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Analyses on variations in the unsaturated characteristics of a mine waste-dump slope during rainfall

机译:降雨过程中矿山排土场边坡非饱和特征的变化分析

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摘要

Field measurement units and a system were constructed and installed in a waste-dump slope at the Imgi mine to investigate and analyze the variations in the unsaturated characteristics of the soil. The field instrumentation system was composed of a data acquisition system, a solar system, and measuring sensors. The rainfall, matric suction, and volumetric water contents were continuously measured from the units in the instrumented site and analyzed with the soil water characteristic curve (SWCC) estimated from laboratory experiments. The variations in matric suction and volumetric water content were primarily affected by the rainfall intensity. At the surface of the slope, the largest increase and decrease in the changes in matric suction and volumetric water content were observed during the wetting and drying processes, respectively. The matric suction and volumetric water content measured from the instrumented area were compared with the SWCCs obtained from the laboratory test, and the measured data were located between the drying and wetting paths. The drying and wetting paths obtained from the laboratory test are regarded as primary drying and wetting curves, respectively. Therefore, the measured data can be defined as scanning curves, which are located between primary drying and wetting curves. The variations in matric suction according to volumetric water content were dependent on depth, and a wide range of variations was observed at shallow depths. It was confirmed that the unsaturated soil near the ground surface has the sensitive reaction induced by the infiltration and evaporation in nature.
机译:在Imgi矿的废物倾倒场中建造并安装了现场测量单元和系统,以调查和分析土壤非饱和特征的变化。现场仪表系统由数据采集系统,太阳能系统和测量传感器组成。从仪器现场中的单位连续测量降雨,基质吸力和体积水含量,并根据实验室实验估算出的土壤水分特征曲线(SWCC)进行分析。基质吸力和体积水含量的变化主要受降雨强度的影响。在斜坡表面,在润湿和干燥过程中分别观察到基质吸力和体积水含量变化的最大增加和减少。将从仪器区域测得的基质吸力和体积水含量与从实验室测试中获得的SWCC进行比较,测得的数据位于干燥和润湿路径之间。从实验室测试获得的干燥和润湿路径分别被视为主要干燥和润湿曲线。因此,可以将测得的数据定义为扫描曲线,位于初级干燥和润湿曲线之间。基质吸力随体积含水量的变化取决于深度,并且在浅深度观察到很大范围的变化。可以确定地表附近的非饱和土壤具有自然界中渗透和蒸发引起的敏感反应。

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