Laboratory and theoretical investigations on the deformation and strength behaviors of artificial frozen soil
In order to study the mechanical characteristic of artificial frozen soils, such as strength, and stress–strain relationship, a series of triaxial compression tests of frozen sand has been conducted under confining pressures varying from 0.0 to 14.0 MPa with different water contents at − 6 °C. Froze...
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Veröffentlicht in: | Cold regions science and technology 2010-10, Vol.64 (1), p.39-45 |
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description | In order to study the mechanical characteristic of artificial frozen soils, such as strength, and stress–strain relationship, a series of triaxial compression tests of frozen sand has been conducted under confining pressures varying from 0.0 to 14.0
MPa with different water contents at −
6
°C. Frozen sand presents strain softening during shearing process under low confining pressures; but with increasing confining pressure, the strain softening decreases, and even presents strain hardening under high confining pressures. The strength of frozen sand is affected by water content and confining pressure. The strength with low water content always increases with increasing confining pressure; however, for frozen sand with a high water content, the strength experiences an increase followed by a decrease with increasing confining pressure. To describe the strength characteristic of frozen sand, the non-linear Mohr–Coulomb criterion, in which the generalized internal friction angle and cohesion under various confining pressures are obtained from experimental results, has been presented. The result shows that the non-linear Mohr–Coulomb criterion can reflect the decrease of strength of frozen sand under high confining pressures. The stress–strain relationships of frozen sand are represented by hyperbolic functions, which can describe both the strain hardening behavior of frozen sand under high confining pressure and the strain softening behavior under a low confining pressure. |
doi_str_mv | 10.1016/j.coldregions.2010.07.003 |
format | Article |
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MPa with different water contents at −
6
°C. Frozen sand presents strain softening during shearing process under low confining pressures; but with increasing confining pressure, the strain softening decreases, and even presents strain hardening under high confining pressures. The strength of frozen sand is affected by water content and confining pressure. The strength with low water content always increases with increasing confining pressure; however, for frozen sand with a high water content, the strength experiences an increase followed by a decrease with increasing confining pressure. To describe the strength characteristic of frozen sand, the non-linear Mohr–Coulomb criterion, in which the generalized internal friction angle and cohesion under various confining pressures are obtained from experimental results, has been presented. The result shows that the non-linear Mohr–Coulomb criterion can reflect the decrease of strength of frozen sand under high confining pressures. The stress–strain relationships of frozen sand are represented by hyperbolic functions, which can describe both the strain hardening behavior of frozen sand under high confining pressure and the strain softening behavior under a low confining pressure.</description><identifier>ISSN: 0165-232X</identifier><identifier>EISSN: 1872-7441</identifier><identifier>DOI: 10.1016/j.coldregions.2010.07.003</identifier><identifier>CODEN: CRSTDL</identifier><language>eng</language><publisher>Amsterdam: Elsevier B.V</publisher><subject>Artificial frozen soil ; Confining ; Earth sciences ; Earth, ocean, space ; Engineering and environment geology. Geothermics ; Engineering geology ; Exact sciences and technology ; External geophysics ; Freezing ; Frozen ; Frozen soils ; Generalized cohesion ; Generalized internal friction angle ; Moisture content ; Sand ; Snow. Ice. Glaciers ; Strain hardening ; Strain softening ; Strength ; Stress–strain relationship</subject><ispartof>Cold regions science and technology, 2010-10, Vol.64 (1), p.39-45</ispartof><rights>2010 Elsevier B.V.</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a472t-5b56509d5e21cea50cf65a8a2d370c37816f26f8f28721d7ea00c960f60e2d6b3</citedby><cites>FETCH-LOGICAL-a472t-5b56509d5e21cea50cf65a8a2d370c37816f26f8f28721d7ea00c960f60e2d6b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0165232X10001448$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27903,27904,65309</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=23287810$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Yang, Yugui</creatorcontrib><creatorcontrib>Lai, Yuanming</creatorcontrib><creatorcontrib>Chang, Xiaoxiao</creatorcontrib><title>Laboratory and theoretical investigations on the deformation and strength behaviors of artificial frozen soil</title><title>Cold regions science and technology</title><description>In order to study the mechanical characteristic of artificial frozen soils, such as strength, and stress–strain relationship, a series of triaxial compression tests of frozen sand has been conducted under confining pressures varying from 0.0 to 14.0
MPa with different water contents at −
6
°C. Frozen sand presents strain softening during shearing process under low confining pressures; but with increasing confining pressure, the strain softening decreases, and even presents strain hardening under high confining pressures. The strength of frozen sand is affected by water content and confining pressure. The strength with low water content always increases with increasing confining pressure; however, for frozen sand with a high water content, the strength experiences an increase followed by a decrease with increasing confining pressure. To describe the strength characteristic of frozen sand, the non-linear Mohr–Coulomb criterion, in which the generalized internal friction angle and cohesion under various confining pressures are obtained from experimental results, has been presented. The result shows that the non-linear Mohr–Coulomb criterion can reflect the decrease of strength of frozen sand under high confining pressures. The stress–strain relationships of frozen sand are represented by hyperbolic functions, which can describe both the strain hardening behavior of frozen sand under high confining pressure and the strain softening behavior under a low confining pressure.</description><subject>Artificial frozen soil</subject><subject>Confining</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Engineering geology</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Freezing</subject><subject>Frozen</subject><subject>Frozen soils</subject><subject>Generalized cohesion</subject><subject>Generalized internal friction angle</subject><subject>Moisture content</subject><subject>Sand</subject><subject>Snow. Ice. Glaciers</subject><subject>Strain hardening</subject><subject>Strain softening</subject><subject>Strength</subject><subject>Stress–strain relationship</subject><issn>0165-232X</issn><issn>1872-7441</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNqNkE1vGyEQhlHVSnXd_oftIeppHWDNsj5WVppWspRLIvWGxjDYWGtIBmIp-fVl4yjKsSfE8H4wD2PfBV8ILvrLw8Km0RHuQop5IXmdc73gvPvAZmLQstXLpfjIZlWrWtnJv5_Zl5wPvN5Xqpux4wa2iaAkemoguqbsMRGWYGFsQjxhLmEHZQpvUpxeG4c-0fFl9uLIhTDuyr7Z4h5OIVFV-gaoBB9sqDGe0jPGJqcwfmWfPIwZv72ec3b36-p2_bvd3Fz_Wf_ctLDUsrRqq3rFV06hFBZBcet7BQNI12luOz2I3sveD17WDYXTCJzbVc99z1G6ftvN2Y9z7j2lh8e6hDmGbHEcIWJ6zEZXn1KiYpqz1VlpKeVM6M09hSPQkxHcTITNwbwjbCbChmtTrdV78doCufLyBNGG_BZQaQ_1q1PH-qzDuvIpIJlsA0aLLhDaYlwK_9H2D-pXmlU</recordid><startdate>20101001</startdate><enddate>20101001</enddate><creator>Yang, Yugui</creator><creator>Lai, Yuanming</creator><creator>Chang, Xiaoxiao</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TB</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20101001</creationdate><title>Laboratory and theoretical investigations on the deformation and strength behaviors of artificial frozen soil</title><author>Yang, Yugui ; Lai, Yuanming ; Chang, Xiaoxiao</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a472t-5b56509d5e21cea50cf65a8a2d370c37816f26f8f28721d7ea00c960f60e2d6b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>Artificial frozen soil</topic><topic>Confining</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Engineering and environment geology. Geothermics</topic><topic>Engineering geology</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Freezing</topic><topic>Frozen</topic><topic>Frozen soils</topic><topic>Generalized cohesion</topic><topic>Generalized internal friction angle</topic><topic>Moisture content</topic><topic>Sand</topic><topic>Snow. Ice. Glaciers</topic><topic>Strain hardening</topic><topic>Strain softening</topic><topic>Strength</topic><topic>Stress–strain relationship</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Yang, Yugui</creatorcontrib><creatorcontrib>Lai, Yuanming</creatorcontrib><creatorcontrib>Chang, Xiaoxiao</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Cold regions science and technology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Yang, Yugui</au><au>Lai, Yuanming</au><au>Chang, Xiaoxiao</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Laboratory and theoretical investigations on the deformation and strength behaviors of artificial frozen soil</atitle><jtitle>Cold regions science and technology</jtitle><date>2010-10-01</date><risdate>2010</risdate><volume>64</volume><issue>1</issue><spage>39</spage><epage>45</epage><pages>39-45</pages><issn>0165-232X</issn><eissn>1872-7441</eissn><coden>CRSTDL</coden><abstract>In order to study the mechanical characteristic of artificial frozen soils, such as strength, and stress–strain relationship, a series of triaxial compression tests of frozen sand has been conducted under confining pressures varying from 0.0 to 14.0
MPa with different water contents at −
6
°C. Frozen sand presents strain softening during shearing process under low confining pressures; but with increasing confining pressure, the strain softening decreases, and even presents strain hardening under high confining pressures. The strength of frozen sand is affected by water content and confining pressure. The strength with low water content always increases with increasing confining pressure; however, for frozen sand with a high water content, the strength experiences an increase followed by a decrease with increasing confining pressure. To describe the strength characteristic of frozen sand, the non-linear Mohr–Coulomb criterion, in which the generalized internal friction angle and cohesion under various confining pressures are obtained from experimental results, has been presented. The result shows that the non-linear Mohr–Coulomb criterion can reflect the decrease of strength of frozen sand under high confining pressures. The stress–strain relationships of frozen sand are represented by hyperbolic functions, which can describe both the strain hardening behavior of frozen sand under high confining pressure and the strain softening behavior under a low confining pressure.</abstract><cop>Amsterdam</cop><pub>Elsevier B.V</pub><doi>10.1016/j.coldregions.2010.07.003</doi><tpages>7</tpages></addata></record> |
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source | Elsevier ScienceDirect Journals |
subjects | Artificial frozen soil Confining Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Engineering geology Exact sciences and technology External geophysics Freezing Frozen Frozen soils Generalized cohesion Generalized internal friction angle Moisture content Sand Snow. Ice. Glaciers Strain hardening Strain softening Strength Stress–strain relationship |
title | Laboratory and theoretical investigations on the deformation and strength behaviors of artificial frozen soil |
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