Anisotropy effect of the clay soil masses on the stress-strain state of transport tunnels

The article considers the kinds of clay soil mass anisotropy in the form of the spatial heterogeneity of properties of thawed and frozen soils, ambiguity of the frost heaving values and shrinkage in different directions. The questions of anisotropy of the clay soil properties at the positive tempera...

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Main Authors: Yushkov Boris Semenovich, Tretyakova Olga Viktorovna
Format: Article
Language:Russian
Published: «Publishing company «World of science», LLC 2014-09-01
Series:Transportnye Sooruženiâ
Subjects:
Online Access:https://t-s.today/en/01TS314.html
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spelling doaj-3cc2bd2d3ea5472891d21964283a03fb2020-11-25T02:06:23Zrus«Publishing company «World of science», LLCTransportnye Sooruženiâ2413-98072014-09-011310.15862/01TS314Anisotropy effect of the clay soil masses on the stress-strain state of transport tunnelsYushkov Boris Semenovich0Tretyakova Olga Viktorovna1Perm National Research Polytechnic University«PZSP»The article considers the kinds of clay soil mass anisotropy in the form of the spatial heterogeneity of properties of thawed and frozen soils, ambiguity of the frost heaving values and shrinkage in different directions. The questions of anisotropy of the clay soil properties at the positive temperatures are reported. The dependence of the heterogeneity of the physical and mechanical properties of frozen soils from the cryogenic texture, natural arrangement, different types of stratification and interbedding is considered. Indexes of the strength and strain anisotropy are noted. The accounting possibilities of the basic numerical indexes of heaving phenomena from the standpoint of anisotropy of the properties and processes inherent in the freezing through soil are analyzed by substitution in the heaving strain formula. The unevenness of thawed soil shrinkage in vertical and horizontal directions is noted during the freezing of the top layer. The unevenness of shrinkage in different directions is connected with kind of stress and cryogenic texture. Anisotropy of the frost heaving process is considered in the context of one-dimensional and non-one-dimensional problem depending on the amount of the freezing fronts and their direction. There is summarized the effect of anisotropy appearances on the stress-strain state of the transport tunnel. One can conclude that the resulting non-uniformity of heaving and shrinkage in conjunction with anisotropic properties of frozen soils, is a significant component in the complex of power factors determining the optimal design solution of a transport tunnel.https://t-s.today/en/01TS314.htmlice formation; moisture migration; cryogenic texture; ice-cement; ice schliers; frost heaving; anisotropy; stress-strain state (SSS)
collection DOAJ
language Russian
format Article
sources DOAJ
author Yushkov Boris Semenovich
Tretyakova Olga Viktorovna
spellingShingle Yushkov Boris Semenovich
Tretyakova Olga Viktorovna
Anisotropy effect of the clay soil masses on the stress-strain state of transport tunnels
Transportnye Sooruženiâ
ice formation; moisture migration; cryogenic texture; ice-cement; ice schliers; frost heaving; anisotropy; stress-strain state (SSS)
author_facet Yushkov Boris Semenovich
Tretyakova Olga Viktorovna
author_sort Yushkov Boris Semenovich
title Anisotropy effect of the clay soil masses on the stress-strain state of transport tunnels
title_short Anisotropy effect of the clay soil masses on the stress-strain state of transport tunnels
title_full Anisotropy effect of the clay soil masses on the stress-strain state of transport tunnels
title_fullStr Anisotropy effect of the clay soil masses on the stress-strain state of transport tunnels
title_full_unstemmed Anisotropy effect of the clay soil masses on the stress-strain state of transport tunnels
title_sort anisotropy effect of the clay soil masses on the stress-strain state of transport tunnels
publisher «Publishing company «World of science», LLC
series Transportnye Sooruženiâ
issn 2413-9807
publishDate 2014-09-01
description The article considers the kinds of clay soil mass anisotropy in the form of the spatial heterogeneity of properties of thawed and frozen soils, ambiguity of the frost heaving values and shrinkage in different directions. The questions of anisotropy of the clay soil properties at the positive temperatures are reported. The dependence of the heterogeneity of the physical and mechanical properties of frozen soils from the cryogenic texture, natural arrangement, different types of stratification and interbedding is considered. Indexes of the strength and strain anisotropy are noted. The accounting possibilities of the basic numerical indexes of heaving phenomena from the standpoint of anisotropy of the properties and processes inherent in the freezing through soil are analyzed by substitution in the heaving strain formula. The unevenness of thawed soil shrinkage in vertical and horizontal directions is noted during the freezing of the top layer. The unevenness of shrinkage in different directions is connected with kind of stress and cryogenic texture. Anisotropy of the frost heaving process is considered in the context of one-dimensional and non-one-dimensional problem depending on the amount of the freezing fronts and their direction. There is summarized the effect of anisotropy appearances on the stress-strain state of the transport tunnel. One can conclude that the resulting non-uniformity of heaving and shrinkage in conjunction with anisotropic properties of frozen soils, is a significant component in the complex of power factors determining the optimal design solution of a transport tunnel.
topic ice formation; moisture migration; cryogenic texture; ice-cement; ice schliers; frost heaving; anisotropy; stress-strain state (SSS)
url https://t-s.today/en/01TS314.html
work_keys_str_mv AT yushkovborissemenovich anisotropyeffectoftheclaysoilmassesonthestressstrainstateoftransporttunnels
AT tretyakovaolgaviktorovna anisotropyeffectoftheclaysoilmassesonthestressstrainstateoftransporttunnels
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