Original Research
Frontiers in Environmental Science ·
Volume 14 - 2026 | https://doi.org/10.3389/fenvs.2026.1908887
Land use change, driving factors, and multi-scenario projections of ecosystem service supply in the Yangtze River delta urban agglomeration
- Aixia Chen1
- Qiao Sun2*corresponding author
- Mingming Zhu1
- Zhiying Shao3
- Kaiyuan He3
- 1School of Business, Jiangsu Open University, Nanjing, Jiangsu Province, China
- 2School of Accounting and International Trade, Suzhou Institute of Trade & Commerce, Suzhou, Jiangsu Province, China
- 3School of Economics and Management, Xiangnan University, Chenzhou, China
Abstract
Rapid urban expansion has intensified regional human-land conflicts and ecological risks. This study examines the Yangtze River Delta Urban Agglomeration the key urban cluster development areas in China, using multi-source spatial data and integrated modeling approaches, including the Integrated Valuation of Ecosystem Services and Tradeoffs (InVEST) and Patch-level Land Use Simulation (PLUS) models, to analyze land use changes from 2000 to 2020 and assess ecosystem service dynamics for 2010–2020, and project future land use patterns under three development scenarios for 2030 and 2060. The results suggest that: (1) conversion of cropland to construction land is primarily associated with land use changes, with over 3,000 km 2 transformed during 2000–2005, resulting in landscape fragmentation and ecosystem service degradation; (2) distinct driving factors are associated with different land types, cropland dynamics respond to both slope constraints and socio-economic factors, construction land expansion correlates strongly with population growth, while forest/grassland distribution follows natural determinants; and (3) scenario analysis projects that continuing current trends would expand construction land by 9,000 km 2 by 2060, associated with substantial carbon storage decline, whereas ecological priority scenarios may substantially mitigate these risks. This research provides valuable insights for balancing ecological conservation and urban development in rapidly urbanizing regions.
Keywords
1 Introduction
Global urbanization is accelerating rapidly, with over half the global population residing in urban areas and this proportion projected to reach 68% by 2050 according to the United Nations World Urbanization Prospects. This trend is particularly pronounced in China, where major city clusters including the Yangtze River Delta have been positioned as core national development engines under strategic spatial planning frameworks (Jia et al., 2024; Zhou et al., 2025). While these policies boost economic agglomeration and infrastructure development effectively (Meury et al., 2025), rapid land use conversion exerts intense ecological pressure. Sustained built-up area expansion encroaches on croplands, forests and wetlands, fundamentally reshaping regional landscape patterns (Verma et al., 2024; Herdt and Wälty, 2026). This transformation fragments natural habitats, degrades ecosystem functions, and reduces the supply of key services such as water conservation, carbon sequestration and soil retention (Jessica et al., 2022; Bagstad et al., 2019; Sharma et al., 2024; Yi et al., 2022). Rapid urban expansion further intensifies pressure on ecosystem service supply, threatening sustainable development in densely urbanized regions (Wang et al., 2021). Therefore, clarifying the interactions between urban expansion, land use change and ecosystem service dynamics is essential to establish effective spatial governance and coordinate socioeconomic development with ecological security.
However, retrospective analyses of historical ES dynamics, though effective in detecting ecosystem service supply pressure (Yu et al., 2025), have limited ability to guide future sustainable development pathways (Sullivan et al., 2024). Urban systems are complex and nonlinear; future changes in ES supply will be dominated by dynamic adjustments in policies, land use strategies and climatic conditions. Thus, simulating the evolution of ecosystem service supply under diverse plausible scenarios is critical for proactive ecological governance (Ai et al., 2024). An integrated framework combining land use simulation models with ES assessment under multiple scenarios supports forward-looking analysis of these dynamics (Li et al., 2023). This multi-scenario approach helps clarify the complex mechanisms by which land use decisions affect ES cascades, and provides reliable scientific support to steer regions toward a more sustainable and ecologically secure development path.
Therefore, to investigate the ecosystem service provision capacity and ecological condition and sustainable development prospects of key regions such as urban agglomerations, this study selects the YRDUA as the research area. Applying ecosystem service theory and employing the InVEST and PLUS model, supported by multi-source data including meteorological observations, remote sensing imagery, and economic statistics, the following research was conducted: (1) assessment of land use changes and ecosystem service capacities in the region; (2) establishment of a driving factors framework for land use changes to identify key drivers of various land types; and (3) development of three scenarios—baseline, economic priority, and ecological priority—to conduct multi-scenario simulations. These simulations project and analyze the spatial patterns of land use changes and ecosystem service prospects in the YRDUA for 2030 and 2060, providing a reference for scientifically mitigating ecological risks in the region.
2 Materials and methods
2.1 Study area and data sources
2.1.1 Study area
The YRDUA (Figure 1), located in eastern coastal China, is a key engine of national economic growth and one of the world’s six major world-class urban agglomerations. Stretching from 116°E to 123°E longitude and 27°N to 33°N latitude, it has a subtropical monsoon climate with clear seasons and coordinated rainfall and temperature. Covering 2.12 × 105 km2, centered on Shanghai, it includes 26 prefecture-level cities across Jiangsu, Zhejiang and Anhui provinces. Dense water networks, including the Yangtze River, Taihu Lake and Qiantang River, sustain water supply and regional ecological stability. The region had a permanent population of about 225 million and a GDP of 31 trillion yuan in 2025 (Tang et al., 2025), making it China’s most economically developed and densely urbanized area. It should be noted that the historical land-use and ecosystem service analysis in this study is based on data from 2000–2020, and future projections are for 2030 and 2060.

2.1.2 Data
This study employed multi-source datasets to examine land use dynamics and ecosystem service changes in the YRDUA. Data included multi-temporal land cover from remote sensing, meteorological data, WorldPop population grids, and GDP and administrative boundaries from the Resource and Environment Science and Data Center of the Chinese Academy of Sciences. Socioeconomic statistics were collected from yearbooks and water bulletins. Transportation and river vectors, 30 m ASTER GDEM, and soil parameters from the Harmonized World Soil Database were also used. The data and sources used are as shown in Table 1.
TABLE 1. Description of data and sources.
| Data category | Data content | Source |
|---|---|---|
| LUCC | LUCC in 2000, 2005, 2010, 2015 and 2020 | Remote sensing monitoring dataset of land use in China (CNLUCC), https://www.resdc.cn, 2000–2020, 30m/1 km |
| Economic statistics | GDP | Resources and Environmental Sciences and Data Center, Chinese Academy of Sciences, https://www.resdc.cn, 2000–2020, 1 km |
| Population | WorldPop Database, https://www.worldpop.org, 2000–2020, 1 km | |
| Major highways | National Catalogue Service for Geographic Information, https://www.webmap.cn | |
| Major railways | ||
| Main rivers | ||
| Vector data of administrative divisions | Standard Map Service System of the Ministry of Natural Resources of China, https://bzdt.ch.mnr.gov.cn | |
| Natural environmentdata | Soil organic matter | Harmonized World Soil Database (HWSD), https://www.isric.org, 1 km |
| Precipitation | National Qinghai-Xizang Plateau Scientific Data Center (Han et al., 2023; Miao et al., 2022; Gou et al., 2021), http://data.tpdc.ac.cn, 2000–2020, 1 km | |
| Evapotranspiration | ||
| Temperature | ||
| Surface runoff | ||
| DEM | Geospatial Data Cloud, https://www.gscloud.cn | |
| Slope data | Generated by DEM processing |
It should be noted that the historical land-use analysis in this study covers 2000–2020, while ecosystem service assessment covers 2010–2020 (three time points: 2010, 2015, and 2020) due to data availability constraints for pixel-level socio-economic parameters before 2010. Future projections are for 2030 and 2060.
2.2 Land use transfer matrix
To accurately characterize the dynamic evolution of geospatial units during the study period, a land use transfer matrix needs to be constructed based on the changes in land use types of the same units between the start and end of each observation period.
This matrix visually reflects the transformation pathways and intensity of various land cover types within the study area. Assuming there are n distinct land use types, the land use transfer matrix can be represented as an n × n matrix. Each element in the matrix denotes the transition proportion or probability from the ith land use type to the jth land use type. This can be used to analyze and predict the changing trends and relationships between different land use types. The land use transfer matrix serves as a critical analytical tool in fields such as land use planning, resource management, and environmental protection, enabling decision-makers to better understand the patterns of land use change and formulate rational land use policies and spatial planning strategies.
2.3 Ecosystem services assessment
The YRDUA faces rapid population growth and urban expansion, which greatly suppresses local ecosystem service supply. As a core region for carbon control under China’s ‘Dual Carbon’ target, the region depends heavily on ecosystem carbon storage. This study selected four key ecosystem services: water conservation, carbon storage, soil conservation, and crop production, to assess regional ecosystem service provision capacity and ecological condition. Following China’s Technical Specification for Ecosystem Service Assessment (HJ 1173–2021) and previous studies, the InVEST model was applied to evaluate ecosystem service status.
Table 2 lists detailed assessment methods for each service. Specifically, the water yield module is based on the Budyko curve framework. Carbon storage is evaluated using the four-carbon-pool framework (aboveground biomass, belowground biomass, soil organic matter, and litter)(Xu et al., 2019). Soil conservation is calculated using the Revised Universal Soil Loss Equation (RUSLE)(Wischmeier, 1959; Zhang et al., 2022). Crop production was assessed using Normalized Difference Vegetation Index (NDVI) data-based spatial allocation method: total grain production for each city was obtained from statistical yearbooks, annual maximum NDVI were used as a proxy for vegetation productivity, and statistical production was allocated to pixels following Y i j = Y j × N D V I i j / ∑ N D V I i j. Crop type differentiation was not separately modeled; comprehensive NDVI was used for total grain production allocation. The ecosystem service assessment covers 2010–2020 (three time points: 2010, 2015, 2020) due to data availability constraints for pixel-level socio-economic parameters before 2010, while land-use change analysis covers 2000–2020. To ensure accuracy, simulation results were compared with official data from water bulletins and statistical yearbooks. Water yield was validated against observed runoff data, and crop production against statistical yearbook data, with errors of all indicators within 15%, consistent with the commonly accepted range (10%–20%) for ecosystem service models. The Zhang coefficient was calibrated to 27.2, meeting research accuracy requirements. For future crop production projections (2030 and 2060), the 2020 NDVI-based productivity conditions were held constant, and crop production was re-allocated spatially based solely on the projected land-use changes under each scenario. This assumption isolates the impact of land-use pattern change on crop production, without considering future improvements or declines in agricultural technology and climate-driven yield changes.
TABLE 2. Evaluation methods for ecosystem services.
| Ecosystem service function | Evaluation method | References |
|---|---|---|
| Water Yield (WY) | Annual Water Yield module of InVEST based on Budyko curve | Wang and Sun (2024); Yang et al. (2019) |
| Carbon Storage (CS) | Carbon Storage and Sequestration module of InVEST | Ocloo and Mizunoya (2025); Zhu et al. (2025) |
| Soil Conservation (SC) | Sediment Delivery Ratio (SDR) module of InVEST based on RUSLE | Qiu et al. (2025), Zhong et al. (2020) |
| Crop Production (CP) | NDVI-based spatial allocation of statistical crop production data | Shi et al. (2021) |
2.4 Analysis of driving factors of land use change
Regional land use change is driven by a combination of socioeconomic demands, natural conditions, and infrastructure development. Infrastructure, such as roads and railways, enhances the efficiency of material and information flow, thereby influencing the spatial concentration or dispersion of resources. The driving factor analysis was conducted using the LEAS (Land Expansion Analysis Strategy) module of the PLUS model, which employs a Random Forest algorithm to extract patch-level land-use expansion data and calculate the contribution (feature importance) of each driving factor for each land-use type. To analyze these effects, this study establishes a driving factors system from three dimensions: infrastructure, socioeconomic conditions, and the natural environment. Specific indicators include proximity to major roads and railways; regional GDP and population; annual rainfall, temperature, and evapotranspiration; distance to major rivers; slope; and DEM. This framework is designed to systematically examine the influence of these factors on recent land use change in the YRDUA. Contribution is expressed as Random Forest feature importance, where higher values indicate higher Random Forest feature importance score for that land-use type’s expansion. The composition of the driving factors system, along with detailed data processing procedures, is provided in Table 3.
TABLE 3. Driving factors of land use type change.
| Factor category | Variable name | Processing procedure | Notes |
|---|---|---|---|
| Infrastructure factors | Distance from main roads | Spatial Euclidean distance | Expressways, first-class and second-class roads within the region |
| Distance from major railways | Spatial Euclidean distance | The main railway trunk lines within the region | |
| Socio-economic factors | GDP | Rasterization | \ |
| Population | Rasterization | \ | |
| Natural environmental factors | Annual precipitation | Rasterization | \ |
| Annual average temperature | Rasterization | \ | |
| Annual evapotranspiration | Rasterization | \ | |
| Distance from major rivers | Spatial Euclidean distance | Including primary and secondary rivers within the area | |
| Slope | Calculated based on the DEM by ArcGIS | \ | |
| DEM | Digital elevation data of regional terrain | 30 m precision |
2.5 Land use change prediction based on PLUS model
The PLUS model is a patch-level land use change simulation model driven by historical raster data. It contains two core modules: the Land Expansion Analysis Strategy (LEAS) and Cellular Automata based on Random patch Seeding (CARS). Built on the Cellular Automata (CA) framework, this model adopts the Random Forest (RF) algorithm to extract patch expansion data. It ranks driving factors sequentially and identifies regional land use trends, thus finishing patch-scale simulation. The PLUS model outperforms traditional models with high integration and superior prediction accuracy.
Figure 2 illustrates the model simulation workflow in this study. The target land-use demand for each category in 2030 and 2060 was determined using a Markov chain prediction based on historical land-use transition probabilities from 2000 to 2020 (Li et al., 2024; Yang et al., 2022). Three contrasting scenarios were designed: (a) Baseline scenario: land-use evolves according to historical transition probabilities from 2000–2020 without additional constraints; (b) Economic priority scenario: construction land demand is increased, natural lands are permitted to convert to cropland and construction land unidirectionally, and ecological land expansion is constrained; (c) Ecological priority scenario: construction land expansion is constrained, forest and grassland are strictly protected, and ecological restoration is encouraged. Each land use type was parameterized separately per scenario logic. The model achieved a Kappa coefficient of 0.928, overall accuracy of 0.951, and FoM (Figure of Merit) of 0.144. FoM specifically assesses the model’s ability to simulate the location of land-use changes; a value of 0.144 is within the acceptable range (0.1–0.3) commonly reported in similar studies. The confusion matrix was computed excluding permanent water bodies and marine areas (approximately 93,600 km2), resulting in approximately 116,984 valid land pixels at 1 km resolution. Detailed parameter settings and model accuracy verification are provided in Supplementary Appendix A1.

3 Results
3.1 The current situation of land use change and transfer
This study utilized land cover data from the YRDUA for the period 2000–2020. The analysis was structured around five-year intervals, specifically 2000–2005, 2005–2010, 2010–2015, and 2015–2020. For each interval, the land use transitions were calculated, the transfer matrices in 2000–2005 and 2015–2020 are presented in Tables 4, 5 respectively. The remaining results can be seen in Supplementary Appendix A2.
TABLE 4. Land type transfer matrix of YRDUA from 2000 to 2005 (unit: km2).
| Types | Year 2005 | |||||||
|---|---|---|---|---|---|---|---|---|
| Cropland | Forest land | Grassland | Water | Construction land | Unutilized land | Total | ||
| Year 2000 | Cropland | 106463.25 | 223.34 | 10.89 | 655.38 | 3163.90 | 0.84 | 110517.60 |
| Forest land | 222.08 | 57034.74 | 66.65 | 34.21 | 166.98 | 1.99 | 57526.64 | |
| Grassland | 54.21 | 78.97 | 7690.60 | 36.89 | 20.40 | 1.59 | 7882.66 | |
| Water | 288.50 | 17.16 | 20.94 | 17954.91 | 102.76 | 0.01 | 18384.28 | |
| Construction land | 157.53 | 11.03 | 0.72 | 13.50 | 16152.87 | 0.04 | 16335.68 | |
| Unutilized land | 0.13 | 0.55 | 0.01 | 0.01 | 2.78 | 31.58 | 35.06 | |
| Total | 107185.69 | 57365.79 | 7789.80 | 18694.89 | 19609.69 | 36.06 | 210681.92 |
TABLE 5. Land type transfer matrix of YRDUA from 2015 to 2020 (unit: km2).
| Types | Year 2020 | |||||||
|---|---|---|---|---|---|---|---|---|
| Cropland | Forest land | Grassland | Water | Construction land | Unutilized land | Total | ||
| Year 2015 | Cropland | 94333.28 | 1036.58 | 105.83 | 493.16 | 3451.68 | 14.86 | 99435.39 |
| Forest land | 743.90 | 55587.93 | 165.92 | 63.20 | 341.80 | 4.29 | 56907.05 | |
| Grassland | 143.15 | 135.60 | 6827.02 | 132.77 | 61.04 | 0.83 | 7300.41 | |
| Water | 753.04 | 59.82 | 313.30 | 17725.83 | 332.22 | 146.05 | 19330.27 | |
| Construction land | 1658.32 | 144.45 | 84.25 | 528.69 | 24952.80 | 19.67 | 27388.18 | |
| Unutilized land | 61.22 | 4.93 | 23.57 | 14.24 | 4.72 | 89.93 | 198.60 | |
| Total | 97692.92 | 56969.31 | 7519.88 | 18957.90 | 29144.26 | 275.64 | 210559.90 |
Between 2000 and 2005, the total cropland area in the YRDUA decreased from 110,517.60 km2 to 107,185.69 km2, representing a net loss of 3,331.91 km2. During this period, 3,163.90 km2 of cropland were converted to construction land, 655.38 km2 to water, and 223.34 km2 to forest land, with minor conversions to grassland and unutilized land. As the second largest land cover type, forest land experienced a total transition of 491.91 km2, primarily to cropland (222.08 km2) and construction land (166.98 km2), while the remainder was converted to grassland, water, and unutilized land.
During the period from 2015 to 2020, land use types in the YRDUA continued to undergo significant changes. Cropland area in the region decreased consistently, from 99,435.39 km2 in 2015 to 97,692.92 km2 in 2020. In contrast, construction land area showed an opposite trend, increasing by 1,756.08 km2 due to urban expansion. Meanwhile, with the growing emphasis on ecological conservation and the implementation of relevant policies, forest land and grassland areas increased by 62.26 km2 and 219.47 km2, respectively. The expansion of these land types helps enhance the provision of fundamental ecosystem services in the region, thereby contributing to alleviating ecosystem service supply pressure.
Figure 3 illustrates the conversion trends among the six major land types in the YRDUA from 2000 to 2020. The results indicate that the conversion of cropland to construction land was the most prominent change across all five-year intervals, with large-scale encroachment on cropland, particularly during 2005–2010, posing a serious threat to the stability of regional grain production services. Furthermore, frequent mutual conversions were observed between cropland and water. Although conversions of forest land and grassland to construction land also occurred, their scale was relatively limited. Overall, sustained economic activity, population growth, and urbanization are associated with the continuous expansion of construction land at the expense of cropland, forest land, and water. This process not only disrupts regional ecological balance but also directly undermines the capacity of natural ecosystems such as forests and grasslands to provide critical services. As these fundamental ecological land covers are progressively eroded, the ecological condition of the region faces significant risks, and the supply level of its ecosystem services is projected to decline markedly, thereby further intensifying ecosystem service supply pressure in the region.

3.2 Analysis of key driving factors of land type changes
To examine the differential impacts of various driving factors on distinct land types, a driving factor analysis was separately conducted for each of the six land types using Random Forest feature importance analysis from the PLUS-LEAS module. As shown in Figure 4, the influence of drivers varies significantly across different land categories: Changes in cropland are jointly associated with slope, GDP, and population. Topographical constraints act as the primary limiting factor, while economic and demographic factors indirectly shape its spatial pattern through grain demand and circulation efficiency, the latter being influenced by proximity to major roads and railways. Changes in forest land are primarily associated with natural factors such as annual rainfall and DEM, consistent with its concentration in the mountainous areas of Zhejiang and Anhui Province, though human activities also exert a notable influence. Changes in grassland are most strongly linked to GDP, indicating that the dynamics of the relatively scarce grassland resources in this region area are primarily associated with human activities like economic development and urban greening. Changes in water areas are mainly driven by natural processes like rainfall and evapotranspiration, with anthropogenic factors playing a comparatively weaker role. The expansion of construction land shows the strongest association with the population factor, directly reflecting how urban population agglomeration may contribute to land urbanization. The distribution of unutilized land is highly correlated with annual potential evapotranspiration, with other natural and proximity factors also contributing, highlighting the inherent environmental characteristics of this vegetation-scarce land type.

3.3 Multi-scenario simulation of changes in ecosystem services
3.3.1 Current situation of ecosystem services
This study assessed the water conservation, carbon storage, soil conservation, and crop production in the YRDUA. The spatial distribution, at a 1 km pixel resolution, is shown in Figure 5, and the ecosystem service supply levels for the 26 cities are summarized in Table 6.

TABLE 6. Ecosystem service status of 26 cities in the YRDUA (2010–2020).
| City | Water conservation (108 m3) | Carbon storage (106 t) | Soil conservation (106 t) | Crop production (105 t) | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 2010 | 2015 | 2020 | 2010 | 2015 | 2020 | 2010 | 2015 | 2020 | 2010 | 2015 | 2020 | |
| Xuancheng | 72.43 | 92.36 | 74.06 | 33.37 | 33.09 | 33.25 | 27.24 | 32.04 | 48.75 | 13.35 | 13.09 | 13.17 |
| Wuhu | 11.87 | 16.21 | 13.65 | 10.26 | 9.93 | 10.06 | 1.78 | 1.83 | 3.22 | 17.55 | 16.85 | 17.15 |
| Chizhou | 70.23 | 77.92 | 65 | 20.57 | 20.55 | 20.5 | 26.84 | 31.79 | 41.59 | 10.26 | 10.15 | 10.08 |
| Tongling | 8.18 | 10.59 | 9.23 | 4.81 | 4.77 | 4.74 | 1.82 | 1.93 | 3.24 | 8.06 | 7.9 | 7.89 |
| Hefei | 10.18 | 14.55 | 14.59 | 16.17 | 15.85 | 15.7 | 2.01 | 1.81 | 3.74 | 30.3 | 29.68 | 29.4 |
| Maanshan | 4.51 | 6.75 | 6.47 | 6.31 | 6.26 | 6.24 | 1.05 | 0.95 | 2.09 | 12.74 | 12.6 | 12.54 |
| Chuzhou | 8.07 | 11.79 | 13.18 | 22.17 | 21.84 | 21.89 | 1.81 | 1.31 | 3.18 | 31.22 | 30.59 | 30.72 |
| Anqing | 61.53 | 70.23 | 71.87 | 28.97 | 29.04 | 28.98 | 40.04 | 35.43 | 64.53 | 23.95 | 23.81 | 23.73 |
| Zhenjiang | 2.04 | 3.17 | 3.85 | 5.5 | 5.43 | 5.31 | 0.41 | 0.36 | 0.93 | 10.51 | 10.39 | 10.19 |
| Yangzhou | 1.46 | 2.14 | 3.38 | 7.6 | 7.54 | 7.41 | 0.19 | 0.15 | 0.43 | 13.17 | 13.08 | 12.85 |
| Yancheng | 4.03 | 4.29 | 9.32 | 21.55 | 21.46 | 21.63 | 0.36 | 0.26 | 0.70 | 38.97 | 38.79 | 39.39 |
| Wuxi | 2.55 | 4.14 | 4.36 | 5.16 | 5.1 | 4.98 | 0.80 | 0.87 | 1.87 | 8.46 | 8.3 | 8.08 |
| Taizhou (Jiangsu) | 1.56 | 2.22 | 3.69 | 7.52 | 7.35 | 7.25 | 0.13 | 0.10 | 0.29 | 13.98 | 13.65 | 13.42 |
| Suzhou | 1.51 | 2.56 | 3.12 | 6.0 | 5.8 | 5.8 | 0.19 | 0.21 | 0.52 | 12.03 | 11.56 | 11.36 |
| Nantong | 3.43 | 5.03 | 7.68 | 13.27 | 12.87 | 12.85 | 0.15 | 0.13 | 0.39 | 27.13 | 26.28 | 26 |
| Changzhou | 2.49 | 4.06 | 4.1 | 5.5 | 5.44 | 5.29 | 0.33 | 0.34 | 0.75 | 12.63 | 12.43 | 11.98 |
| Nanjing | 4.04 | 6.43 | 6.62 | 8.75 | 8.71 | 8.42 | 0.91 | 0.81 | 1.94 | 13.54 | 13.46 | 12.84 |
| Shanghai | 1.49 | 2.19 | 2.59 | 7.1 | 6.77 | 6.33 | 0.09 | 0.09 | 0.26 | 16.81 | 16.06 | 14.77 |
| Huzhou | 17.66 | 24.37 | 21.38 | 13.81 | 13.67 | 13.48 | 6.32 | 7.38 | 13.32 | 10.25 | 9.99 | 9.65 |
| Jiaxing | 1.94 | 2.85 | 2.39 | 4.97 | 4.84 | 4.56 | 0.06 | 0.07 | 0.15 | 11.42 | 11.08 | 10.44 |
| Ningbo | 35.92 | 30.54 | 25.59 | 20.13 | 20.23 | 20.46 | 12.24 | 9.72 | 17.49 | 13.67 | 13.49 | 11.84 |
| Shaoxing | 45.13 | 41.75 | 31.74 | 21.34 | 21.16 | 21.05 | 13.42 | 11.72 | 19.44 | 11.06 | 10.56 | 10.4 |
| Taizhou (Zhejiang) | 78.69 | 67.52 | 43.85 | 26.2 | 26.12 | 25.85 | 30.39 | 27.95 | 37.67 | 10.99 | 10.51 | 10.27 |
| Zhoushan | 1.95 | 2.03 | 2.16 | 2.46 | 2.72 | 2.6 | 0.70 | 0.65 | 0.87 | 1.65 | 1.74 | 1.15 |
| Jinhua | 95.86 | 84.35 | 56.97 | 30.19 | 30.09 | 29.7 | 31.92 | 28.59 | 40.98 | 14.16 | 13.79 | 13.28 |
| Hangzhou | 135.48 | 145.59 | 112.54 | 47.86 | 47.65 | 47.25 | 53.79 | 58.09 | 90.58 | 13.32 | 12.52 | 11.92 |
| YRDUA | 684.24 | 735.64 | 613.38 | 397.52 | 394.24 | 391.55 | 255.01 | 254.58 | 398.90 | 401.16 | 392.31 | 384.52 |
In terms of water conservation, the maximum pixel-based water yield was 2345.1 mm in 2010 and decreased to 1995.3 mm in 2020. Spatially, pixels with high water yield became significantly more concentrated around Taihu Lake in 2020, primarily due to the expansion of construction land areas in cities like Shanghai, Suzhou, and Wuxi to meet urban development and population needs. Additionally, pixels with high water yield capacity were mainly located in southern Anhui Province and western Zhejiang Province, where forest ecosystems play a role in storing and conserving natural rainfall and surface water resources. In terms of physical volume, Hangzhou had the highest total water conservation volume, 135.48 × 108 m3 in 2010, followed by Jinhua and Taizhou. Zhoushan had the lowest, 1.95 × 108 m3, due to its limited land area. Cities with high total water conservation volume were primarily in Anhui and Zhejiang provinces, where larger administrative areas and higher forest coverage contribute to greater aggregate water yield, while Jiangsu and Shanghai, with less forest and grassland coverage, lagged significantly. By 2020, Hangzhou remained the highest, 112.54 × 108 m3, followed by Xuancheng and Anqing. Overall, total water conservation volume in the YRDUA decreased compared to 2010, largely due to urban expansion encroaching on vegetated areas.
For carbon storage, the spatial concentration of carbon storage pixels showed little change across the three time points. High-value pixels were consistently concentrated in the forested mountainous areas of southern Anhui and western Zhejiang, as forests and grasslands are primary natural carbon sinks. The maximum pixel value remained 1192.4 t/pixel for all 3 years. Pixels with significant carbon storage changes were mainly found around Shanghai, Suzhou, Hangzhou Bay, and Nanjing, resulting from urbanization replacing natural ecosystems. In terms of physical supply, Hangzhou and Xuancheng had the highest total carbon storage volumes among the 26 cities in both 2010 and 2020, largely due to their larger land areas and extensive forest coverage. A comparative analysis from 2010 to 2020 revealed a continuous decline in carbon storage in cities such as Yangzhou, Wuxi, Zhenjiang, Shanghai, Hangzhou, Jinhua, and Shaoxing. Shanghai experienced the largest decrease, 7.67 × 105 t, reflecting the impact of economic and urban development on ecosystem services.
Regarding soil conservation, the soil conservation service calculated by the InVEST SDR module, higher soil conservation values indicate that the ecosystem retains more soil, i.e., avoids more soil loss, reflecting stronger service provision capacity. The maximum pixel value increased from 15,162.4 t/pixel in 2010 to 232,544.4 t/pixel in 2020, reflecting both enhanced soil retention capacity and increased potential soil erosion pressure due to changes in rainfall and land-use conditions. Pixels with high soil conservation capacity were concentrated in the mountainous areas of southern Anhui and western Zhejiang, where forest vegetation plays a crucial role in preventing soil erosion. In 2010, Hangzhou had the highest total soil conservation volume, 53.79 × 106 t, followed by Anqing and Jinhua. By 2020, the spatial pattern remained similar, but the physical supply of soil conservation services increased across most cities due to rising potential soil erosion.
For crop production, the maximum potential yield per pixel remained relatively stable during the study period, peaking at 51.8 t/pixel in 2020. Pixels with high production potential were concentrated in the central part of the urban agglomeration, along the Yangtze River and Taihu Lake water networks, with particularly dense distribution in the Subei Plain. In contrast, pixels in Zhejiang Province were more scattered due to limited arable land. Overall crop production in 2015 was lower than in 2010 and 2020. In 2020, Yancheng had the highest total crop production, 39.39 × 105 t, reflecting its extensive arable land in the Subei Plain, followed by Chuzhou, 30.72 × 105 t. Zhoushan had the lowest, 1.15 × 105 t, while Tongling and Wuxi also had relatively low supplies.
3.3.2 Multi-scenario prediction results of land use change
Based on 2020 land cover data from the YRDUA, the accuracy of the PLUS model for multi-scenario forecasting was validated (Supplementary Appendix A1). Building on the analysis of driving factors, land use changes under three scenarios—baseline (current situation), economic development priority, and ecological protection priority—were simulated for the years 2030 and 2060. The spatial distribution of the simulation results is shown in Figure 6, and a comparative area statistic by land use type is provided in Table 7. The previously established model for quantifying the supply of ecosystem services was applied to predict changes under these multiple scenarios.

TABLE 7. Projected area of land-use types under different scenarios in the YRDUA, unit: km2.
| Types | Area in 2020 | Area in 2030 | Area in 2060 | |||||
|---|---|---|---|---|---|---|---|---|
| Actual | Predicted | Scenario 1 | Scenario 2 | Scenario 3 | Scenario 1 | Scenario 2 | Scenario 3 | |
| Cropland | 97692.92 | 97702.11 | 94658.49 | 94478.49 | 94613.49 | 89666.28 | 87917.49 | 88097.49 |
| Forest land | 56969.31 | 56957.31 | 56697.48 | 56919.69 | 57196.98 | 56313.81 | 57010.05 | 57276.27 |
| Grassland | 7519.88 | 7112.97 | 7846.22 | 7325.46 | 7573.59 | 7179.39 | 7365.96 | 7614.99 |
| Water | 18957.90 | 18589.48 | 18925.11 | 19089.09 | 18941.04 | 18865.53 | 19494.09 | 19457.73 |
| Construction land | 29144.26 | 29149.83 | 32183.73 | 32498.73 | 32003.73 | 38298.15 | 38523.15 | 37893.15 |
| Unutilized land | 275.64 | 185.13 | 277.92 | 277.47 | 260.11 | 265.77 | 278.19 | 249.30 |
Comparison with 2020 land use data shows certain deviations in the simulation results: cropland area is overestimated by 9.19 km2, forest land is underestimated by 12 km2, construction land area is overestimated by 5.57 km2, and unutilized land is significantly reduced by 90.51 km2. The primary prediction errors lie in the estimation of water bodies and grassland, with grassland underestimated by 406.91 km2 and water bodies underestimated by 368.42 km2 compared to the actual data.
Under the baseline scenario, urbanization and expansion within the YRDUA are the main drivers of reductions in other land types, with cropland experiencing the most significant loss. By 2030, construction land area is projected to increase by 3,039.37 km2 compared to 2020, while cropland decreases by 3,034.43 km2, forest land by 271.83 km2, and water bodies by 32.79 km2. Unutilized land remains relatively stable, increasing slightly by 2.28 km2. The degradation of some forest areas leads to their conversion into grassland, which has a lower ecosystem service capacity, resulting in an increase of 326.34 km2 in grassland area. By 2060, the expansion of construction land areas intensifies further, increasing by 9,153.89 km2 compared to 2020, while cropland, forest land, and grassland decrease by 8,026.64 km2, 655.50 km2, and 340.49 km2, respectively.
Under the economic development priority scenario, the rate of urbanization and expansion exceeds that of the natural development scenario. By 2030, construction land area increases by 3,354.47 km2 compared to 2020, while cropland, forest land, and grassland decrease by 3,214.43 km2, 49.62 km2, and 194.42 km2, respectively. By 2060, urban expansion further encroaches on other land types, resulting in a total increase of 9,378.89 km2 in construction land area and decreases of 9,775.43 km2 in cropland and 153.92 km2 in grassland compared to 2020.
Under the ecological protection priority scenario, the implementation of protection policies for natural land types such as forests and grasslands effectively restricts urban encroachment and development, yielding significant ecological benefits. By 2030, the expansion of construction land area is considerably slower than in other scenarios, increasing by only 2,859.47 km2 compared to 2020. Forest and grassland areas increase by 227.67 km2 and 53.71 km2, respectively, while cropland decreases by 3,079.43 km2. By 2060, the total construction land area increases by 8,748.89 km2, cropland decreases by 9,595.43 km2, and forest and grassland increase by 306.96 km2 and 95.11 km2, respectively.
3.3.3 Prediction results of ecosystem services under different scenarios
Based on the simulated land use changes under various scenarios in the YRDUA, the physical supply of four ecosystem services was calculated using the previously established quantification method. This allowed for further analysis of the changing characteristics of ecosystem service provision in the region.
The results of the physical water conservation volume by prefectural city are shown in Table 8. The data indicate that in 2030, the total water conservation service under the natural development scenario is 53.5176 billion m3, compared to 51.3119 billion m3 under the economic development priority scenario and 57.6333 billion m3 under the ecological protection priority scenario. Compared to the historical baseline year of 2020, the region’s water conservation capacity shows varying degrees of decline under all three 2030 scenarios. This reduction is attributed to the expansion of urban built-up areas and the encroachment on forest land, which severely impairs the water conservation capacity of the original landscapes. For the 2030 and 2060 projections, climate variables (precipitation, temperature, evapotranspiration) are held constant at 2020 levels, and only land-use patterns change based on PLUS scenario projections. Thus, the projections isolate the effect of land-use pattern changes on ecosystem services under current climate conditions. However, by 2060, simulation results suggest an improvement in ecological condition and that water yield may surpass 2020 levels. It should be noted that an increase in water yield (annual water production) does not necessarily indicate improved water conservation service; it may reflect increased surface runoff due to expanded impervious surfaces, rather than enhanced ecological water storage capacity. Cities with significant forest coverage, such as Xuancheng, Hangzhou, and Anqing, exhibit notable variations in water conservation volumes across scenarios, with values under the ecological protection priority scenario being significantly higher than those under the economic development priority scenario. The multi-scenario simulations suggest that ecological protection policies and curbing excessive construction and environmental degradation in the YRDUA may contribute to ecological restoration and enhance the region’s ecosystem service capacity.
TABLE 8. Prediction results of water yield in the YRDUA unit: 108 m3.
| City | 2020 | Scenario 1baseline | Scenario 2economic priority | Scenario 3ecological priority | |||
|---|---|---|---|---|---|---|---|
| 2030 | 2060 | 2030 | 2060 | 2030 | 2060 | ||
| Xuancheng | 74.06 | 63.15 | 64.89 | 60.51 | 62.00 | 68.19 | 68.37 |
| Wuhu | 13.65 | 12.08 | 29.47 | 11.60 | 28.30 | 12.98 | 31.02 |
| Tongling | 9.23 | 8.31 | 16.32 | 7.98 | 15.67 | 8.96 | 17.17 |
| Hefei | 14.59 | 13.12 | 53.02 | 12.67 | 51.07 | 14.12 | 55.28 |
| Maanshan | 6.47 | 5.70 | 16.76 | 5.47 | 16.06 | 6.12 | 17.46 |
| Chuzhou | 13.18 | 11.72 | 32.49 | 11.34 | 31.76 | 12.60 | 34.42 |
| Anqing | 71.87 | 63.57 | 83.03 | 60.91 | 79.35 | 68.53 | 87.17 |
| Zhenjiang | 3.85 | 3.52 | 18.44 | 3.40 | 17.55 | 3.82 | 19.24 |
| Yangzhou | 3.38 | 3.03 | 23.02 | 2.91 | 22.06 | 3.26 | 23.88 |
| Yancheng | 9.32 | 8.25 | 42.35 | 7.91 | 40.26 | 8.90 | 44.10 |
| Wuxi | 4.36 | 3.90 | 22.23 | 3.76 | 21.24 | 4.22 | 23.26 |
| Taizhou (Jiangsu) | 3.69 | 3.31 | 23.48 | 3.17 | 22.36 | 3.55 | 24.34 |
| Suzhou | 3.12 | 2.84 | 33.51 | 2.73 | 31.95 | 3.06 | 35.18 |
| Nantong | 7.68 | 6.78 | 33.63 | 6.51 | 32.03 | 7.30 | 35.18 |
| Changzhou | 4.10 | 3.70 | 22.03 | 3.55 | 21.04 | 3.97 | 22.99 |
| Nanjing | 6.62 | 5.93 | 32.53 | 5.71 | 31.02 | 6.37 | 33.97 |
| Shanghai | 2.59 | 2.32 | 32.10 | 2.24 | 30.53 | 2.51 | 33.49 |
| Huzhou | 21.38 | 18.54 | 27.43 | 17.86 | 26.23 | 20.02 | 28.88 |
| Jiaxing | 2.39 | 2.24 | 23.56 | 2.16 | 22.54 | 2.42 | 24.69 |
| Ningbo | 25.59 | 22.50 | 35.51 | 21.64 | 34.15 | 24.23 | 37.49 |
| Shaoxing | 31.74 | 27.61 | 35.09 | 26.64 | 33.76 | 29.79 | 37.06 |
| Taizhou (Zhejiang) | 43.85 | 37.79 | 41.09 | 36.31 | 39.36 | 40.83 | 43.33 |
| Zhoushan | 2.16 | 1.89 | 2.77 | 1.82 | 2.64 | 2.05 | 2.90 |
| Jinhua | 56.97 | 48.91 | 56.72 | 47.01 | 54.19 | 52.78 | 59.52 |
| Hangzhou | 112.54 | 97.83 | 97.93 | 93.63 | 92.57 | 105.28 | 101.92 |
| Chizhou | 65.00 | 56.65 | 59.05 | 53.70 | 55.23 | 60.49 | 60.83 |
| Total | 613.38 | 535.18 | 958.44 | 513.12 | 914.88 | 576.33 | 1003.12 |
Table 9 presents the simulated physical supply of carbon storage services for cities in the YRDUA under three development scenarios. Similar to the water conservation results, the region’s carbon storage capacity in 2030 declines compared to the 2020 level across all scenarios. This reduction is attributed to the significant loss of vegetation, particularly forests and grasslands, key land cover types for carbon storage, due to continued expansion of built-up areas, which impairs the ecosystem’s ability to absorb and store carbon dioxide. In the economic development priority scenario, total carbon storage decreases by 60.78 × 106 t; under the baseline scenario, it falls by 40.60 ×106 t; while the smallest reduction of 24.64 × 106 t occurs under the ecological protection scenario.
TABLE 9. Prediction results of carbon storage in the YRDUA unit: 106 t.
| City | 2020 | Scenario 1baseline | Scenario 2economic priority | Scenario 3ecological priority | |||
|---|---|---|---|---|---|---|---|
| 2030 | 2060 | 2030 | 2060 | 2030 | 2060 | ||
| Xuancheng | 33.25 | 30.24 | 29.20 | 28.48 | 27.43 | 31.74 | 30.48 |
| Wuhu | 10.06 | 9.00 | 8.10 | 8.46 | 7.85 | 9.40 | 8.68 |
| Tongling | 4.74 | 4.26 | 3.91 | 3.98 | 3.72 | 4.44 | 4.14 |
| Hefei | 15.70 | 13.79 | 12.21 | 12.95 | 11.50 | 14.41 | 12.85 |
| Maanshan | 6.24 | 5.58 | 5.12 | 5.24 | 4.84 | 5.83 | 5.39 |
| Chuzhou | 21.89 | 19.68 | 19.14 | 18.47 | 17.29 | 20.53 | 19.18 |
| Anqing | 28.98 | 26.03 | 24.80 | 24.56 | 23.14 | 27.19 | 25.56 |
| Zhenjiang | 5.31 | 4.63 | 4.05 | 4.33 | 3.80 | 4.82 | 4.23 |
| Yangzhou | 7.41 | 6.56 | 5.93 | 6.17 | 5.54 | 6.85 | 6.16 |
| Yancheng | 21.63 | 19.36 | 17.87 | 18.15 | 16.81 | 20.18 | 18.63 |
| Wuxi | 4.98 | 4.37 | 3.86 | 4.10 | 3.63 | 4.55 | 4.02 |
| Taizhou (Jiangsu) | 7.25 | 6.41 | 5.78 | 6.05 | 5.44 | 6.70 | 6.02 |
| Suzhou | 5.79 | 5.02 | 4.34 | 4.73 | 4.07 | 5.23 | 4.46 |
| Nantong | 12.85 | 11.50 | 10.63 | 10.84 | 10.10 | 12.00 | 11.15 |
| Changzhou | 5.29 | 4.61 | 4.04 | 4.34 | 3.79 | 4.83 | 4.21 |
| Nanjing | 8.42 | 7.41 | 6.67 | 6.94 | 6.24 | 7.76 | 6.95 |
| Shanghai | 6.33 | 5.51 | 4.79 | 5.19 | 4.55 | 5.74 | 5.03 |
| Huzhou | 13.47 | 12.17 | 11.33 | 11.46 | 10.86 | 12.68 | 11.96 |
| Jiaxing | 4.56 | 3.76 | 2.84 | 3.52 | 2.67 | 3.91 | 2.97 |
| Ningbo | 20.46 | 18.43 | 16.66 | 17.35 | 16.41 | 19.23 | 18.11 |
| Shaoxing | 21.05 | 19.02 | 17.59 | 17.88 | 17.00 | 19.83 | 18.78 |
| Taizhou (Zhejiang) | 25.85 | 23.47 | 22.54 | 22.09 | 21.17 | 24.48 | 23.39 |
| Zhoushan | 2.60 | 2.37 | 2.26 | 2.23 | 2.15 | 2.47 | 2.37 |
| Jinhua | 29.70 | 26.91 | 25.56 | 25.36 | 24.26 | 28.07 | 26.78 |
| Hangzhou | 47.25 | 42.65 | 39.38 | 40.37 | 38.68 | 44.65 | 42.63 |
| Chizhou | 20.50 | 18.20 | 17.05 | 17.53 | 16.81 | 19.39 | 18.54 |
| Total | 391.55 | 350.95 | 325.64 | 330.76 | 309.73 | 366.91 | 342.69 |
Unlike the trend observed for water conservation services, the region’s carbon storage capacity does not recover over time. Damage to forest vegetation may be difficult to reverse, leading to a further weakening of overall carbon storage by 2060 under all three scenarios compared to both 2020 and 2030 levels. However, the trends in carbon storage capacity among cities vary significantly across scenarios. Under the ecological protection scenario, cities with stronger ecological foundations, such as Xuancheng, Anqing, Chizhou, and Hangzhou, are able to restore their carbon storage capacity to the level projected under the 2030 natural development scenario, or even exceed it in terms of physical supply.
Ecosystem soil conservation service is also directly linked to the type and density of surface vegetation cover. The simulation results for the YRDUA under the three development scenarios are shown in Table 10. Similar to the carbon storage simulations, the soil conservation capacity of the ecosystem exhibits a declining trend across all cities in the region due to the destruction of forest vegetation, with Jiangsu Province and Shanghai, areas with relatively poor forest resources, experiencing the most pronounced declines. For cities in Anhui and Zhejiang provinces with a higher proportion of mountainous forests, the decrease in the physical supply of soil conservation service under the economic development priority scenario is significantly greater than under the other two scenarios. By 2060, the decline in soil conservation becomes even more severe across all regions. However, under the ecological protection priority scenario, the decrease in soil retention capacity can be mitigated, and the supply provided by the ecosystem is significantly higher than under the economic development priority scenario.
TABLE 10. Prediction results of soil conservation in the YRDUA unit: 106 t.
| City | 2020 | Scenario 1baseline | Scenario 2economic priority | Scenario 3ecological priority | |||
|---|---|---|---|---|---|---|---|
| 2030 | 2060 | 2030 | 2060 | 2030 | 2060 | ||
| Xuancheng | 48.75 | 43.49 | 41.63 | 41.02 | 39.57 | 45.33 | 43.61 |
| Wuhu | 3.22 | 2.92 | 2.79 | 2.75 | 2.66 | 3.04 | 2.93 |
| Tongling | 3.24 | 2.94 | 2.81 | 2.77 | 2.68 | 3.06 | 2.95 |
| Hefei | 3.74 | 3.37 | 3.23 | 3.18 | 3.07 | 3.51 | 3.38 |
| Maanshan | 2.09 | 1.89 | 1.81 | 1.79 | 1.72 | 1.97 | 1.90 |
| Chuzhou | 3.18 | 2.85 | 2.74 | 2.68 | 2.59 | 2.96 | 2.85 |
| Anqing | 64.53 | 57.80 | 55.49 | 54.54 | 52.60 | 60.25 | 57.96 |
| Zhenjiang | 0.93 | 0.84 | 0.81 | 0.79 | 0.77 | 0.88 | 0.85 |
| Yangzhou | 0.42 | 0.37 | 0.36 | 0.35 | 0.34 | 0.39 | 0.38 |
| Yancheng | 0.70 | 0.62 | 0.59 | 0.58 | 0.56 | 0.64 | 0.62 |
| Wuxi | 1.86 | 1.69 | 1.62 | 1.59 | 1.54 | 1.76 | 1.70 |
| Taizhou (Jiangsu) | 0.28 | 0.25 | 0.24 | 0.23 | 0.23 | 0.26 | 0.25 |
| Suzhou | 0.52 | 0.46 | 0.44 | 0.44 | 0.42 | 0.48 | 0.47 |
| Nantong | 0.39 | 0.34 | 0.33 | 0.32 | 0.31 | 0.36 | 0.35 |
| Changzhou | 0.75 | 0.67 | 0.64 | 0.63 | 0.61 | 0.70 | 0.68 |
| Nanjing | 1.94 | 1.76 | 1.68 | 1.66 | 1.60 | 1.83 | 1.77 |
| Shanghai | 0.26 | 0.23 | 0.22 | 0.22 | 0.21 | 0.24 | 0.24 |
| Huzhou | 13.32 | 11.98 | 11.47 | 11.30 | 10.90 | 12.48 | 12.01 |
| Jiaxing | 0.15 | 0.13 | 0.13 | 0.12 | 0.12 | 0.14 | 0.13 |
| Ningbo | 17.49 | 15.60 | 14.88 | 14.71 | 14.19 | 16.25 | 15.64 |
| Shaoxing | 19.44 | 17.32 | 16.55 | 16.34 | 15.76 | 18.05 | 17.36 |
| Taizhou (Zhejiang) | 37.67 | 33.91 | 32.44 | 31.98 | 30.86 | 35.34 | 34.00 |
| Zhoushan | 0.87 | 0.79 | 0.75 | 0.74 | 0.72 | 0.82 | 0.79 |
| Jinhua | 40.98 | 36.82 | 35.21 | 34.73 | 33.51 | 38.37 | 36.91 |
| Hangzhou | 90.57 | 81.31 | 77.63 | 76.72 | 74.01 | 84.75 | 81.53 |
| Chizhou | 41.59 | 37.28 | 35.72 | 35.21 | 33.97 | 38.90 | 37.42 |
| Total | 398.90 | 357.63 | 342.20 | 337.41 | 325.52 | 372.79 | 358.66 |
In the multi-scenario simulations of land use change, cropland patches show significant reduction across all three scenarios compared to 2020. Besides forests and grasslands, urban expansion primarily encroaches on cropland, leading to a decline in the region’s ecosystem service of crop production. The simulation results confirm this trend. As shown in Table 11, the physical crop production in the YRDUA decreases markedly under all three scenarios. Compared to 2020 levels, the total crop production under the natural development scenario decreases by 46.21 × 105 t in 2030, while the economic development priority scenario results in a reduction of 66.07 × 105 t, and the ecological protection priority scenario shows a smaller decrease of 32.16 × 105 t. By 2060, the ecosystem’s crop production capacity further weakens. Under the baseline scenario, the region’s crop production decreases by 77.28 × 105 t compared to 2020. Without ecological protection policies, accelerated urban expansion and further loss of cropland would lead to a reduction of 99.89 × 105 t by 2060. However, by restricting the expansion of built-up areas and protecting natural land covers such as forests and grasslands, this declining trend can be mitigated. Under the ecological priority scenario, the total crop production in 2060 decreases by only 70.17 × 105 t compared to 2020, performing better than the baseline scenario.
TABLE 11. Prediction results of crop production in the YRDUA unit: 105 t.
| City | 2020 | Scenario 1baseline | Scenario 2economic priority | Scenario 3ecological priority | |||
|---|---|---|---|---|---|---|---|
| 2030 | 2060 | 2030 | 2060 | 2030 | 2060 | ||
| Xuancheng | 13.17 | 11.83 | 10.96 | 11.23 | 10.57 | 11.89 | 11.13 |
| Wuhu | 17.15 | 15.22 | 14.59 | 14.32 | 13.06 | 15.91 | 14.44 |
| Tongling | 7.89 | 7.03 | 6.68 | 6.60 | 6.01 | 7.34 | 6.66 |
| Hefei | 29.40 | 25.74 | 22.79 | 24.17 | 21.26 | 26.89 | 23.78 |
| Maanshan | 12.54 | 11.15 | 10.37 | 10.49 | 9.52 | 11.66 | 10.59 |
| Chuzhou | 30.72 | 27.43 | 24.68 | 25.77 | 23.82 | 28.64 | 26.44 |
| Anqing | 23.73 | 20.78 | 18.46 | 19.60 | 17.40 | 21.68 | 19.27 |
| Zhenjiang | 10.19 | 8.76 | 7.21 | 8.21 | 6.93 | 9.08 | 7.67 |
| Yangzhou | 12.85 | 11.38 | 10.27 | 10.72 | 9.61 | 11.88 | 10.69 |
| Yancheng | 39.40 | 35.21 | 32.40 | 33.16 | 30.59 | 36.70 | 33.77 |
| Wuxi | 8.08 | 6.97 | 5.88 | 6.54 | 5.51 | 7.25 | 6.11 |
| Taizhou (Jiangsu) | 13.42 | 11.87 | 10.72 | 11.20 | 10.09 | 12.41 | 11.17 |
| Suzhou | 11.36 | 9.78 | 8.37 | 9.23 | 7.82 | 10.21 | 8.57 |
| Nantong | 26.00 | 23.23 | 21.37 | 21.89 | 20.30 | 24.24 | 22.41 |
| Changzhou | 11.98 | 10.29 | 8.63 | 9.70 | 8.17 | 10.77 | 9.03 |
| Nanjing | 12.84 | 11.13 | 9.52 | 10.45 | 9.05 | 11.63 | 10.02 |
| Shanghai | 14.77 | 12.81 | 11.06 | 12.09 | 10.51 | 13.34 | 11.65 |
| Huzhou | 9.65 | 8.57 | 8.14 | 8.04 | 7.31 | 8.92 | 8.03 |
| Jiaxing | 10.44 | 8.52 | 6.32 | 7.99 | 5.93 | 8.85 | 6.59 |
| Ningbo | 11.84 | 10.25 | 10.47 | 9.65 | 8.40 | 10.72 | 9.29 |
| Shaoxing | 10.40 | 9.03 | 8.99 | 8.47 | 7.41 | 9.40 | 8.19 |
| Taizhou (Zhejiang) | 10.27 | 9.09 | 8.25 | 8.59 | 7.82 | 9.43 | 8.55 |
| Zhoushan | 1.15 | 1.05 | 1.00 | 0.99 | 0.95 | 1.09 | 1.05 |
| Jinhua | 13.28 | 11.78 | 10.91 | 11.06 | 10.08 | 12.25 | 11.14 |
| Hangzhou | 11.92 | 10.41 | 10.66 | 9.81 | 8.67 | 10.85 | 9.55 |
| Chizhou | 10.08 | 9.00 | 8.52 | 8.48 | 7.81 | 9.33 | 8.56 |
| Total | 384.52 | 338.31 | 307.24 | 318.45 | 284.63 | 352.36 | 314.35 |
4 Discussion
4.1 Urban expansion and regional ecological imbalance risks
From 2000 to 2020, the YRDUA witnessed a nonlinear, tightly coupled relationship between urban expansion and land use change. Continuous construction land expansion is associated with sharp cropland loss. The pattern of ‘urban encroachment on cropland’ was primarily associated with regional land use change throughout the study period. Later ecological policies restored small parts of forest and grassland to build ecological security barriers, but the scale and speed failed to offset cropland loss and habitat degradation caused by urbanization inertia. This unbalanced land competition reflects path dependence of the traditional growth model relying on land finance and spatial expansion.
From a landscape ecology perspective, this process reshaped regional landscape patterns and degraded ecological functions. It aggravated natural landscape fragmentation, reduced landscape connectivity, and strengthened construction land dominance, forming a sprawling urban spatial structure. Such changes broke ecological process integrity, blocked species migration, and disrupted water and nutrient cycles, posing long-term risks to regional ecological condition. This shift is associated with socioeconomic needs, infrastructure layout and natural conditions, reflecting trade-offs between economic growth, food security and ecological protection. Urban-driven land change is associated with multi-dimensional ecosystem service declines. Core cities saw declining water conservation and carbon storage; ecologically fragile areas faced higher soil erosion risks. Service supply concentrated in peripheral ecological zones, while core metropolitan areas experienced the most pronounced service declines, creating spatial pressure on ecosystem service supply. It should be noted that inter-city comparisons in this study are based on total ecosystem service volumes within each administrative boundary, reflecting each city’s aggregate contribution to regional supply an approach relevant to cross-jurisdictional ecological compensation and regional ecological security planning. Total-volume comparisons do not directly indicate ecological quality or service provision intensity per unit area. Coordinated multi-objective management of ecosystem services has become critical for regional sustainable development under the Dual Carbon goals.
4.2 Influencing factors and mechanisms of land use change
Land use transitions in the YRDUA reflect complex human-land interactions under rapid urbanization. Driving forces differ distinctly across land types. Cropland change is limited by slope but mainly associated with GDP growth and population agglomeration. Forest distribution is strongly associated with annual rainfall and topography, yet pressured by infrastructure expansion. Grassland dynamics correlate strongly with GDP, while construction land expansion links closely to population. This significant divergence in driving forces suggests that natural geographical elements form a “rigid” constraint framework for regional development, while human activities exert “steering” and “intensifying” effects upon this natural baseline.
This significant divergence in driving forces demonstrates that natural geographical elements form a rigid constraint framework for regional development, while human activities exert “steering” and “intensifying” effects upon this natural baseline. Through nonlinear interactions, these elements collectively shape the regional landscape pattern. Natural factors establish the possibility boundaries for land use conversion, while socioeconomic factors determine the direction and intensity of conversion by altering resource demands and circulation efficiency. This complex driving mechanism indicates that the land use system in urban agglomerations represents a typical multiple-stress system, whose evolutionary trajectory is co-determined by the continuous feedback between natural baseline conditions and socioeconomic processes.
4.3 Urban agglomerations ecological risk prevention based on multi-scenario prediction
Multi-scenario simulation of land use change and ecosystem services provides critical scientific support for ecological governance in the YRDUA. This study applied the PLUS model to project land use patterns and corresponding ecological dynamics for 2030 and 2060 under three targeted scenarios: natural development, economic priority, and ecological priority. Simulation results reveal sharp divergence in ecological outcomes. By 2060, the natural development and economic priority scenarios are projected to drive construction land expansion to approximately 9,150 km2, triggering a loss of roughly 9,000 km2 of cropland and widespread degradation of key ecosystem services, especially substantial declines in carbon storage. In contrast, the ecological priority scenario restrains construction land to 8,750 km2, effectively protects and slightly expands forest and grassland areas, and significantly mitigates ecosystem service degradation. These findings show that while ecological policies cannot entirely prevent degradation during urbanization, they may contribute to mitigating its impacts, especially on carbon sequestration and soil retention. The study further reveals that ecosystem services exhibit varying sensitivities to land use changes, with carbon storage showing limited recovery potential once disturbed. Model underestimation of water bodies and grasslands highlights the need for improved parameterization of hydrological and vegetation processes. Future research should prioritize next-generation models that integrate multi-agent systems and deep learning to better simulate human-environment interactions. Developing quantitative frameworks for assessing cross-scale ecosystem service trade-offs, coupled with predictive early-warning systems, can enable adaptive spatial governance through dynamic ecological protection lines—supporting sustainable urban development.
4.4 Limitations and prospects
This study has several limitations. First, the 1 km resolution remote sensing data restricts land use simulation accuracy, especially for grassland and water bodies; interpolation uncertainties of meteorological data also affect assessment precision. Second, inter-city comparisons are based on total ecosystem service volumes within administrative boundaries, which are inherently influenced by city area size; higher total values should not be interpreted as stronger per-unit-area service provision capacity. Others, the FoM value of 0.144 suggests that the precise spatial location of future land-use changes carries some uncertainty, and the 2030 and 2060 projections should be interpreted as scenario-dependent trend projections rather than precise spatial predictions. Future projections do not consider climate change impacts, reflecting only the isolated effect of land-use pattern changes; actual future ecosystem services will also be influenced by climate change, CO2 fertilization, and other factors. The crop production assessment did not differentiate among crop types (e.g., rice, wheat, maize) and relied on comprehensive NDVI for total grain production spatial allocation, which may introduce uncertainty in areas with diverse cropping systems.
Future research will address these gaps: expand to other urban agglomerations for cross-regional comparison; integrate longer-term data to deepen trend analysis; develop hybrid models coupling process-based methods and machine learning; optimize ecological project evaluation and spatial governance strategies, to support high-quality urban agglomeration development.
5 Conclusion
Based on a systematic analysis of land use dynamics (2000–2020) and ecosystem service assessment (2010–2020) in the YRDUA, core findings can be summarized as follows: (1) Land use change exhibited a clear pattern of cropland conversion to construction land. During 2000–2005, cropland experienced a net loss of 3,331.91 km2, with 3,163.90 km2 converted to construction land, marking the dominant conversion path. This trend persisted through 2020, while construction land expanded by 1,756.08 km2 in 2015–2020 alone. (2) The drivers of land use change varied significantly across land types. Cropland changes were jointly influenced by slope and socioeconomic factors, while construction land expansion correlated most strongly with population. Forest distribution is primarily associated with natural factors including annual rainfall and DEM. (3) Multi-scenario projections revealed substantial ecological risks and mitigation potential. Continuing current trends would lead to construction land expansion exceeding 9,000 km2 by 2060, associated with substantial carbon storage decline, e.g., 60.78 × 106 t decrease by 2030 under economic priority scenario. However, compared with the economic priority scenario (60.78 × 106 t decrease by 2030), the ecological priority scenario reduces carbon storage loss to 24.64 × 106 t, representing a reduction of approximately 60%, while maintaining higher water supply capacity. These findings underscore the necessity of a diagnosis and simulation framework that can inform spatial governance and ecological regulation decisions, enable dynamic optimization of ecological security patterns while balance development needs in urban agglomerations.
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Supplementary material
The Supplementary Material for this article can be found online at: https://www.frontiersin.org/articles/10.3389/fenvs.2026.1908887/full#supplementary-material
Supplementary material Supplementary material at the source
Footnotes
Edited by: Merja H Tölle, University of Kassel, Germany
Reviewed by: Quanzhi Li, China University of Mining and Technology, Beijing, China
Jianyu Liao, Hunan University of Technology, China
Statements
- Conflict of interest
The author(s) declared that this work was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
- Funding
The author(s) declared that financial support was received for this work and/or its publication. This research was supported by Youth Fund for Humanities and Social Sciences Research of the Chinese Ministry of Education (Grant NO. 25YJCZH210); Suzhou Social Science Fund Project (Applied Countermeasures Category) (Project No.: Y2026LX211); Scientific research planning Project of Jiangsu Open University (Grant NO. 2021-C-03); High-Level Talent Supporting Fund of Suzhou Institute of Trade and Commerce (Grant NO. 705S104).
- Data availability
The original contributions presented in the study are included in the article/Supplementary Material, further inquiries can be directed to the corresponding author.
- Author contributions
AC: Methodology, Writing – original draft. QS: Supervision, Writing – review and editing. MZ: Project administration, Supervision, Writing – review and editing. ZS: Project administration, Writing – review and editing. KH: Methodology, Writing – review and editing.
- Acknowledgements
We thank the reviewers and editors during the review process.
References
- Ai X., Zheng X., Zhang Y., Liu Y., Ou X., Xia C. (2024). Climate and land use changes impact the trajectories of ecosystem service bundles in an urban agglomeration: intricate interaction trends and driver identification under SSP-RCP scenarios. Sci. Total Environment 944, 173828. doi:10.1016/j.scitotenv.2024.173828
- Bagstad K. J., Semmens D. J., Diffendorfer J. E., Mattsson B. J., Dubovsky J., Thogmartin W. E. (2019). Ecosystem service flows from a migratory species: spatial subsidies of the northern pintail. Ambio 48 (1), 61 – 73. doi:10.1007/s13280-018-1049-4
- Gou J. J., Miao C. Y., Samaniego L., Xiao M., Wu J., Guo X. (2021). CNRD v1.0: a high-quality natural runoff dataset for hydrological and climate studies in China. Bull. Am. Meteorological Soc. 102 (5), E929 – E947. doi:10.1175/bams-d-20-0094.1
- Han J. Y., Miao C. Y., Gou J. J., Zheng H., Zhang Q., Guo X. (2023). A new daily gridded precipitation dataset based on gauge observations across mainland China. Earth Syst. Sci. Data 15 (7), 3147 – 3161. doi:10.5194/essd-15-3147-2023
- Herdt T., Wälty S. (2026). Revisiting density: the impact of CIAM on Zurich's plans for sustainable urban growth. Cities 169, 106539. doi:10.1016/j.cities.2025.106539
- Jessica C., Almeida I. Y., Katrin F., Floria A. D., Florian D., Mario K. (2022). Synergies and trade-offs in ecosystem services from urban and peri-urban forests and their implication to sustainable city design and planning. Sustain. Cities Soc. 82, 103903. doi:10.1016/j.scs.2022.103903
- Jia Y. C., Jie F. X., Kang G., Yiwu W. (2024). Balancing urban expansion with ecological integrity: an ESP framework for rapidly urbanizing small and medium-sized cities, with insights from suizhou, China. Ecol. Inf. 80, 102508. doi:10.1016/j.ecoinf.2024.102508
- Li L., Ji G., Li Q., Zhang J., Gao H., Jia M. (2023). Spatiotemporal evolution and prediction of ecosystem carbon storage in the yiluo river basin based on the PLUS-InVEST model. Forests 14 (12), 2442. doi:10.3390/f14122442
- Li Y. W., Lin T., Zhou W. Q., Yang L. (2024). Analysis of ecosystem service value with multi-scenario simulation in DongTing Lake basin. Chin. J. Agric. Resour. Regional Plan. 45 (10), 109 – 121. doi:10.7621/cjarrp.1005-9121.20241011
- Meury S. W., François J. B., Patrick L., Chassiot L. (2025). From industry to recreation: the role of land use changes in shaping an estuarine urban beach system. J. Coast. Res. 41 (5), 856 – 872. doi:10.2112/JCOASTRES-D-24-00060.1
- Miao C. Y., Gou J. J., Fu B. J., Tang Q., Duan Q., Chen Z. (2022). High-quality reconstruction of China’s natural streamflow. Sci. Bull. 67 (5), 547 – 556. doi:10.1016/j.scib.2021.09.022
- Ocloo M. D., Mizunoya T. (2025). Carbon storage and land use dynamics in Ghanaian university campuses: a scenario-based assessment using the InVEST model. Land 14 (10), 1987. doi:10.3390/land14101987
- Qiu Z., Gong D., Zhao M., Dong D. (2025). Spatiotemporal dynamics and driving mechanisms of soil conservation services (SCS) in Zhejiang Province, China: insights from InVEST modeling and machine learning. Remote Sens. 17 (16), 2865. 2865-2865. doi:10.3390/rs17162865
- Sharma M., Ashraf J., Mehta D., Pandey R. (2024). Assessment of nature-based interventions adherence with IUCN global standards and an analysis of flow of associated ecosystem services in tropical drylands of India. Ecol. Indic. 159, 111717. doi:10.1016/j.ecolind.2024.111717
- Shi L. Y., Yang B., Juha M. A., Hui M. W., Bo J., Gang L. (2021). Spatiotemporal changes in water-related ecosystem services provision and trade-offs with food production. J. Clean. Prod. 286: 125316. doi:10.1016/j.jclepro.2020.125316
- Sullivan K. M., Vleminckx J., Bissiemou M. A. P., Niangadouma R., Mayoungou M. I., Temba J. L. (2024). Low-intensity logging alters species and functional composition, but does not negatively impact key ecosystem services in a Central African tropical forest. Glob. Ecol. Conservation 53, e02996. doi:10.1016/j.gecco.2024.e02996
- Tang L., Zhao H., Zhou Z., Qian Z., Hou S., Liu B. (2025). Spatiotemporal distribution and driving factors of water use efficiency in the yangtze river Delta urban agglomeration under the background of sustainability. Ecol. Indic. 179, 114159. doi:10.1016/j.ecolind.2025.114159
- Verma P., Jangra R., Kaushik S. (2024). Geospatial measurement of urban sprawl and land transformation using multi-temporal datasets: a case study of sonipat-kundli urban agglomeration. Sustain. Environ. 10 (1), 2366556. doi:10.1080/27658511.2024.2366556
- Wang H., Sun Q. (2024). Urban sprawl and imbalance between supply and demand of ecosystem services: evidence from china’s yangtze river Delta urban agglomerations. Sustainability 16 (18), 8269. doi:10.3390/su16188269
- Wang C. D., Li W. Q., Sun M. X., Wang Y., Wang S. (2021). Exploring the formulation of ecological management policies by quantifying interregional primary ecosystem service flows in yangtze river Delta region, China. J. Environ. Manag. 284, 112042. doi:10.1016/j.jenvman.2021.112042
- Wischmeier W. H. (1959). A rainfall erosion index for a universal soil-loss equation. Soil Sci. Soc. Am. J. 23 (3), 246 – 249. doi:10.2136/sssaj1959.03615995002300030027x
- Xu L., He N. P., Yu G. R. (2019). A dataset of carbon density of China’s terrestrial ecosystems 2010s. China Scientific Data, 4 (1), 21.86101/csdata.2018.0026.zh. doi:10.11922/csdata.2018.0026.zh
- Yang D., Liu W., Tang L., Chen L., Li X., Xu X. (2019). Estimation of water provision service for monsoon catchments of south China: applicability of the InVEST model. Landsc. Urban Plan. 182, 133 – 143. doi:10.1016/j.landurbplan.2018.10.011
- Yang S., Su H., Zhao G. P. (2022). Multi-scenario simulation of urban ecosystem service value based on PLUS model: a case study of hanzhong city. J. Arid Land Resour. Environ. 36 (10), 86 – 95. doi:10.13448/j.cnki.jalre.2022.255
- Yi Y., Yuan Y. Z., Hui Y., Feng Y. Y. (2022). Horizontal ecological compensation as a tool for sustainable development of urban agglomerations: exploration of the realization mechanism of guanzhong plain urban agglomeration in China. Environ. Sci. Policy 137, 301 – 313. doi:10.1016/j.envsci.2022.09.004
- Yu J., Guo S., Wang S., Luo Y. (2025). Multi-scenario simulation of land use change and ecosystem health assessment in chengdu metropolitan area based on SD-PLUS-VORS coupled modeling. Sustainability 17 (7), 3202. doi:10.3390/su17073202
- Zhang W., Wang F. C., Wan H. L., Zhang L. J., Li Z. M., Wang H. X. (2022). Spatiotemporal variations and influencing factors of soil conservation service based on InVEST model: a case study of miyun reservoir upstream basin of zhangcheng area in Hebei. Prog. Geophys. 37 (6), 2339 – 2350. doi:10.6038/pg2022GG0067
- Zhong J. T., Wang B., Mi W. B., Fan X. G., Yang M. L., Yang X. M. (2020). Spatial recognition of ecological compensation standard for grazing grassland in yanchi county based on InVEST model. Sci. Geogr. Sincia 40 (06), 1019 – 1028. doi:10.13249/j.cnki.sgs.2020.06.018
- Zhou X., Ji G., Wang F., Ji X. (2025). Identification and simulation of ecological zoning in the yangtze river delta (YRD) urban agglomeration based on ecological service value (ESV)–landscape ecological risk (LER). J. Clean. Prod. 516, 145778. doi:10.1016/j.jclepro.2025.145778
- Zhu Y., Ma B., Hu H., Ding D., Zhou H., Liu J. (2025). Analysis and prediction of spatiotemporal carbon storage changes in the taihu Lake basin in Jiangsu Province based on PLUS and InVEST model. Trees, For. People 21, 100916. doi:10.1016/j.tfp.2025.100916
Citation
Chen, A., et al. (2026). Land use change, driving factors, and multi-scenario projections of ecosystem service supply in the Yangtze River delta urban agglomeration. Frontiers in Environmental Science, Volume 14. https://doi.org/
- Received
- Accepted
- Published
- Volume
- 14 - 2026
Copyright
Copyright © 2026 Chen, Sun, Zhu, Shao and He.
License: https://creativecommons.org/licenses/by/4.0/
*Correspondence: Qiao Sun
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