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    三峡库区三种泥沙连通性指数的时间尺度效应

    The time-scale effects of three types of sediment connectivity indices in the Three Gorges Reservoir Area

    • 摘要: 【目的】泥沙连通性是解析区域输沙路径与物源贡献的核心指标。目前研究多集中于单一连通性单尺度时空分布,多种连通性指数对流域不同时间尺度输沙状况的时空特征及适用情景仍待深入。【方法】以三峡库区香溪河流域为研究对象,基于结构、功能和复合连通性指数,探究不同尺度下多种泥沙连通性时空变化特征,对比分析不同指数适用情景。【结果】1)三类指数的年际变幅为1.34%~52.03%,而月际尺度波动幅度明显高于年际尺度,其中复合连通性(ICR)月际变幅达到407.87%。功能连通性(IC_R)受降雨主导,表现为夏秋高、冬春低。结构连通性(IC)受植被拦截效应驱动,变化趋势与植被覆盖相反。2)IC_R对降雨事件的响应具有非线性特征,呈边际效应递减趋势(R2=0.98)。3)在年际尺度下,三种连通性高值区域集中于沟道、汇水区及人类活动区。月际尺度上,IC、ICR在冬春季(11月至次年3月)时反常,距水系较远区域较高。4)年际尺度下,三类连通性指数均与泥沙量正相关,月际IC_R、ICR显著正相关,IC、IC_R在部分月份有重要解释作用。【结论】多种泥沙连通性均具有时间尺度效应,复合连通性是表征亚热带季风气候多尺度流域输沙的最优指标。水土流失治理应重点关注流域中下游两岸及人类活动区关键拦截带及降雨植被驱动下的季节性连通性高峰。

       

      Abstract: Objective Sediment connectivity is a core indicator for analyzing regional sediment transport pathways and source contributions. Current research mainly focuses on the spatiotemporal distribution of single connectivity at a single type of connectivity index, while the spatiotemporal characteristics and applicable scenarios of multiple connectivity indices for sediment transport conditions at different time scales in a watershed remain to be further explored. Method Taking the Xiangxi River Basin in the Three Gorges Reservoir Area as the research object, based on structural, functional, and composite connectivity indices, this study explores the spatiotemporal variation characteristics of multiple sediment connectivity at different scales and compares the applicable scenarios of different indices. Result 1) The interannual variation range of the three types of indices is 1.34% to 52.03%, while the monthly variation amplitude is significantly higher than the interannual variation, with the monthly variation range of the composite connectivity (ICR) reaching up to 407.87%. Functional connectivity (IC_R) is dominated by rainfall, showing high values in summer and autumn and low values in winter and spring. Structural connectivity (IC) is driven by the interception effect of vegetation, and its trend is opposite to that of vegetation coverage. 2) The response of IC_R to rainfall events has a nonlinear characteristic, showing a decreasing marginal effect trend (R2 = 0.93). 3) At the interannual scale, the three high-value connectivity areas are concentrated in the channels, catchment areas and human activity areas. At the monthly scale, IC and ICR are abnormal in winter and spring (from November to March of the following year), with higher values in areas farther from water systems. 4) At the interannual scale, all three types of connectivity indices are positively correlated with sediment yield. At the monthly scale, IC_R and ICR are significantly positively correlated, and IC and IC_R have important characterization effects in some months. Conclusion Multiple sediment connectivity indices all have time scale effects, and composite connectivity is the optimal index for characterizing sediment transport in multi-scale watersheds under a subtropical monsoon climate. Soil and water conservation should focus on key interception zones on both banks of the middle and lower reaches of the watershed and seasonal connectivity peaks driven by rainfall and vegetation.

       

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