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Laboratory experiments on rainfall-induced flowslide from pore pressure and moisture content measurements

水槽 植被与边坡稳定性 含水量 压力计 孔隙水压力 岩土工程 边坡稳定性 边坡破坏 饱和(图论) 地表径流 地质学 水分 前期水分 环境科学 土壤科学 材料科学 流量(数学) 地下水 含水层 生物 数学 组合数学 径流曲线数 复合材料 生态学 几何学
作者
M. R. Hakro,I. S. H. Harahap
出处
期刊:Natural Hazards and Earth System Sciences Discussions 被引量:12
标识
DOI:10.5194/nhessd-3-1575-2015
摘要

Abstract. During or immediately after rainfall many slope failures have been observed. The slope failure occurred due to rainfall infiltration that rapidly increase the pore pressure and trigger the slope failure. Numerous studies have been conducted to investigate the rainfall-induced slope failure, but the mechanism of slope failure is still not well clarified. To investigate mechanism of rainfall-induced slope failure laboratory experiments have been conducted in flume. The slope was prepared with sandy soil in flume with constant inclination of 45°, because most of rainfall-induced slope failure occurred in sandy soil and on steep slope. The hydrological parameters such as pore pressure and moisture content were measured with piezometers and advanced Imko TDRs respectively. The slope failure occurred due to increase in moisture content and rise in pore pressure. During the flowslide type of slope failure the sudden increase in pore pressure was observed. The higher moisture content and pore pressure was at the toe of the slope. The pore pressure was higher at the toe of the slope and smaller at the upper part of the slope. After the saturation the run-off was observed at the toe of the slope that erodes the toe and forming the gullies from toe to upper part of the slope. In the case antecedent moisture conditions the moisture content and the pore pressure increased quickly and producing the surface runoff at the horizontal part of the slope. The slope having less density suffer from flowslide type of the failure, however in dense slope no major failure was occurred even at higher rainfall intensity. The antecedent moisture accompanied with high rainfall intensity also not favors the initiation of flowslide in case of dense slope. The flowslide type of failure can be avoided by controlling the density of soil slope. Knowing such parameters that controls the large mass movement helpful in developing the early warning system for flowslide type of failure.
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