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Research experiment on infiltration and runoff in Jujube land of northern Shaanxi Province

机译:陕北枣地入渗径流研究实验

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To provide guidance for the efficient use of rainwater in Jujube forests of the northern Shaanxi Province, research on the processes of infiltration and runoff under field simulated rainfall were conducted. The process of infiltration and runoff-yield on sloping land was simulated with Richards equation and the water balance equation under different rainfall intensities and soil water content, in the north of Shaanxi province. It reached results via comparing with observation results: the mean relative error of the period cumulative infiltration was less than 3%, with a root mean squared error (RSME) less than 0.3. The mean relative error of the period cumulative runoff was less than 12.5%, RSME < 0.4. The simulation results were reasonable; however, the simulation ponding time generally lagged behind measured ponding time probably because of spatial variation of saturated hydraulic conductivity and uneven rainfall.
机译:为了对陕北枣林中雨水的有效利用提供指导,对田间模拟降雨下的入渗和径流过程进行了研究。利用Richards方程和水平衡方程,模拟了陕北不同降雨强度和土壤含水量下坡地入渗入渗过程。通过与观察结果进行比较可以得出结果:该时期累积入渗的平均相对误差小于3%,均方根误差(RSME)小于0.3。期间累计径流的平均相对误差小于12.5%,RSME <0.4。仿真结果合理。但是,模拟的淤积时间通常滞后于测量的淤积时间,这可能是由于饱和导水率的空间变化和降雨不均造成的。

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