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中国长江嘉陵江流域水文情势变化及其影响因素。

Hydrologic regime alteration and influence factors in the Jialing River of the Yangtze River, China.

机构信息

College of Water Resources, North China University of Water Resources and Electric Power, Zhengzhou, 450045, China.

School of Water Conservancy, North China University of Water Resources and Electric Power, Zhengzhou, 450045, China.

出版信息

Sci Rep. 2022 Jul 1;12(1):11166. doi: 10.1038/s41598-022-15127-4.

Abstract

Under the influence of climate alteration and human activities, the hydrological regime of rivers is changing dramatically, which has become a hot spot for water environment research. In this study, we quantitatively assessed the degree of hydrological variability of the Jialing River and the contribution of climate alteration and human activities to hydrological alterations using the ecohydrological indicator range of alteration (IHA-RVA) method and Budyko hypothesis formulations. The results showed that (1) The average annual runoff and the precipitation of Jialing River showed a decreasing trend, the potential evapotranspiration showed an increasing trend. (2) Compared with before the hydrological situation changed, the degree of alteration in the annual extreme streamflow is 31%, which is a low degree of alteration; the degree of alteration in monthly streamflow, annual extreme flow magnitude, extreme flow ephemeris, and streamflow alteration frequency are 51%, 43%, 54%, and 64% respectively, which are all moderate degrees of alteration; the overall hydrological alteration is 50%, which belongs to moderate alteration. (3) The contribution of precipitation, potential evapotranspiration, and human activities to the runoff alteration is 61%, - 16%, and 55%, respectively. This study provides corresponding references for ecological restoration and sustainable development of the Yangtze River Basin in China.

摘要

在气候变化和人类活动的影响下,河流的水文状况发生了巨大变化,这已成为水环境研究的热点。本研究采用生态水文学变化幅度范围(IHA-RVA)方法和布地克假说公式,定量评估了嘉陵江的水文变异性程度以及气候变化和人类活动对水文变化的贡献。结果表明:(1)嘉陵江的年平均径流量和降水量呈减少趋势,潜在蒸散量呈增加趋势。(2)与水文状况改变之前相比,年极端径流量的变化程度为 31%,属于低度变化;月径流量、年极端流量大小、极端流量历时和径流量变化频率的变化程度分别为 51%、43%、54%和 64%,均属于中度变化;整体水文变化程度为 50%,属于中度变化。(3)降水、潜在蒸散量和人类活动对径流量变化的贡献分别为 61%、-16%和 55%。本研究为中国长江流域的生态恢复和可持续发展提供了相应的参考。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ad70/9249885/c2de30fc49ce/41598_2022_15127_Fig1_HTML.jpg

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