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Development of combined tank model and saturated-unsaturated flow simulations and its application to the slope stability problem

机译:组合储罐模型与饱和-非饱和流模拟的发展及其在边坡稳定性问题中的应用

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Slope failure/collapse due to heavy rain occurs frequently and causes serious damages and losses of infrastructures. For the slope stability analysis, porewater pressure and its distribution along the potential sliding planes as well as their time evolution will be the most sensitive and important factors. To evaluate the porewater pressure distribution properly, a new technique combining the tank model and saturated-unsaturated flow simulations was proposed in this paper. Using this technique, the field condition can be represented more realistic by adjusting time-dependent hydraulic head boundary conditions as well as the infiltration of the rain water. The tank model was applied at both sides of modeling area to predict groundwater level variations due to rainfall intensity pulse. The groundwater level was derived from the components affecting water entering and leaving the system. The numerical flow simulations were carried out to estimate groundwater level within the modeling area controlled by physical characteristics of the system such as unsaturated soil properties. This proposed method was also implemented into the real field slope stability problem in Japan. Verification was carried out by comparing estimated groundwater level with a set of observed data. The flow simulation results show a good agreement with the observed ones.
机译:由于大雨而导致的斜坡破坏/坍塌经常发生,并造成严重的破坏和基础设施的损失。对于边坡稳定性分析,孔隙水压力及其沿潜在滑动面的分布及其时间演化将是最敏感和重要的因素。为了适当地评估孔隙水压力分布,提出了一种将储罐模型与饱和-不饱和水流模拟相结合的新技术。使用该技术,可以通过调整与时间有关的水力头边界条件以及雨水的渗透来更真实地表示现场条件。在建模区域的两侧应用储罐模型来预测由于降雨强度脉冲而引起的地下水位变化。地下水水位来自影响水进入和离开系统的各个组成部分。进行了数值流模拟,以估计受系统物理特性(例如不饱和土壤特性)控制的模型区内的地下水位。在日本的实际边坡稳定性问题中也采用了这种方法。通过将估计的地下水位与一组观测数据进行比较来进行验证。流动模拟结果与观察到的结果吻合良好。

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