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Experimental study of the hydraulic behaviour of Melbourne silt

机译:墨尔本淤泥水力特性试验研究

摘要

Soil partially saturated with water is referred to as unsaturated soil. Unsaturated soil has very complicated behaviour. A change in the degree of saturation can cause significant changes in soil volume, shear strength and hydraulic properties. Recently, research interest in soil’s thermo-hydro-mechanical interactive behaviour is growing due to an increasing number of geotechnical problems involving thermal and unsaturated issues. For example, soils surrounding buried nuclear waste would certainly be casted into elevated temperature and partially saturated conditions. The soil-water characteristic curve (SWCC, also called soil-water retention curve, SWRC) has emerged as a widely used estimation tool for obtaining soil’s hydraulic properties in unsaturated state. However, the current test results and theoretical investigation on SWCCs are limited within isothermal states and deformation caused by temperature variation is usually neglected for simplification purpose. The proposed research aims to investigate the influences of temperature on the water retention behaviour of deformable unsaturated soil. Volume change caused by temperature variation will be taken into consideration. This research will produce a better understanding and interpretation of thermal effects on SWCCs by providing experimental results for deformable unsaturated soils.
机译:被水部分饱和的土壤称为不饱和土壤。不饱和土壤的行为非常复杂。饱和度的变化会导致土壤体积,抗剪强度和水力性质发生重大变化。近来,由于涉及热和非饱和问题的岩土工程问题越来越多,对土壤的热-水-机械相互作用行为的研究兴趣正在增长。例如,埋在核废料周围的土壤肯定会被浇铸成高温和部分饱和的状态。土壤-水特征曲线(SWCC,也称为土壤-水保持曲线,SWRC)已经成为一种广泛使用的估算工具,用于获得非饱和状态下的土壤水力特性。但是,目前关于SWCC的测试结果和理论研究仅限于等温状态,为简化起见,通常忽略了温度变化引起的变形。拟议的研究旨在调查温度对可变形不饱和土壤保水性能的影响。将考虑温度变化引起的体积变化。通过提供可变形非饱和土的实验结果,这项研究将更好地理解和解释SWCC的热效应。

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    Wang Lijing;

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  • 年度 2014
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