DEFORMATIONS OF SOIL MASSES UNDER THE ACTION OF HUMAN-INDUCED FACTORS

M. Kuzlo, V. Moshynskyi, Nataliya Zhukovska, V. Zhukovskyy
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引用次数: 0

Abstract

Significant changes in the stress-strain state cause a change in the soil profile of the massif, which is affected by various physical and chemical factors. In particular, groundwater filtration, mass transfer, heat transfer, dissolution and leaching of soil masses. This can lead to various types of accidents. Therefore, the study of the stress-strain state of the soil massif is an important topic. Nonlinear dependences in the form of polynomials of the modulus of deformation and Lame coefficients on the concentration of salt solutions and their temperature have been received in this research based on experimental research and their statistical processing. This allowed improving the mathematical model of the stress-strain state of the soil taking into account the nonlinear deformation processes occurring in the soil masses under the presence and filtration of saline solutions in non-isothermal conditions.
人为因素作用下的土块变形
应力-应变状态的显著变化会引起地块土壤剖面的变化,而这种变化会受到各种物理和化学因素的影响。特别是地下水的过滤、传质、传热、土块的溶解和沥滤。这可能导致各种类型的事故。因此,研究土体的应力应变状态是一个重要课题。本研究在实验研究和统计处理的基础上,获得了盐溶液浓度和温度对变形模量和拉梅系数的多项式形式的非线性依赖关系。这有助于改进土壤应力-应变状态的数学模型,同时考虑到在非等温条件下盐溶液存在和过滤时土体发生的非线性变形过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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