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首页> 外文期刊>Canadian Geotechnical Journal >Flume-scale laboratory study of rainfall-runoff responses in Devon silt and capillary barrier profiles
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Flume-scale laboratory study of rainfall-runoff responses in Devon silt and capillary barrier profiles

机译:德文淤泥和毛细管屏障剖面降雨径流响应的水槽级实验室研究

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摘要

The design of soil covers for mine waste reclamation requires comprehensive water balance calculations at the ground surface and the subsurface. To achieve a determinate water balance equation, rainfall-runoff quantities need to be predicted or measured. The parameters that control rainfall runoff were investigated by performing rainfall-runoff experiments on Devon silt and capillary barrier profiles at different saturation stages. A rainfall simulator apparatus was employed to measure water balance components at different rainfall intensities during each test; the apparatus' design is presented. The rainfall intensity and the saturated hydraulic conductivity of the soil govern runoff volumes and rates in the saturated profiles. The rainfall intensity and infiltration capacity of the soil govern runoff volumes and rates in the unsaturated profiles. The capillary barrier effects are evaluated and discussed by comparing time-lapse photographs of the wetting front during each test with changes in matric suction and volumetric water content measurements.
机译:矿山废物复垦的土壤覆盖层设计需要在地表和地下进行全面的水平衡计算。为了获得确定的水平衡方程,需要预测或测量降雨径流量。通过在不同饱和阶段对德文郡淤泥和毛细屏障剖面进行降雨径流试验,研究了控制降雨径流的参数。在每次试验期间,使用降雨模拟装置测量不同降雨强度下的水平衡分量;介绍了该装置的设计。降雨强度和土壤的饱和水力传导率决定了饱和剖面中的径流量和速率。土壤的降雨强度和渗透能力决定了非饱和剖面中的径流量和速率。通过比较每次试验期间湿润锋的延时照片与基质吸力和体积含水量测量值的变化,评估和讨论毛细屏障效应。

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