1980s以来长江中下游河-湖-库-塘复合水域景观格局演变及驱动机制
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宁波大学地理科学与遥感技术学院

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国家社会科学基金重大项目(23&ZD105)


Landscape Pattern Evolution and Driving Mechanisms of the River–Lake–Reservoir–Pond Composite Water System in the Middle and Lower Reaches of the Yangtze River since 1980s
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School of Geography and Remote Rensing, Ningbo University

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    摘要:

    长江中下游河-湖-库-塘复合水域系统作为流域水文连通性与生态过程交互的核心载体,其多要素协同演化规律与驱动机制尚待深入揭示。现有研究多聚焦单一水域类型,难以系统解析复合系统内部组分的动态关联及多因子耦合效应。基于多源遥感影像生成的专题数据产品,本文综合运用景观格局分析方法与地理探测器模型,系统阐明了长江中下游复合水域景观格局时空分异特征,并定量识别了自然与人为驱动因子的交互作用机制。结果表明:(1)研究期内复合水域景观总面积呈增加趋势,但内部结构分异显著;河渠、水库坑塘及滩地面积扩张,而湖泊、滩涂与沼泽湿地持续萎缩,凸显了人类活动对水域结构的深度改造。(2)复合水域景观组分间动态转换特征明显,前者表现为净转入,后者呈净转出,揭示了水域景观要素间的复杂权衡关系。(3)整体景观格局趋于破碎化与复杂化,表现为斑块数量(NP)、斑块密度(PD)、边界密度(ED)、景观形状指数(LSI)、香农多样性指数(SHDI)及均匀度指数(SHEI)持续上升,聚集度指数(AI)则呈下降趋势;不同类型水域景观指数响应存在显著差异,反映了其演化路径的分异。(4)复合水域景观演变受自然基础与人为扰动的交互驱动,其中气温与降水奠定了其区域格局,而人口密度变化率对湖泊萎缩、沼泽退化等过程影响尤为显著。本研究揭示了长江中下游复合水域系统的结构演化规律及驱动机制,可为流域水资源统筹管理、生态修复与国土空间规划提供科学依据。

    Abstract:

    The river-lake-reservoir-pond composite water system in the middle and lower reaches of the Yangtze River represents a critical medium through which watershed hydrological connectivity interacts with ecological processes. However, the coordinated evolutionary dynamics of its multiple components and their underlying driving mechanisms remain inadequately understood. Most existing studies have focused on individual water-body types, which limits a systematic understanding of the dynamic interactions among components within the composite system and the coupled effects of multiple driving factors. Using thematic datasets derived from multi-source remote sensing imagery, this study integrates landscape pattern analysis with the Geographical Detector model to systematically characterize the spatiotemporal differentiation of composite water landscapes in the middle and lower reaches of the Yangtze River. In addition, the interactive effects of natural and anthropogenic driving factors are quantitatively identified. The results show that: (1) During the study period, the total area of composite water landscapes exhibited an overall increasing trend, while their internal structure underwent pronounced differentiation. Areas of rivers and channels, reservoirs and ponds, and shoal lands expanded, whereas lakes, tidal flats, and marsh wetlands continued to decline, highlighting the substantial restructuring of water systems driven by human activities. (2) Significant dynamic transitions occurred among landscape components within the composite water system. Some components experienced net gains, whereas others showed net losses, revealing complex trade-off relationships among water-landscape elements. (3) The overall landscape pattern became increasingly fragmented and complex. Indicators including the number of patches (NP), patch density (PD), edge density (ED), landscape shape index (LSI), Shannon’s diversity index (SHDI), and Shannon’s evenness index (SHEI) increased continuously, whereas the aggregation index (AI) declined. The responses of landscape metrics varied significantly among different water-body types, reflecting divergent evolutionary pathways. (4) The evolution of the composite water landscape was jointly driven by natural conditions and anthropogenic disturbances. Temperature and precipitation established the fundamental regional pattern, while changes in population density exerted particularly strong influences on processes such as lake shrinkage and marsh degradation. Overall, this study elucidates the structural evolution and driving mechanisms of the composite water system in the middle and lower reaches of the Yangtze River, providing a scientific basis for integrated watershed water-resource management, ecological restoration, and territorial spatial planning.

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  • 收稿日期:2025-11-29
  • 最后修改日期:2026-03-13
  • 录用日期:2026-05-08
  • 在线发布日期: 2026-07-29
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