1985-2020年三峡库区沉积物连通性时空演变及其驱动因素
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作者单位:

1.中国科学院重庆绿色智能技术研究院;2.重庆师范大学数学科学学院

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基金项目:

国家自然科学基金(No.42371071);重庆市水利局三峡后续科研项目(No.5000002021BF40001);重庆市科技创新与应用发展重点专项(No. CSTB2023TIAD-KPX0077)


Spatial and temporal evolution and driving forces of sediment connectivity (IC) in the Three Gorges reservoir area
Author:
Affiliation:

1.Chongqing Institute of Green and Intelligent Technology , Chinese Academy of Sciences;2.School of Mathematics Sciences, Chongqing Normal University

Fund Project:

the National Natural Science Foundation of China (Grant No. 42371071); Chongqing Water Resources Bureau Three Gorges Follow-up Research Project, No.5000002021BF40001; Chongqing Science and Technology Innovation and Application Development Key Project (No. CSTB2023TIAD-KPX0077)

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    摘要:

    【目的】由于三峡建坝,库区内沉积物连通性增加,是引发区域内水土流失的重要诱因之一。因此,探究其沉积物连通性时空变化规律及其驱动因素,可为维持三峡库区生态环境稳定和推动社会可持续发展提供重要依据。【方法】本文以三峡库区为研究区,采用冷热点分析阐明了1985 ~ 2020年三峡库区内沉积物连通性的时空演变特征,并采用最优参数地理探测器(OPGD)揭示了其变化的影响因素。【结果】结果表明:(1)1985 ~ 2020年,三峡库区沉积物连通性整体呈下降趋势,截止2020年降低了4.40%;呈现出明显的东部降低,西部升高的空间分异格局;(2)1985 ~ 2000年,库区沉积物连通性变化冷热点区域范围逐渐减小;2000年之后,热点区域主要集中在重庆市主城区,冷点区域主要集中在渝东北的开州区、云阳县;(3)三峡库区沉积物连通性空间分布受多种因素耦合影响,总体上,土壤可蚀性与植被覆盖是影响库区沉积物潜在连通性时空变化的关键因子。【结论】这表明,三峡库区的沉积物连通性在过去35年间整体上呈下降趋势,有效的植被恢复和气候变化应对策略有助于减少水土流失,从而维持区域生态系统的健康和可持续发展。

    Abstract:

    [Objective] Due to the construction of the Three Gorges Dam, the connectivity of sediments within the reservoir area has significantly changed and increased, becoming one of the important factors inducing soil erosion in the region. Therefore, exploring the spatial and temporal patterns of sediment connectivity and its driving factors can provide an important basis for maintaining the stability of the ecological environment in the Three Gorges Reservoir Area and promoting the sustainable development of the society. [Methods] Taking the Three Gorges Reservoir Area as the study area, this paper elucidates the spatial and temporal evolution characteristics of sediment connectivity within the Three Gorges Reservoir Area from 1985 ~ 2020 using cold hotspot analysis, and reveals the influencing factors of its changes using the Optimal Parameter-based Geographical Detectors (OPGD). [Results] The results show that: (1) From 1985 ~ 2020, the sediment connectivity in the Three Gorges Reservoir area shows an overall decreasing trend, with a decrease of 4.40% as of 2020; it presents an obvious spatial differentiation pattern of decreasing in the east and increasing in the west; (2) From 1985 ~ 2000, the range of cold hotspot areas of the sediment connectivity change in the reservoir area decreases gradually; after 2000, the hotspot areas are mainly concentrated in the main urban area of Chongqing Municipality, and the cold spot area was mainly concentrated in Kaizhou District and Yunyang County in northeastern Chongqing; (3) The spatial distribution of sediment connectivity in the Three Gorges Reservoir area is influenced by the coupling of multiple factors. Overall, soil erodibility and vegetation cover are the key factors affecting the spatiotemporal variation of sediment connectivity in the reservoir area. [Conclusions] This suggests that sediment connectivity in the Three Gorges reservoir area has shown an overall decreasing trend over the past 35 years, and that effective vegetation restoration and climate change coping strategies can help to reduce soil erosion and thus maintain the health and sustainable development of the regional ecosystem.

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  • 收稿日期:2024-10-09
  • 最后修改日期:2025-02-20
  • 录用日期:2025-05-08
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