The generation of surface runoff in laboratory conditions using two portable rainfall simulators – an experimental study

M. Danáčová, M. Danko, R. Výleta, K. Hlavčová
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Abstract

The use of laboratory methods in soil water erosion studies and rainfall simulation experiments has recently been considered more important because of the many advantages in controlling rainfall-runoff processes and sediment transport. In a laboratory study, rainfall simulation experiments (one alone and two identical rainfall simulators connected in a series) were focused on an analysis of the impact of the size of the irrigated area on the temporal distribution and volume of the surface runoff and the amount of eroded soil material. The experiments were conducted on a disturbed soil sample exposed to quasi-continuous 60-minute simulated rainfall events with an intensity of 2.7 mm min -1 . The two experiments were carried out on slopes of different lengths of 0.25 m (irrigated area: 0.0625 m 2 ) and 0.5 m (irrigated area: 0.125 m 2 ). The results showed the effects of the size of the irrigated area on surface runoff generation and changes in the soil structure, sediment concentration, and amount of soil loss. Knowledge of the rate of changes in the volume of the surface runoff and soil loss with respect to the size of the irrigated area in the laboratory conditions and subsequent generalization of the results provides essential information, which is irreplaceable for the preparation of field measurements and obtaining essential calibration and validation data for erosion and rainfall-runoff modelling.
在实验室条件下使用两个便携式降雨模拟器产生地表径流-一项实验研究
在土壤水分侵蚀研究和降雨模拟实验中使用实验室方法最近被认为是更重要的,因为在控制降雨径流过程和泥沙运输方面有许多优点。在一项实验室研究中,降雨模拟实验(一个单独的和两个相同的降雨模拟器串联在一起)的重点是分析灌区的大小对地表径流的时间分布和体积以及侵蚀土壤物质的数量的影响。实验以受扰动土壤样品为研究对象,该土壤样品暴露于强度为2.7 mm min -1的准连续60分钟模拟降雨事件中。两项试验分别在0.25 m(灌区:0.0625 m 2)和0.5 m(灌区:0.125 m 2)不同长度的斜坡上进行。结果表明,灌区面积对地表产流、土壤结构、含沙量和土壤流失量的变化有影响。在实验室条件下,地表径流和土壤流失量随灌溉区面积的变化率的知识以及随后对结果的推广提供了必不可少的信息,这对于准备实地测量和获得侵蚀和降雨径流模型的基本校准和验证数据是不可替代的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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