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Numerical Simulation of Moisture Fluctuations in Unsaturated Expansive Clay, Heave/Settlement Predictions, and Validation with Field Measurements

机译:非饱和膨胀黏土中水分波动的数值模拟,升沉/沉降预测以及现场测量的验证

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Expansive soil problem is one of the major problems in the field of geotechnical engineering. The change in water content in unsaturated expansive soil is the major reason of heave or shrinkage of the soil. Numerical simulation is a valuable tool for analysis of water content or suction variation in unsaturated soil. Numerically solving unsaturated soil problems needs the assessment of moisture variation in time and space as a response to the variation of environmental factors such as rainfall and evaporation rate. This study involves a comparison of measured water contents of an expansive clay subgrade beneath a flexible pavement in the country road FM 2 project by TXDOT with numerical simulations conducted using VADOSE/W (Geo-Slope 2012). With the input of soil properties, climate data, and proper initial and boundary conditions, the numerical simulation results gave a good approximation of the water content variations as compared with the field measurements. Both numerical results and field measurements show that significant moisture fluctuations occurred in the clay subgrade under the unpaved shoulder and in the soil below the ditch, while moisture fluctuation was negligible in the subgrade below the pavement. This difference in water content change indicates the probable cause of the volume change as well as the longitudinal crack. After the model calibration and validation on the water content change, the heave/shrinkage of the subgrade soil was evaluated following the empirical equations based on the one-dimensional deformation assumption. For heave or shrinkage prediction the extreme weather (extreme dry and extreme wet period) conditions were considered. This study is of value in the sense that, the numerical results reached a good agreement with the measured moisture fluctuations. The research outcome indicates that VADOSE/W is a robust tool, capable of predicting the moisture content fluctuations below pavement with proper soil properties and initial and boundary conditions specified. This study highlights the convincing capacity of numerical simulations for predicting the moisture fluctuations in expansive soils. The analysis is simple but efficient for use in conventional engineering practice for designs of pavement and shallow foundation on expansive soils.
机译:膨胀土问题是岩土工程领域中的主要问题之一。非饱和膨胀土中水含量的变化是土壤胀大或收缩的主要原因。数值模拟是分析非饱和土壤中水分或吸力变化的有价值的工具。用数字方法解决非饱和土壤问题需要评估水分在时间和空间上的变化,以响应降雨和蒸发速率等环境因素的变化。这项研究包括将TXDOT在乡村公路FM 2项目中的柔性人行道下膨胀粘土路基的含水量与使用VADOSE / W进行的数值模拟(Geo-Slope 2012)进行比较。通过输入土壤特性,气候数据以及适当的初始条件和边界条件,与田间测量相比,数值模拟结果可以很好地逼近含水量的变化。数值结果和现场测量都表明,在未铺砌的路肩下的粘土路基和沟渠以下的土壤中,水分的波动很大,而在人行道下的路基中,水分的波动可以忽略不计。含水量变化的这种差异表明了体积变化以及纵向裂纹的可能原因。在模型校准和对含水量变化的验证之后,基于一维变形假设,根据经验方程式对路基土壤的胀大/收缩进行了评估。对于隆起或收缩预测,考虑了极端天气(极端干燥和极端潮湿期)条件。在一定意义上说,这项研究具有价值,数值结果与测得的水分波动达到了很好的一致性。研究结果表明,VADOSE / W是一款功能强大的工具,能够在适当的土壤特性以及指定的初始和边界条件下,预测人行道下方的含水量波动。这项研究强调了数值模拟在预测膨胀土中水分波动方面的令人信服的能力。该分析很简单,但在常规工程实践中用于膨胀土的人行道和浅层基础设计时有效。

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