基于土-水特征曲线参数的水分传递有限元建模及其在Nhan Co赤泥盆地边坡中的应用

N. Hoang, H. V. Hung, P. Dung
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引用次数: 0

摘要

自2017年以来,在德农省Nhan Co氧化铝厂的赤泥盆地,雨季发生了山体滑坡。雨水入渗引起的土体物理力学参数变化被认为是边坡失稳的主要因素。土壤的黏聚力和内摩擦角在很大程度上取决于土壤的含水量。具体来说,低含水率的土比高含水率的土具有更高的抗剪强度。通过土壤水分、土壤吸力、非饱和渗透性和土壤水分弥散度之间的关系建立非饱和土中水分传递的有限元模型,能够准确预测湿润锋的发展。在详细分析了解析误差估计和不同单元尺寸数值模拟误差的基础上,选择了单元尺寸和时间步长。采集土壤样品,在实验室中测定了土壤的不同吸力和相应的土壤水分值。采用最小二乘误差法对土壤水分特征曲线(SWCC)参数a、n和m进行了最佳拟合。确定了饱和土的水导率这一关键输入参数。在研究区边坡上的应用结果表明,在90天的雨水入渗输湿过程中,湿锋深度可达8米。湿润锋深度和水分分布曲线中间部分长度随入渗时间的增加而增加。土壤水分随深度的分布是边坡稳定性分析中获得土体强度参数的重要信息。土体剪切作用下的边坡稳定性分析________ *通讯作者。E-mail地址:VDC@yahoo.com https://doi.org/10.25073/2588-1094/vnuees.4655 N.V. Hoang et al. / VNU学报:地球与环境科学,Vol. 37, No. 1(2021) 103-115 104个强度参数与水分变化严格对应,可以提供最准确可靠的边坡稳定结果,提供更可靠的边坡稳定解决方案。
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Moisture Transfer Finite Element Modeling with Soil-Water Characteristic Curve-Based Parameters and its Application to Nhan Co Red Mud Basin Slope
Since the year of 2017, landslides at the red mud basins in Nhan Co alumina factory, Dak Nong province have been occurring during the rainy season. The change of the soil physical and mechanical parameters due to rainwater infiltration has been considered as the main factor of the slope instability. The soil cohesion and angle of internal friction depend greatly on the soil moisture. Specifically, soil with a lower moisture content has a higher shearing strength than that in soil with higher moisture content. The finite element modeling of moisture transfers in unsaturated soils through the relationship between soil moisture, soil suction, unsaturated permeability and soilmoisture dispersivity is capable of accurately predicting the wetting front development. The element sizes and time steps have been selected based on detailed analysis of analytical error estimation and on the numerical simulations with different element sizes numerical simulation errors. Soil samples had been taken then the soil different suctions and corresponding soil moisture values have been determined in the laboratory. The soil water characteristic curve (SWCC) parameters (a, n and m) have been determined by the best fitting using the least squared error method. The hydraulic conductivity of the saturated soil, one of the key input parameters was also determined. The results of the application to the study area's slope has shown that the wetting front depth could be up to 8 meters for 90 days of moisture transfer due to the rainwater infiltration. The wetting front depth and the length of the intermediate part of the moisture distribution curve have increased with the infiltration time. The soil moisture distribution with a depth is an essential information to have soil strength parameters for the slope stability analyses. The slope stability analysis with the soil shear ________ * Corresponding author. E-mail address: VDC@yahoo.com https://doi.org/10.25073/2588-1094/vnuees.4655 N.V. Hoang et al. / VNU Journal of Science: Earth and Environmental Sciences, Vol. 37, No. 1 (2021) 103-115 104 strength parameters which are strictly corresponding with the moisture change would provide the most accurate and reliable slope stability results and provide more reliable slope stabilization solutions.
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