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生态学杂志 ›› 2024, Vol. 43 ›› Issue (3): 861-868.doi: 10.13292/j.1000-4890.202403.006

• 研究报告 • 上一篇    下一篇

赣江上游章水流域水沙变化及其归因分析

张婷,刘士余*,盛菲,李俊,余敏琪   

  1. (江西农业大学国土资源与环境学院, 江西省鄱阳湖流域农业资源与生态重点实验室, 南昌 330045)
  • 出版日期:2024-03-10 发布日期:2024-03-15

Variations of runoff and sediment and its attribution analysis in Zhangshui watershed of the upper reaches of Ganjiang River.

ZHANG Ting, LIU Shiyu*, SHENG Fei, LI Jun, YU Minqi   

  1. (College of Land Resources and Environment of Jiangxi Agricultural University, Key Laboratory of Poyang Lake Watershed Agricultural Resources and Ecology of Jiangxi Province, Nanchang 330045, China).

  • Online:2024-03-10 Published:2024-03-15

摘要: 随着气候变化和人类活动的加剧,流域水沙情势发生变化,定量分析降水变化和人类活动的水沙效应是当前水科学研究的热点。本文基于赣江上游章水流域1961—2020年的水文、气象观测资料,采用累积量斜率变化率比较法、经验统计分析法定量分析了降水变化和人类活动对水沙变化的贡献率及人类活动的水沙效应对年降水量响应的临界值。结果表明:降水量和径流量均呈非显著下降趋势(P>0.05),输沙量呈极显著下降趋势(P<0.001);降水量和径流量的突变年份均为2003年,输沙量的突变年份为1998年;降水变化和人类活动对径流减少的贡献率分别为10.7%和89.3%,对输沙减少的贡献率分别为3.5%和96.5%;人类活动的减水、减沙效应对年降水量响应的临界值分别为1170 mm和858 mm。研究成果可为流域生态建设、水土资源优化管理提供科学依据。


关键词: 章水流域, 降水变化, 人类活动, 水沙变化, 临界值

Abstract: The runoff and sediment situation in the watershed has changed with climate change and the intensification of human activities. Quantitative analysis of the runoff and sediment effects of precipitation variation and human activities is a hot topic in current water science research. Based on the hydrological and meteorological observation data of Zhangshui watershed in the upper reaches of Ganjiang River from 1961 to 2020, we quantitatively analyzed the contribution rate of precipitation variation and human activities to the changes of runoff and sediment, and the critical value of the runoff and sediment effect of human activities to the annual precipitation response by using the slope change ratio of accumulative quantity and empirical statistical analysis. The results showed that precipitation and runoff showed a nonsignificant downward trend (P>0.05), and the sediment transport showed a significant downward trend (P<0.001). The abrupt change of precipitation and runoff was in 2003, and the abrupt change of sediment was in 1998. The contribution rates of precipitation variation and human activities to runoff reduction were 10.7% and 89.3%, and to sediment reduction were 3.5% and 96.5%, respectively. The critical values of runoff and sediment reduction effects of human activities in response to annual precipitation were 1170 mm and 858 mm, respectively. Our results could provide scientific basis for watershed ecological construction and optimal management of water and land resources.


Key words: Zhangshui watershed, precipitation variation, human activity, runoff and sediment change, critical value