首页> 外文期刊>Chinese Geographical Science >VARIATION IN FLOW AND SEDIMENT OF DASHA RIVER AND INFLUENCE OF HUMAN ACTIVITIES ON IT IN SOUTHWEST REGION OF ANHUI PROVINCE
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VARIATION IN FLOW AND SEDIMENT OF DASHA RIVER AND INFLUENCE OF HUMAN ACTIVITIES ON IT IN SOUTHWEST REGION OF ANHUI PROVINCE

机译:安徽省西南地区大沙河水流变化及泥沙变化及其对人类活动的影响

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摘要

Soil and water loss is now a major environmental problem in many areas of China, especially in the area of the Dabie Mountain, Anhui Province, which results in environmental degradation and does harm to the people's life and production there. Based on the observational records from the Dasha River, the authors analyze the character of the variation in flow and sediment in different flood and dry seasons from 1970 to 2000. The result shows that human activities had significantly reduced the sediment discharge and sediment module, and increased the runoff in low-water seasons since the 1980s. The average contribution rate of human activities to decreasing sediment was 65.67%, and at the same period the contribution rate of runoff and rainfall was about 34.33%. Therefore, it is necessary to take the biological and engineering measures to solve the problem of soil and water loss in the Dasha River watershed.
机译:目前,水土流失是中国许多地区的主要环境问题,特别是在安徽省大别山地区,这导致环境恶化,并危害当地人民的生活和生产。根据大沙河的观测记录,作者分析了1970年至2000年不同汛期和干旱季节的流量和泥沙变化特征。结果表明,人类活动显着减少了泥沙的排放和泥沙组成,并且自1980年代以来,增加了枯水季节的径流。人类活动对减少沉积物的平均贡献率为65.67%,而同期径流和降雨的贡献率约为34.33%。因此,有必要采取生物和工程措施来解决大沙河流域的水土流失问题。

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