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The study on the development saturation profile in soil its effect on groundwater fluctuation

机译:土壤发育饱和度分布特征及其对地下水波动的影响研究

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摘要

This study was carried out to investigate the mechanisms involved in the development of saturation profiles in soil. A series of numerical simulations and laboratory tests were conducted to monitor the saturation profiles in four types of soil under various rainfall conditions. In addition, two sloping sites were monitored for a period of one year to provide field verification for the findings. The understanding in saturation profile is essential to predict the shear strength of soil, particularly for slope stability problem. The study showed that the saturation profile in soil is greatly affected by the soil permeability and rainfall pattern. The effect of rainfall pattern on the saturation profile of high permeable soil is relatively insignificant. Conversely, the saturation profile in less permeable soil could be significantly altered when the soil is subjected to a prolonged rainfall. A chart is developed in the present study to determine the critical rainfall duration and intensity, as well as the resultant minimum suction value. The analysis result from the developed chart show good agreement with the field monitoring data. It is believed that the findings from the present study could lead to a better understanding of saturation profile in soil, and subsequently contribute efforts in mitigating rainfall-induced slope failure.
机译:进行了这项研究以调查参与土壤饱和度剖面发展的机制。进行了一系列数值模拟和实验室测试,以监测四种降雨条件下四种土壤的饱和度分布。此外,对两个斜坡站点进行了为期一年的监控,以对发现的结果进行现场验证。对饱和度剖面的理解对于预测土壤的抗剪强度至关重要,特别是对于边坡稳定性问题。研究表明,土壤的饱和度剖面受土壤渗透率和降雨模式的影响很大。降雨模式对高渗透性土壤饱和度剖面的影响相对较小。相反,当土壤受到长时间降雨时,渗透性较低的土壤中的饱和度分布可能会发生显着变化。在本研究中开发了一个图表,以确定临界降雨持续时间和强度,以及由此产生的最小吸力值。所开发图表的分析结果与现场监测数据吻合良好。可以相信,本研究的结果可以使人们更好地了解土壤的饱和度分布,并为减轻降雨引起的边坡破坏做出贡献。

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