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Rainfall simulation for the study of the effects of efficient factors on run-off rate

机译:降雨模拟研究有效因素对径流率的影响

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Depending upon the watershed characteristics and weather conditions, a substantial part of the precipitation may be changed into run-off. Knowledge about the discharge and volume of the run-off generated by rainfall, especially in ungauged catchments, plays an important role in water resources management planning. In the absence of sufficient data recorded from the real rainfall events, use of rainfall simulators in the field and laboratory may be recommended to simulate runoff in different conditions of soil, vegetation cover, slope and rainfall. In this study, a rainfall simulator ( a portable non-pressurized type) was used to examine the effects of slope steepness, vegetation cover, clay, sand, silt and antecedent soil moisture content on run-off amount. Two sets of simulated rainfall events with 24.5 and 32 mm/h intensity were applied on 145 experimental plots with dimensions 1.2 m x 0.89 m in Taleghan watershed, Iran, and the relevant run-off amounts were measured in each experimental plot.Based on the results obtained from the correlation matrix, the most influential factors on run-off were vegetation cover, antecedent soil moisture content, clay, sand, silt and slope, for rainfall intensity of 24.5 mm/h. While for the rainfall intensityof 32 mm/h, vegetation cover, sand, antecedent soil moisture content, silt, clay and slope were the most influential factors. Two regression equations were also developed for predicting surface run-off with different field and rainfall conditions.
机译:取决于流域的特征和天气条件,大部分降水可能会变成径流。关于降雨(特别是在未开垦集水区)降雨产生的径流量和流量的知识,在水资源管理规划中起着重要作用。在没有实际降雨事件记录的足够数据的情况下,建议在野外和实验室使用降雨模拟器,以模拟土壤,植被,坡度和降雨等不同条件下的径流。在这项研究中,使用了一个降雨模拟器(便携式非加压型)来检查坡度,植被覆盖度,粘土,沙子,淤泥和前期土壤水分含量对径流量的影响。在伊朗塔莱汉河小流域的145个尺寸为1.2 mx 0.89 m的实验地块上应用了两组强度分别为24.5和32 mm / h的模拟降雨事件,并在每个实验区中测量了相关的径流量。从相关矩阵中获得的数据,降雨强度为24.5 mm / h时,径流最主要的影响因素是植被覆盖度,前期土壤含水量,粘土,沙土,淤泥和坡度。对于32 mm / h的降雨强度,影响最大的因素是植被覆盖率,沙土,前期土壤含水量,淤泥,黏土和坡度。还开发了两个回归方程来预测不同田间和降雨条件下的地表径流。

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