Li Yi, Shao Ming-An
College of Water Resources and Architecture Engineering, Northwest Sci-Tech University for Agriculture and Forestry, Yangling 712100, Shaanxi, China.
Ying Yong Sheng Tai Xue Bao. 2008 Jul;19(7):1511-6.
Based on the experiments of controlled intermittent and repetitive rainfall on slope land, the infiltration and distribution characteristics of soil water on loess slope land were studied. The results showed that under the condition of intermittent rainfall, the cumulative runoff during two rainfall events increased linearly with time, and the wetting front also increased with time. In the interval of the two rainfall events, the wetting front increased slowly, and the infiltration rate was smaller on steeper slope than on flat surface. During the second rainfall event, there was an obvious decreasing trend of infiltration rate with time. The cumulative infiltration on 15 degrees slope land was larger than that of 25 degrees slope land, being 178 mm and 88 mm, respectively. Under the condition of repetitive rainfall, the initial infiltration rate during each rainfall event was relatively large, and during the first rainfall, both the infiltration rate and the cumulative infiltration at various stages were larger than those during the other three rainfall events. However, after the first rainfall, there were no obvious differences in the infiltration rate among the next three rainfall events. The more the rainfall event, the deeper the wetting front advanced.
基于坡面土地控制间歇和重复降雨试验,研究了黄土坡面土地土壤水分的入渗和分布特征。结果表明,在间歇降雨条件下,两次降雨事件期间的累积径流量随时间呈线性增加,湿润锋也随时间增加。在两次降雨事件的间隔期间,湿润锋增加缓慢,且陡坡上的入渗率比平面上的小。在第二次降雨事件期间,入渗率随时间有明显下降趋势。15度坡地的累积入渗量大于25度坡地,分别为178毫米和88毫米。在重复降雨条件下,每次降雨事件的初始入渗率相对较大,且在第一次降雨期间,各阶段的入渗率和累积入渗量均大于其他三次降雨事件。然而,第一次降雨后,后三次降雨事件的入渗率没有明显差异。降雨事件越多,湿润锋推进越深。