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Effects of forest vegetation on soil moisture and runoff of watershed in east China

机译:森林植被对华东地区水域土壤水分和径流的影响

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hydrological effects of natural secondary forest ecosystem were studied from March to October in 2009. The results showed that soil moisture ranged from 14.24% to 22.55% in observation period. The monthly variation trend in soil moisture of top layers (5cm and 10cm) was similar to that of rainfall. Deep layers (20cm and 50cm) moisture became gradually stable as the depth increasing. The soil moisture of 10cm layer was obviously higher than that in other three layers. Runoff analysis showed that the annual runoff ratio in this research watershed is 68.5%, but the ratio for quick runoff, composed of direct runoff and surface runoff, is only 0.10%. The total watershed runoff during this period was 836.5 mm. It was shown that the amount of surface runoff increased with the increasing of precipitation, but having various tendencies for different precipitation intensity classes.
机译:从2009年3月到10月研究了自然中林生态系统的水文效应。结果表明,观察期内土壤水分含量为14.24%至22.55%。顶层土壤湿度(5cm和10cm)的月度变异趋势与降雨相似。深层(20cm和50cm)水分随着深度增加而逐渐稳定。 10cm层的土壤水分明显高于其他三层。径流分析表明,本研究流域的年径流比率为68.5%,但快速径流的比率,由直接径流和表面径流组成,仅为0.10%。在此期间的流域径流总数为836.5毫米。结果表明,表面径流量随着沉淀的增加而增加,但具有不同沉淀强度等级的各种趋势。

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