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    中国西南地区未来不同情景下土地利用变化模拟

    Future land use change simulation in Southwest China under different scenarios

    • 摘要: 本研究针对水土流失敏感的中国西南地区,基于MCD12Q1和LUH2数据,使用斑块生成土地利用模拟模型(PLUS)模拟了SSP1-RCP1.9(可持续发展)、SSP2-RCP4.5(中等发展)和SSP5-RCP8.5(高速发展)三种情景下2020–2100年土地利用分布。通过土地利用动态度、转移矩阵及空间扩张分析,揭示该区域21世纪的土地利用时空变化特征。结果表明:1)2001-2020年,土地利用综合动态度为0.47%,变化强度较高,林地增加42191 km2,草地减少52614 km2,建设用地超越未利用地成为第四大类,扩张集中于成渝经济区等城市群;2)模型精度较高,Kappa = 0.85,OA = 0.91,FoM = 0.18。2020-2100年各情景下,草地是主要转出地类;建设用地呈现倒U型变化,在50年代达到峰值后转出;3)SSP119情景下土地利用变化强度最高,综合动态度峰值达1.71%,林地和耕地面积增加57.33%和66.96%,林地覆盖除四川盆地外大部分区域,耕地在川西北-东和滇东等地扩张,草地面积净减少96.23%;SSP245情景下土地利用变化强度较低,综合动态度为0.08至0.34%,林地和耕地面积增加10.18%和18.40%,草地面积减少19.21%;SSP585情景下2040年前变化强度高,之后趋缓,至2100年各地类面积与SSP245情景趋同,城市群建设用地呈现高强度圈层式扩张。研究结果填补了西南易受侵蚀地区未来多情景土地利用模拟研究的空白,可为国土空间规划(如生态保护红线划定)和土地管理策略制定(如水土流失防控)提供坚实的科学支持。

       

      Abstract: Background Southwest China (Yunnan, Guizhou, Sichuan, and Chongqing), highly prone to erosion, faces significant ecological and soil-water conservation challenges due to rapid socioeconomic development and land use change. However, research on future land use changes under diverse socioeconomic scenarios in this critical region remains limited. This study simulated future land use changes to inform land resource management and ecosystem protection strategies, particularly for soil and water loss prevention. Methods Based on MCD12Q1 historical land use data (2001-2020) and LUH2 future data, the Patch-generating Land Use Simulation (PLUS) model was used to simulate land use distribution from 2020 to 2100 under three Shared Socioeconomic Pathway-Representative Concentration Pathway (SSP-RCP) scenarios: SSP1-RCP1.9 (Sustainable Development), SSP2-RCP4.5 (Medium Development), and SSP5-RCP8.5 (High-speed Development). Spatiotemporal characteristics of change were analyzed using land use dynamics, transition matrices, and spatial expansion analysis. Results 1) Historically (2001–2020), forest area increased significantly by 42,191 km² (reaching 47.73% coverage), primarily converted from grassland (-52,614 km²). Urban expanded by 42.35%, concentrated in agglomerations like the Chengdu-Chongqing. 2) The PLUS model demonstrated high accuracy (Kappa = 0.85, OA = 0.91, FoM = 0.18). Future simulations (2020-2100) revealed strong scenario dependence: SSP119 exhibited peak land use intensit (comprehensive dynamic degree: 1.71%), with dramatic forest (+57.33%) and cropland (+66.96%) increases but severe grassland decline (-96.23%). Forest covered most regions except the Sichuan Basin, and cropland expanded in northwestern/eastern Sichuan, eastern Yunnan, and central/western Guizhou. SSP245 showed moderate changes (forest: +10.18%, cropland: +18.40%, grassland: −19.21%). SSP585 exhibited high early-period intensity (pre-2040), featuring concentric urban expansion within clusters, converging towards SSP245 patterns by 2100. Grassland consistently remained the primary conversion source across all scenarios. Built-up land followed an inverted U-shaped trajectory, peaking in the 2050s. Conclusion The PLUS model reliably simulates long-term land use changes in Southwest China’s complex terrain. Multi-scenario outcomes reveal divergent policy-relevant pathways: SSP119 drives extensive ecological conversion (forest/cropland increase, grassland loss), while SSP245/SSP585 show moderated changes with mid-century urban peaks. These projections provide a robust scientific basis for optimizing territorial spatial planning and sustainable land management to support soil and water loss prevention and broader ecological protection goals.

       

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