 and 1990, urban expansion across the YRD was relatively uniform, as evidenced by low UEII levels, with most regions reporting UEIIs below 0.1. Jinhua stood out with the highest UEII (0.171) and UEDI (2.645), primarily due to administrative adjustments. From 1990 to 2005, significant disparities in urban expansion became evident across the region, with the southeast exhibiting markedly higher UEII than those in the north. Jinhua and Shaoxing in Zhejiang Province reported UEDI exceeding 2, reflecting nearly a tenfold increase in urban area during this period. Between 2000 and 2005, the north-south disparity in urban expansion within the YRD became increasingly pronounced. In the northwestern area, only Hefei exhibited a UEDI of 0.810, while the other cities in this region reported UEDI values below 0.750. Conversely, in the southeastern area encompassing Jinhua, Shaoxing, and Suzhou, all cities recorded UEDI values exceeding 2. Additionally, most other cities had UEDI scores above 1, indicating a significant trend of urban expansion. For instance, Suzhou’s UEDI increased by nearly 1.5 times during this period. Between 2010 and 2015, the UEDI for Fuyang and Lu’an in the northwestern region of the YRD exceeded 2.0, whereas the UEDI for Shanghai and its surrounding cities was comparatively lower. Notably, Wuxi recorded a minimum value of 0.469.

Figure 4 
                  The UEDI in the YRD from 1985 to 2020. (a) 1985–1990, (b) 1990–1995, (c) 1995–2000, (d) 2000–2005, (e) 2005–2010, (f) 2010–2015, (g) 2015–2020, and (h) 1985–2020.
Figure 4

The UEDI in the YRD from 1985 to 2020. (a) 1985–1990, (b) 1990–1995, (c) 1995–2000, (d) 2000–2005, (e) 2005–2010, (f) 2010–2015, (g) 2015–2020, and (h) 1985–2020.

3.3 Analysis of urban development patterns

From 1985 to 2020, urban land expansion in the YRD was primarily characterized by edge expansion (Figure 5), accounting for approximately 74.7% of the total expansion. Enclave expansion constituted about 19.6%, while infilling expansion was minimal at only 5.6%. During the period from 1985 to 2000, infilling expansion remained low, particularly between 1985 and 1990 when it was less than 1%. However, after 2000, edge expansion began to decline, while the proportion of infilling expansion gradually increased. By 2015–2020, infilling expansion had risen to approximately 16.33%. A significant shift was observed in Shanghai between 2000 and 2005, where edge expansion accounted for approximately 85%, while infilling expansion was only 3.5%. However, by 2015–2020, edge expansion decreased to around 51%, while infilling expansion surged to approximately 38.4%, marking a substantial increase.

Figure 5 
                  The proportional composition of the three urban expansion types in the YRD. Each dot represents a city, with its size indicating the scale of urban expansion. (a) 1985–1990, (b) 1990–1995, (c) 1995–2000, (d) 2000–2005, (e) 2005–2010, (f) 2010–2015, and (g) 2015–2020.
Figure 5

The proportional composition of the three urban expansion types in the YRD. Each dot represents a city, with its size indicating the scale of urban expansion. (a) 1985–1990, (b) 1990–1995, (c) 1995–2000, (d) 2000–2005, (e) 2005–2010, (f) 2010–2015, and (g) 2015–2020.

To analyze the trends in urban spatial expansion types within the YRD from 1985 to 2020, Ward’s Euclidean squared distance clustering method based on the proportions of each city’s expansion types was employed. The analysis resulted in three categories: Category I represents a transition toward spatial agglomeration, characterized by a rapid decline in enclave expansion to below 10%, while edge expansion also experiences a slight decrease, remaining below 65%. Conversely, infilling type growth accelerates quickly to reach 25%, indicating a shift toward connotative development. Notable cities in this category include Shanghai, Nanjing, Hangzhou, Suzhou (Jiangsu), Wuxi, Zhenjiang, Shaoxing, and Jinhua. Category II is defined by rapid spatial growth, where the proportion of enclave expansion slightly decreases but remains elevated at above 20%. These cities continue to experience rapid outward growth with spatial diffusion still prevailing, suggesting that significant distances remain before achieving urban spatial agglomeration. Representative cities include Xuzhou, Nantong, Suzhou (Anhui), Wenzhou, Zhoushan, Wuhu, Chuzhou, Chizhou, and Xuancheng. Category III pertains to edge-expanding cities where enclave proportions decline slightly to below 15%, while edge expansions rise significantly to approximately 70%. The infilling type also shows a minor reduction to under 15%, indicating that edge expansion is the predominant mode of development. Representative cities in this category include Yancheng, Hefei, Anqing, and Taizhou; these areas continue their outward spread, reflecting an absence of intensive and compact urban development.

4 Discussion

4.1 Interpretation of spatiotemporal dynamics and driving Forces

The spatiotemporal dynamics of urban expansion revealed in the study – characterized by a region-wide structural transition from dispersed leapfrog growth to consolidated edge-expansion and infilling – not only corroborate the established “diffusion-coalescence” theoretical framework [53] but also reflect the spatial manifestation of a convergence of powerful driving forces at work over the past three decades. This observed trajectory, including the conspicuous northward shift of the developmental center of gravity [54], is not a random phenomenon but rather the geographical expression of intricate interactions among economic, demographic, and political-institutional forces. Robust economic expansion, fueled by capital accumulation, generated significant demand for industrial, commercial, and residential land, serving as the foundational impetus [55]. Concurrently, demographic pressures, intensified by large-scale rural-to-urban migration, gave rise to a self-reinforcing feedback loop between population aggregation and territorial expansion [56].

Foremost among these forces, state policy has played a pivotal role, acting as a decisive mechanism in modulating the pace, scale, and configuration of urban expansion. The “land finance” regime, a central component of local governance, clearly accelerated rapid and often fragmented land development during the earlier stages [57]. The more recent deceleration of expansion rates and the increasing prevalence of infilling patterns also correspond to a broader shift in national macro-planning, which has pivoted from prioritizing sheer growth to championing ecological civilization and high-quality development [58]. This policy-driven evolution suggests that the YRD’s experience may serve as a precursor to the trajectories of other urbanizing regions in China [57]. Moreover, top-down regional integration strategies have directly promoted the functional decentralization of core cities, thereby contributing to the observed geographical shift in development focus [56]. Therefore, the YRD’s urban expansion is a contingent outcome shaped by the interplay between market dynamics and state regulation, with its historical evolution reflecting the dynamic interplay and changing dominance of these driving forces.

4.2 High-precision impervious surface mapping challenges and policy applications

A rigorous academic inquiry necessitates a critical appraisal of the study’s limitations, which highlight essential directions for future research. Methodologically, while the D-S theory produced high-performance results, its inherent constraints in managing high-conflict evidence and the potential subjectivity in BPA call for a systematic comparative evaluation against other advanced fusion algorithms, such as ensemble learning, modified D-S rules, or deep learning-based fusion networks [59]. Regarding data resolution, the 30 m resolution, while effective for macroscopic pattern detection, inherently limits the capacity to resolve fine-grained intra-urban textural details. Future investigations would be substantially enriched by integrating higher-resolution remote sensing data (e.g., from Sentinel or Gaofen series). Finally, the predominantly qualitative assessment of driving forces should be replaced by quantitative, spatially explicit modeling approaches, enabling a more rigorous analysis of the spatially heterogeneous impacts of diverse drivers [60].

Notwithstanding the methodological considerations, the high-precision IS area dataset generated herein offers substantial scientific value and broad policy relevance. For urban planners and local governments, the dataset can provide critical support for more accurate urban growth forecasting, evaluating the effectiveness of existing plans, and optimizing future land-use configurations and infrastructure allocation, thereby fostering a transition towards more compact and efficient urban development models. For regional development and environmental protection agencies, the expansion patterns and shifts in the center of gravity revealed herein can inform the formulation of more targeted regional coordination policies and ecological conservation strategies, such as defining urban growth boundaries and protecting critical ecological spaces. Additionally, this dataset can serve as a foundational data layer for researchers investigating the urban heat island effect, changes in biodiversity, carbon cycling, and other environmental and socioeconomic consequences of urbanization, thus facilitating deeper interdisciplinary investigations.

5 Conclusion

Since the 1990s, the urban land in the YRD region has experienced rapid expansion. A key challenge for the integrated development of the YRD is guiding the sustainable development of urban land while improving the quality of urban growth. Using the fused IS data based on D-S evidence theory, changes in urban land in the YRD urban agglomeration were examined across three dimensions: urban land expansion intensity, urban expansion difference index, and urban expansion patterns. The results show that

  1. Cropland was the most common feature misclassified as IS, the dataset fused by D-S evidence theory achieved an OA of 98.26% and a kappa coefficient of 0.965, both notably higher than those of the CLCD, GLC_FCS30, and GISA datasets.

  2. The intensity of urban land expansion in the YRD exhibited distinct phase characteristics: slow growth, rapid growth, and rapid decline. Early urban expansion was more intense in the southern YRD, particularly in the southeast area. Over time, the expansion of the northern region accelerated, and the center of regional development gradually shifted towards the north.

  3. The urban development pattern of the YRD was predominantly characterized by edge expansion, with the proportion of infilling gradually increasing. Urban expansion can be categorized into three types: spatial aggregation, rapid spatial growth, and edge expansion dominance.

Acknowledgments

The authors are grateful for the reviewer’s valuable comments that improved the manuscript.

  1. Funding information: This work was supported by the National Natural Science Foundation of China under Grants 42001332.

  2. Author contributions: All authors have accepted responsibility for the entire content of this manuscript and consented to its submission to the journal, reviewed all the results, and approved the final version of the manuscript. J.J. and J.Y. contributed to the study conception and design. Material preparation, data collection, and analysis were performed by Y.C.H. and L.L. The first draft of the manuscript was written by Y.C.H., L.L., and J.J.

  3. Conflict of interest: Authors state no conflict of interest.

References

[1] Arnold CL Jr, Gibbons CJ. Impervious surface coverage: The emergence of a key environmental indicator. J Am Plan Assoc. 1996;62:243–58.10.1080/01944369608975688Suche in Google Scholar

[2] Hu M, Ye C, Gu M, Xiao W, Hu H, Dong Q. Slowing the expansion of impervious surfaces: the key to promoting high-quality and sustainable regional development. Environ Sci Pollut Res. 2024;31:37574–93.10.1007/s11356-024-33651-wSuche in Google Scholar PubMed

[3] Chen M, Liu W, Lu D. Challenges and the way forward in China’s new-type urbanization. Land Use Policy. 2016;55:334–9.10.1016/j.landusepol.2015.07.025Suche in Google Scholar

[4] Xu F, Wang Z, Chi G, Zhang Z. The impacts of population and agglomeration development on land use intensity: New evidence behind urbanization in China. Land Use Policy. 2020;95:104639.10.1016/j.landusepol.2020.104639Suche in Google Scholar

[5] Gabriel SA, Rosenthal SS. Urbanization, agglomeration economies, and access to mortgage credit. Reg Sci Urban Econ. 2013;43:42–50.10.1016/j.regsciurbeco.2012.11.006Suche in Google Scholar

[6] Liu Y, Zhang X, Kong X, Wang R, Chen L. Identifying the relationship between urban land expansion and human activities in the Yangtze River Economic Belt, China. Appl Geogr. 2018;94:163–77.10.1016/j.apgeog.2018.03.016Suche in Google Scholar

[7] Domingo D, Palka G, Hersperger AM. Effect of zoning plans on urban land-use change: A multi-scenario simulation for supporting sustainable urban growth. Sustain Cities Soc. 2021;69:102833.10.1016/j.scs.2021.102833Suche in Google Scholar

[8] Jiao L, Xu Z, Xu G, Zhao R, Liu J, Wang W. Assessment of urban land use efficiency in China: A perspective of scaling law. Habitat Int. 2020;99:102172.10.1016/j.habitatint.2020.102172Suche in Google Scholar

[9] Cheng Z, Hu X. The effects of urbanization and urban sprawl on CO2 emissions in China. Environ Dev Sustain. 2023;25:1792–808.10.1007/s10668-022-02123-xSuche in Google Scholar

[10] Liu X, Huang Y, Xu X, Li X, Li X, Ciais P, et al. High-spatiotemporal-resolution mapping of global urban change from 1985 to 2015. Nat Sustain. 2020;3:564–70.10.1038/s41893-020-0521-xSuche in Google Scholar

[11] Lu J, Li B, Li H, Al-Barakani A. Expansion of city scale, traffic modes, traffic congestion, and air pollution. Cities. 2021;108:102974.10.1016/j.cities.2020.102974Suche in Google Scholar

[12] Mahtta R, Fragkias M, Güneralp B, Mahendra A, Reba M, Wentz EA, et al. Urban land expansion: The role of population and economic growth for 300+ cities. NPJ Urban Sustain. 2022;2:5.10.1038/s42949-022-00048-ySuche in Google Scholar

[13] Azabdaftari A, Sunar F. Predicting urban tomorrow: CA-Markov modeling and district evolution. Earth Sci Inform. 2024;17:3215–32.10.1007/s12145-024-01340-4Suche in Google Scholar

[14] Angel S, Parent J, Civco DL. Ten compactness properties of circles: Measuring shape in geography. Can Geogr/Le Géographe canadien. 2010;54:441–61.10.1111/j.1541-0064.2009.00304.xSuche in Google Scholar

[15] Liu J, Jiao L, Zhang B, Xu G, Yang L, Dong T, et al. New indices to capture the evolution characteristics of urban expansion structure and form. Ecol Indic. 2021;122:107302.10.1016/j.ecolind.2020.107302Suche in Google Scholar

[16] Zhong S, Wang M, Zhu Y, Chen Z, Huang X. Urban expansion and the urban–rural income gap: Empirical evidence from China. Cities. 2022;129:103831.10.1016/j.cities.2022.103831Suche in Google Scholar

[17] Jia Y, Tang L, Xu M, Yang X. Landscape pattern indices for evaluating urban spatial morphology–A case study of Chinese cities. Ecol Indic. 2019;99:27–37.10.1016/j.ecolind.2018.12.007Suche in Google Scholar

[18] Mubareka S, Koomen E, Estreguil C, Lavalle C. Development of a composite index of urban compactness for land use modelling applications. Landsc Urban Plan. 2011;103:303–17.10.1016/j.landurbplan.2011.08.012Suche in Google Scholar

[19] Aljoufie M, Brussel M, Zuidgeest M, Van Maarseveen M. Urban growth and transport infrastructure interaction in Jeddah between 1980 and 2007. Int J Appl Earth Observ Geoinf. 2013;21:493–505.10.1016/j.jag.2012.07.006Suche in Google Scholar

[20] Wang Y. Development characteristics, influencing mechanism and coping strategies of resource-based cities in developing countries: A case study of urban agglomeration in Northeast China. Environ Sci Pollut Res Int. 2022;29:25336–48.10.1007/s11356-021-17820-9Suche in Google Scholar PubMed

[21] Wu Y, Han Z, Koko AF, Zhang S. Spatio-temporal analysis of the driving factors of urban land use expansion in China: A study of the Yangtze River Delta region. Open Geosci. 2024;16:16.10.1515/geo-2022-0609Suche in Google Scholar

[22] Güneralp B, Reba M, Hales BU, Wentz EA, Seto KC. Trends in urban land expansion, density, and land transitions from 1970 to 2010: A global synthesis. Environ Res Lett. 2020;15:044015.10.1088/1748-9326/ab6669Suche in Google Scholar

[23] Liu X, Li X, Chen Y, Tan Z, Li S, Ai B. A new landscape index for quantifying urban expansion using multi-temporal remotely sensed data. Landsc Ecol. 2010;25:671–82.10.1007/s10980-010-9454-5Suche in Google Scholar

[24] Theres L, Radhakrishnan S, Ogwankwa F, Murali G. Determining region of urban expansion based on urban growth pattern and intensity as a driving factor using regression modelling approach in Salem, India. Earth Sci Inform. 2025;18:235.10.1007/s12145-025-01752-wSuche in Google Scholar

[25] Dadashpoor H, Azizi P, Moghadasi M. Land use change, urbanization, and change in landscape pattern in a metropolitan area. Sci Total Environ. 2019;655:707–19.10.1016/j.scitotenv.2018.11.267Suche in Google Scholar PubMed

[26] Inkoom JN, Frank S, Greve K, Walz U, Fürst C. Suitability of different landscape metrics for the assessments of patchy landscapes in West Africa. Ecol Indic. 2018;85:117–27.10.1016/j.ecolind.2017.10.031Suche in Google Scholar

[27] Lustig A, Stouffer DB, Roigé M, Worner SP. Towards more predictable and consistent landscape metrics across spatial scales. Ecol Indic. 2015;57:11–21.10.1016/j.ecolind.2015.03.042Suche in Google Scholar

[28] Schwarz N. Urban form revisited—Selecting indicators for characterising European cities. Landsc Urban Plan. 2010;96:29–47.10.1016/j.landurbplan.2010.01.007Suche in Google Scholar

[29] Ashiagbor G, Amoako C, Asabere SB, Quaye-Ballard JA. Landscape transformations in rapidly developing peri-urban areas of Accra, Ghana: Results of 30 years. Open Geosci. 2019;11:172–82.10.1515/geo-2019-0014Suche in Google Scholar

[30] Frolking S, Mahtta R, Milliman T, Esch T, Seto KC. Global urban structural growth shows a profound shift from spreading out to building up. Nat Cities. 2024;1:555–66.10.1038/s44284-024-00100-1Suche in Google Scholar

[31] Fei W, Zhao S. Urban land expansion in China’s six megacities from 1978 to 2015. Sci Total Environ. 2019;664:60–71.10.1016/j.scitotenv.2019.02.008Suche in Google Scholar PubMed

[32] Zhang Z, Liu F, Zhao X, Wang X, Shi L, Xu J, et al. Urban expansion in China based on remote sensing technology: A review. Chin Geogr Sci. 2018;28:727–43.10.1007/s11769-018-0988-9Suche in Google Scholar

[33] Hemati M, Hasanlou M, Mahdianpari M, Mohammadimanesh F. A systematic review of landsat data for change detection applications: 50 years of monitoring the earth. Remote Sens. 2021;13:2869.10.3390/rs13152869Suche in Google Scholar

[34] Liu J, Li Y, Zhang Y, Feng Q, Shi T, Zhang D, et al. Impervious surface Mapping and its spatial–temporal evolution analysis in the Yellow River Delta over the last three decades using Google Earth Engine. Earth Sci Inform. 2023;16:1727–39.10.1007/s12145-023-01010-xSuche in Google Scholar

[35] Afroz F, Hasan MM, Rouf RB, Nazir MMH, Altuwaijri HA, Al Kafy A, et al. Comparative analysis of machine learning algorithms in Google Earth Engine for urban land use dynamics in rapidly urbanizing South Asian cities. Open Geosci. 2025;17:20250769.10.1515/geo-2025-0769Suche in Google Scholar

[36] Basommi PL, Guan Q, Cheng D. Exploring land use and land cover change in the mining areas of Wa East District, Ghana using satellite imagery. Open Geosci. 2015;7:20150058.10.1515/geo-2015-0058Suche in Google Scholar

[37] Yu Z, Ciais P, Piao S, Houghton RA, Lu C, Tian H, et al. Forest expansion dominates China’s land carbon sink since 1980. Nat Commun. 2022;13:5374.10.1038/s41467-022-32961-2Suche in Google Scholar PubMed PubMed Central

[38] Zhang X, Liu L, Chen X, Gao Y, Xie S, Mi J. GLC_FCS30: Global land-cover product with fine classification system at 30 m using time-series Landsat imagery. Earth Syst Sci Data Discuss. 2020;2020:1–31.10.5194/essd-2020-182Suche in Google Scholar

[39] Liu J, Jin X, Xu W, Gu Z, Yang X, Ren J, et al. A new framework of land use efficiency for the coordination among food, economy and ecology in regional development. Sci Total Environ. 2020;710:135670.10.1016/j.scitotenv.2019.135670Suche in Google Scholar PubMed

[40] Gong P, Li X, Wang J, Bai Y, Chen B, Hu T, et al. Annual maps of global artificial impervious area (GAIA) between 1985 and 2018. Remote Sens Environ. 2020;236:111510.10.1016/j.rse.2019.111510Suche in Google Scholar

[41] Florczyk AJ, Corbane C, Ehrlich D, Freire S, Kemper T, Maffenini L, et al. GHSL data package 2019. Luxembourg, eur. 2019;29788:290498.Suche in Google Scholar

[42] Huang X, Li J, Yang J, Zhang Z, Li D, Liu X. 30 m global impervious surface area dynamics and urban expansion pattern observed by Landsat satellites: From 1972 to 2019. Sci China Earth Sci. 2021;64:1922–33.10.1007/s11430-020-9797-9Suche in Google Scholar

[43] Wu C, Wei YD, Huang X, Chen B. Economic transition, spatial development and urban land use efficiency in the Yangtze River Delta, China. Habitat Int. 2017;63:67–78.10.1016/j.habitatint.2017.03.012Suche in Google Scholar

[44] Chen L, Xia X, Zhang J, Zhu Y, Long C, Chen Y, et al. The food security risks in the Yangtze River Delta of China associated with water scarcity, grain production, and grain trade. Sci Total Environ. 2024;948:174863.10.1016/j.scitotenv.2024.174863Suche in Google Scholar PubMed

[45] Zhang X, Liu L, Chen X, Gao Y, Jiang M. Automatically monitoring impervious surfaces using spectral generalization and time series Landsat imagery from 1985 to 2020 in the Yangtze River Delta. J Remote Sens. 2021;2021:1–16.10.34133/2021/9873816Suche in Google Scholar

[46] Zhou D, Zhao S, Liu S, Zhang L, Zhu C. Surface urban heat island in China’s 32 major cities: Spatial patterns and drivers. Remote Sens Environ. 2014;152:51–61.10.1016/j.rse.2014.05.017Suche in Google Scholar

[47] Camagni R, Gibelli MC, Rigamonti P. Urban mobility and urban form: the social and environmental costs of different patterns of urban expansion. Ecol Econ. 2002;40:199–216.10.1016/S0921-8009(01)00254-3Suche in Google Scholar

[48] Huang X, Xia J, Xiao R, He T. Urban expansion patterns of 291 Chinese cities, 1990–2015. Int J Digit Earth. 2019;12:62–77.10.1080/17538947.2017.1395090Suche in Google Scholar

[49] Shao Z, Fu H, Fu P, Yin L. Mapping urban impervious surface by fusing optical and SAR data at the decision level. Remote Sens. 2016;8:945.10.3390/rs8110945Suche in Google Scholar

[50] Zhang Y, Zhang H, Lin H. Improving the impervious surface estimation with combined use of optical and SAR remote sensing images. Remote Sens Environ. 2014;141:13.10.1016/j.rse.2013.10.028Suche in Google Scholar

[51] Hu X, Weng Q. Impervious surface area extraction from IKONOS imagery using an object-based fuzzy method. Geocarto Int. 2011;26:3–20.10.1080/10106049.2010.535616Suche in Google Scholar

[52] El-Deen Taha LG. Classifier ensemble for improving land cover classification. Int J Circuits Syst Signal Process. 2016;10:346.Suche in Google Scholar

[53] Fang C, Zhao S. A comparative study of spatiotemporal patterns of urban expansion in six major cities of the Yangtze River Delta from 1980 to 2015. Ecosyst Health Sustain. 2018;4:95–114.10.1080/20964129.2018.1469960Suche in Google Scholar

[54] Yu Z, Chen L, Li L, Zhang T, Yuan L, Liu R, et al. Spatiotemporal characterization of the urban expansion patterns in the Yangtze River Delta region. Remote Sens. 2021;13:4484.10.3390/rs13214484Suche in Google Scholar

[55] Cai WJ, Tu FY. Spatiotemporal characteristics and driving forces of construction land expansion in Yangtze River economic belt, China. PLoS One. 2020;15:e0227299.10.1371/journal.pone.0227299Suche in Google Scholar PubMed PubMed Central

[56] Zhao W, Liu X, Deng Q, Li D, Xu J, Li M, et al. Spatial association of urbanization in the Yangtze River Delta, China. Int J Environ Res Public Health. 2020;17:7276.10.3390/ijerph17197276Suche in Google Scholar PubMed PubMed Central

[57] Li M, Cao Y, Song J, Li H, Liang M. Spatiotemporal characteristics and determinants of urban expansion in China: perspective of urban agglomerations. Front Earth Sci. 2025;12:1523020.10.3389/feart.2024.1523020Suche in Google Scholar

[58] Zou YH, Peng HQ, Liu G, Yang KD, Xie YH, Weng QH. Monitoring urban clusters expansion in the middle reaches of the Yangtze River, China, using time-series nighttime light images. Remote Sens. 2017;9:1007.10.3390/rs9101007Suche in Google Scholar

[59] Bethuel C, Arvor D, Corpetti T, Hélie J, Descals A, Gaveau D, et al. Applying the dempster–shafer fusion theory to combine independent land-use maps: A case study on the mapping of oil palm plantations in Sumatra, Indonesia. Remote Sens. 2025;17:234.10.3390/rs17020234Suche in Google Scholar

[60] Li L, Jiang X, Geng HZ, Wang YF, Zhao BC. Spatial expansion characteristics and nonlinear relationships of driving factors in urban agglomerations: A case study of the Yangtze River Delta urban agglomeration in China. Land. 2024;13:1951.10.3390/land13111951Suche in Google Scholar

Received: 2025-04-28
Revised: 2025-07-10
Accepted: 2025-08-01
Published Online: 2025-09-12

© 2025 the author(s), published by De Gruyter

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

Artikel in diesem Heft

  1. Research Articles
  2. Seismic response and damage model analysis of rocky slopes with weak interlayers
  3. Multi-scenario simulation and eco-environmental effect analysis of “Production–Living–Ecological space” based on PLUS model: A case study of Anyang City
  4. Remote sensing estimation of chlorophyll content in rape leaves in Weibei dryland region of China
  5. GIS-based frequency ratio and Shannon entropy modeling for landslide susceptibility mapping: A case study in Kundah Taluk, Nilgiris District, India
  6. Natural gas origin and accumulation of the Changxing–Feixianguan Formation in the Puguang area, China
  7. Spatial variations of shear-wave velocity anomaly derived from Love wave ambient noise seismic tomography along Lembang Fault (West Java, Indonesia)
  8. Evaluation of cumulative rainfall and rainfall event–duration threshold based on triggering and non-triggering rainfalls: Northern Thailand case
  9. Pixel and region-oriented classification of Sentinel-2 imagery to assess LULC dynamics and their climate impact in Nowshera, Pakistan
  10. The use of radar-optical remote sensing data and geographic information system–analytical hierarchy process–multicriteria decision analysis techniques for revealing groundwater recharge prospective zones in arid-semi arid lands
  11. Effect of pore throats on the reservoir quality of tight sandstone: A case study of the Yanchang Formation in the Zhidan area, Ordos Basin
  12. Hydroelectric simulation of the phreatic water response of mining cracked soil based on microbial solidification
  13. Spatial-temporal evolution of habitat quality in tropical monsoon climate region based on “pattern–process–quality” – a case study of Cambodia
  14. Early Permian to Middle Triassic Formation petroleum potentials of Sydney Basin, Australia: A geochemical analysis
  15. Micro-mechanism analysis of Zhongchuan loess liquefaction disaster induced by Jishishan M6.2 earthquake in 2023
  16. Prediction method of S-wave velocities in tight sandstone reservoirs – a case study of CO2 geological storage area in Ordos Basin
  17. Ecological restoration in valley area of semiarid region damaged by shallow buried coal seam mining
  18. Hydrocarbon-generating characteristics of Xujiahe coal-bearing source rocks in the continuous sedimentary environment of the Southwest Sichuan
  19. Hazard analysis of future surface displacements on active faults based on the recurrence interval of strong earthquakes
  20. Structural characterization of the Zalm district, West Saudi Arabia, using aeromagnetic data: An approach for gold mineral exploration
  21. Research on the variation in the Shields curve of silt initiation
  22. Reuse of agricultural drainage water and wastewater for crop irrigation in southeastern Algeria
  23. Assessing the effectiveness of utilizing low-cost inertial measurement unit sensors for producing as-built plans
  24. Analysis of the formation process of a natural fertilizer in the loess area
  25. Machine learning methods for landslide mapping studies: A comparative study of SVM and RF algorithms in the Oued Aoulai watershed (Morocco)
  26. Chemical dissolution and the source of salt efflorescence in weathering of sandstone cultural relics
  27. Molecular simulation of methane adsorption capacity in transitional shale – a case study of Longtan Formation shale in Southern Sichuan Basin, SW China
  28. Evolution characteristics of extreme maximum temperature events in Central China and adaptation strategies under different future warming scenarios
  29. Estimating Bowen ratio in local environment based on satellite imagery
  30. 3D fusion modeling of multi-scale geological structures based on subdivision-NURBS surfaces and stratigraphic sequence formalization
  31. Comparative analysis of machine learning algorithms in Google Earth Engine for urban land use dynamics in rapidly urbanizing South Asian cities
  32. Study on the mechanism of plant root influence on soil properties in expansive soil areas
  33. Simulation of seismic hazard parameters and earthquakes source mechanisms along the Red Sea rift, western Saudi Arabia
  34. Tectonics vs sedimentation in foredeep basins: A tale from the Oligo-Miocene Monte Falterona Formation (Northern Apennines, Italy)
  35. Investigation of landslide areas in Tokat-Almus road between Bakımlı-Almus by the PS-InSAR method (Türkiye)
  36. Predicting coastal variations in non-storm conditions with machine learning
  37. Cross-dimensional adaptivity research on a 3D earth observation data cube model
  38. Geochronology and geochemistry of late Paleozoic volcanic rocks in eastern Inner Mongolia and their geological significance
  39. Spatial and temporal evolution of land use and habitat quality in arid regions – a case of Northwest China
  40. Ground-penetrating radar imaging of subsurface karst features controlling water leakage across Wadi Namar dam, south Riyadh, Saudi Arabia
  41. Rayleigh wave dispersion inversion via modified sine cosine algorithm: Application to Hangzhou, China passive surface wave data
  42. Fractal insights into permeability control by pore structure in tight sandstone reservoirs, Heshui area, Ordos Basin
  43. Debris flow hazard characteristic and mitigation in Yusitong Gully, Hengduan Mountainous Region
  44. Research on community characteristics of vegetation restoration in hilly power engineering based on multi temporal remote sensing technology
  45. Identification of radial drainage networks based on topographic and geometric features
  46. Trace elements and melt inclusion in zircon within the Qunji porphyry Cu deposit: Application to the metallogenic potential of the reduced magma-hydrothermal system
  47. Pore, fracture characteristics and diagenetic evolution of medium-maturity marine shales from the Silurian Longmaxi Formation, NE Sichuan Basin, China
  48. Study of the earthquakes source parameters, site response, and path attenuation using P and S-waves spectral inversion, Aswan region, south Egypt
  49. Source of contamination and assessment of potential health risks of potentially toxic metal(loid)s in agricultural soil from Al Lith, Saudi Arabia
  50. Regional spatiotemporal evolution and influencing factors of rural construction areas in the Nanxi River Basin via GIS
  51. An efficient network for object detection in scale-imbalanced remote sensing images
  52. Effect of microscopic pore–throat structure heterogeneity on waterflooding seepage characteristics of tight sandstone reservoirs
  53. Environmental health risk assessment of Zn, Cd, Pb, Fe, and Co in coastal sediments of the southeastern Gulf of Aqaba
  54. A modified Hoek–Brown model considering softening effects and its applications
  55. Evaluation of engineering properties of soil for sustainable urban development
  56. The spatio-temporal characteristics and influencing factors of sustainable development in China’s provincial areas
  57. Application of a mixed additive and multiplicative random error model to generate DTM products from LiDAR data
  58. Gold vein mineralogy and oxygen isotopes of Wadi Abu Khusheiba, Jordan
  59. Prediction of surface deformation time series in closed mines based on LSTM and optimization algorithms
  60. 2D–3D Geological features collaborative identification of surrounding rock structural planes in hydraulic adit based on OC-AINet
  61. Spatiotemporal patterns and drivers of Chl-a in Chinese lakes between 1986 and 2023
  62. Land use classification through fusion of remote sensing images and multi-source data
  63. Nexus between renewable energy, technological innovation, and carbon dioxide emissions in Saudi Arabia
  64. Analysis of the spillover effects of green organic transformation on sustainable development in ethnic regions’ agriculture and animal husbandry
  65. Factors impacting spatial distribution of black and odorous water bodies in Hebei
  66. Large-scale shaking table tests on the liquefaction and deformation responses of an ultra-deep overburden
  67. Impacts of climate change and sea-level rise on the coastal geological environment of Quang Nam province, Vietnam
  68. Reservoir characterization and exploration potential of shale reservoir near denudation area: A case study of Ordovician–Silurian marine shale, China
  69. Seismic prediction of Permian volcanic rock reservoirs in Southwest Sichuan Basin
  70. Application of CBERS-04 IRS data to land surface temperature inversion: A case study based on Minqin arid area
  71. Geological characteristics and prospecting direction of Sanjiaoding gold mine in Saishiteng area
  72. Research on the deformation prediction model of surrounding rock based on SSA-VMD-GRU
  73. Geochronology, geochemical characteristics, and tectonic significance of the granites, Menghewula, Southern Great Xing’an range
  74. Hazard classification of active faults in Yunnan base on probabilistic seismic hazard assessment
  75. Characteristics analysis of hydrate reservoirs with different geological structures developed by vertical well depressurization
  76. Estimating the travel distance of channelized rock avalanches using genetic programming method
  77. Landscape preferences of hikers in Three Parallel Rivers Region and its adjacent regions by content analysis of user-generated photography
  78. New age constraints of the LGM onset in the Bohemian Forest – Central Europe
  79. Characteristics of geological evolution based on the multifractal singularity theory: A case study of Heyu granite and Mesozoic tectonics
  80. Soil water content and longitudinal microbiota distribution in disturbed areas of tower foundations of power transmission and transformation projects
  81. Oil accumulation process of the Kongdian reservoir in the deep subsag zone of the Cangdong Sag, Bohai Bay Basin, China
  82. Investigation of velocity profile in rock–ice avalanche by particle image velocimetry measurement
  83. Optimizing 3D seismic survey geometries using ray tracing and illumination modeling: A case study from Penobscot field
  84. Sedimentology of the Phra That and Pha Daeng Formations: A preliminary evaluation of geological CO2 storage potential in the Lampang Basin, Thailand
  85. Improved classification algorithm for hyperspectral remote sensing images based on the hybrid spectral network model
  86. Map analysis of soil erodibility rates and gully erosion sites in Anambra State, South Eastern Nigeria
  87. Identification and driving mechanism of land use conflict in China’s South-North transition zone: A case study of Huaihe River Basin
  88. Evaluation of the impact of land-use change on earthquake risk distribution in different periods: An empirical analysis from Sichuan Province
  89. A test site case study on the long-term behavior of geotextile tubes
  90. An experimental investigation into carbon dioxide flooding and rock dissolution in low-permeability reservoirs of the South China Sea
  91. Detection and semi-quantitative analysis of naphthenic acids in coal and gangue from mining areas in China
  92. Comparative effects of olivine and sand on KOH-treated clayey soil
  93. YOLO-MC: An algorithm for early forest fire recognition based on drone image
  94. Earthquake building damage classification based on full suite of Sentinel-1 features
  95. Potential landslide detection and influencing factors analysis in the upper Yellow River based on SBAS-InSAR technology
  96. Assessing green area changes in Najran City, Saudi Arabia (2013–2022) using hybrid deep learning techniques
  97. An advanced approach integrating methods to estimate hydraulic conductivity of different soil types supported by a machine learning model
  98. Hybrid methods for land use and land cover classification using remote sensing and combined spectral feature extraction: A case study of Najran City, KSA
  99. Streamlining digital elevation model construction from historical aerial photographs: The impact of reference elevation data on spatial accuracy
  100. Analysis of urban expansion patterns in the Yangtze River Delta based on the fusion impervious surfaces dataset
  101. A metaverse-based visual analysis approach for 3D reservoir models
  102. Late Quaternary record of 100 ka depositional cycles on the Larache shelf (NW Morocco)
  103. Review Articles
  104. Humic substances influence on the distribution of dissolved iron in seawater: A review of electrochemical methods and other techniques
  105. Applications of physics-informed neural networks in geosciences: From basic seismology to comprehensive environmental studies
  106. Ore-controlling structures of granite-related uranium deposits in South China: A review
  107. Shallow geological structure features in Balikpapan Bay East Kalimantan Province – Indonesia
  108. A review on the tectonic affinity of microcontinents and evolution of the Proto-Tethys Ocean in Northeastern Tibet
  109. Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part II
  110. Depopulation in the Visok micro-region: Toward demographic and economic revitalization
  111. Special Issue: Geospatial and Environmental Dynamics - Part II
  112. Advancing urban sustainability: Applying GIS technologies to assess SDG indicators – a case study of Podgorica (Montenegro)
  113. Spatiotemporal and trend analysis of common cancers in men in Central Serbia (1999–2021)
  114. Minerals for the green agenda, implications, stalemates, and alternatives
  115. Spatiotemporal water quality analysis of Vrana Lake, Croatia
  116. Functional transformation of settlements in coal exploitation zones: A case study of the municipality of Stanari in Republic of Srpska (Bosnia and Herzegovina)
  117. Hypertension in AP Vojvodina (Northern Serbia): A spatio-temporal analysis of patients at the Institute for Cardiovascular Diseases of Vojvodina
  118. Regional patterns in cause-specific mortality in Montenegro, 1991–2019
  119. Spatio-temporal analysis of flood events using GIS and remote sensing-based approach in the Ukrina River Basin, Bosnia and Herzegovina
  120. Flash flood susceptibility mapping using LiDAR-Derived DEM and machine learning algorithms: Ljuboviđa case study, Serbia
  121. Geocultural heritage as a basis for geotourism development: Banjska Monastery, Zvečan (Serbia)
  122. Assessment of groundwater potential zones using GIS and AHP techniques – A case study of the zone of influence of Kolubara Mining Basin
  123. Impact of the agri-geographical transformation of rural settlements on the geospatial dynamics of soil erosion intensity in municipalities of Central Serbia
  124. Where faith meets geomorphology: The cultural and religious significance of geodiversity explored through geospatial technologies
  125. Applications of local climate zone classification in European cities: A review of in situ and mobile monitoring methods in urban climate studies
  126. Complex multivariate water quality impact assessment on Krivaja River
Heruntergeladen am 2.10.2025 von https://www.degruyterbrill.com/document/doi/10.1515/geo-2025-0869/html?lang=de
Button zum nach oben scrollen