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Research on Xilamuren Desert-steppe Rainfall Experiment Segmentation Regular Pattern — Based on Rainfall Simulation Experiment

机译:Xilamuren Desert-Steppe降雨实验细分常规模式研究 - 基于降雨模拟实验

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The rainfall is the main soil water supply to the soil of desert-steppe. It divides into three parts, evaporation, infiltration and runoff, after falling on to the surface. Those three parts are affected by many factors. Studies of rainfall division in desert-steppe were rare, the proportions of evaporation, infiltration and runoff are uncertain. So Under the condition of different vegetation, we conduct six times rainfall simulation experiment under different rainfall intensity. Simulation shows that rainfall process, the surface coverage and soil condition affect division. The evaporation section of rainfall accounted for 1/2 ~ 2/3. Infiltration section accounted for 30% ~ 50%. Runoff is the smallest. The rainfall intensity plays a decisive role on the runoff. Different vegetation coverage, division proportion is different. The interception and delay function of vegetation main effect evaporation and runoff, it can make the evaporation increased to more than 70%, reduce runoff to a third. Water content of soil profile before rainfall is the main factors affecting infiltration volume. The soil moisture before rain affects the infiltration rate at the beginning of rainfall. If rainfall duration is long enough, infiltration capacity is almost a constant.
机译:降雨是沙漠草原土壤的主要土壤供水。它在落到表面后分为三个部分,蒸发,渗透和径流。这三个部分受到许多因素的影响。在沙漠草原降雨分裂的研究很少见,蒸发,渗透和径流的比例不确定。因此,在不同植被的条件下,我们在不同的降雨强度下进行了六次降雨模拟实验。仿真显示降雨过程,表面覆盖和土壤条件影响划分。降雨的蒸发部分占1/2〜2/3。渗透部分占30%〜50%。径流是最小的。降雨强度在径流中起着决定性作用。不同的植被覆盖,分裂比例不同。植被的截取和延迟功能蒸发和径流,它可以使蒸发增加到70%以上,减少径流到第三个。降雨前土壤分析含水量是影响渗透量的主要因素。雨前的土壤水分影响降雨开始时的渗透率。如果降雨持续时间足够长,渗透能力几乎是一个常数。

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