北京贵水河流域对人类活动的水文响应

Yuming Liu, Jing Zhang, Pengfei Wu, H. Gong
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引用次数: 0

摘要

本研究以1986-1987年和2005-2006年为研究期,以1987年和2005年两幅TM影像为基础,对两幅土地利用图进行人工分类。然后对土地利用变化和天气变化进行分析。在研究区建立了SWAT模型,模拟了人类活动对水文的响应。结果表明:人类活动对径流有显著影响。在研究期间,直接效应对径流的影响远大于间接效应。在间接影响下,月径流量增加0.47m3/s,汛期(6、7、8月)径流量增加2.36m3/s,变化率为34.7%。在直接作用下,月径流量减少3.01m3/s,汛期径流量减少8.71m3/s,变化率为95.1%。分析结果表明,人类活动可以改善水运行因子,减少洪涝灾害。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The hydrological response to human activities in Guishui River Basin, Beijing, China
In this research, the year of 1986-1987 and 2005-2006 were chosen as two study periods, two land use maps on the base of two TM images of 1987 and 2005 were classified manually. Then the land use changes and weather changes were analyzed. Moreover, a SWAT model was setup and carried out in the study area to simulate the hydrological response to human activities. The results showed that: Human activities had remarkable effects on runoff. In the study periods, the direct effects affected the runoff much more than the indirect effects did. Under the indirect effects, the runoff increased by 0.47m3/s monthly, and the runoff increased by 2.36m3/s in flood season (June, July and August) when the variation percentage is 34.7%. Under the direct effects, the runoff decreases by 3.01m3/s monthly, and the runoff decreases by 8.71m3/s in flood season when the variation percentage is 95.1%. The analysis results prove that human activities can improve the water operating factor and make fewer flood disasters.
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