Liquid bridge contribution to shear behavior of unsaturated soil: modeling and application to a micromechanics model
Liquid bridges in unsaturated soils attach to grain contacts and contribute to strengthening microscopic bonding forces, which leads to macroscopic high strength and stiffness compared with dry or saturated soils. This study investigated microscopic liquid bridge behaviors in monodisperse granular m...
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description | Liquid bridges in unsaturated soils attach to grain contacts and contribute to strengthening microscopic bonding forces, which leads to macroscopic high strength and stiffness compared with dry or saturated soils. This study investigated microscopic liquid bridge behaviors in monodisperse granular media by combining X-ray micro-computed tomography and image analyses. Evaluating the anisotropy of grain contact orientation by fabric tensor revealed that fabric transitions under a triaxial process for both grain contacts and that with liquid bridges are equivalent, which indicates that the orientation of the liquid bridge contribution does not have unique anisotropy. The liquid bridge ratio (LBR) was defined as the ratio of the number of grain contacts with liquid bridges to the total number of grain contacts, representing the magnitude of the liquid bridge contribution. LBR distributions—the relationship of LBR to degree of saturation obtained by water retention tests for both dense and loose specimens—exhibited different peak positions depending on the void ratio and constant dispersion, which was then modeled using
β
distribution. A constitutive model on an experimental micromechanics basis for unsaturated soils was proposed by applying the liquid bridge contribution model as a combination of the LBR distribution model and the soil water characteristic curve model to a micromechanics model, in which spherical and monodisperse grains are assumed and the pendular saturation regime is focused. The proposed model qualitatively reproduced the macroscopic suction effect by describing the microscopic liquid bridge contribution. |
doi_str_mv | 10.1007/s11440-021-01263-0 |
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β
distribution. A constitutive model on an experimental micromechanics basis for unsaturated soils was proposed by applying the liquid bridge contribution model as a combination of the LBR distribution model and the soil water characteristic curve model to a micromechanics model, in which spherical and monodisperse grains are assumed and the pendular saturation regime is focused. The proposed model qualitatively reproduced the macroscopic suction effect by describing the microscopic liquid bridge contribution.</description><identifier>ISSN: 1861-1125</identifier><identifier>EISSN: 1861-1133</identifier><identifier>DOI: 10.1007/s11440-021-01263-0</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Anisotropy ; Behavior ; Bonding strength ; Complex Fluids and Microfluidics ; Computed tomography ; Constitutive models ; Distribution ; Engineering ; Fabrics ; Foundations ; Geoengineering ; Geotechnical Engineering & Applied Earth Sciences ; Grain size ; Granular materials ; Granular media ; Hydraulics ; Laboratories ; Liquid bridges ; Mathematical models ; Micromechanics ; Moisture content ; Orientation ; Research Paper ; Retention ; Saturated soils ; Saturation ; Soft and Granular Matter ; Soil ; Soil investigations ; Soil Science & Conservation ; Soil suction ; Soil water ; Solid Mechanics ; Stiffness ; Tensors ; Tomography ; Unsaturated soils ; Void ratio</subject><ispartof>Acta geotechnica, 2021-09, Vol.16 (9), p.2693-2711</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2021</rights><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2021.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a408t-7090d62eeb48497fd5f0616fe7a1d1c82f79c19f41c01035035ec6fcb8bf40583</citedby><cites>FETCH-LOGICAL-a408t-7090d62eeb48497fd5f0616fe7a1d1c82f79c19f41c01035035ec6fcb8bf40583</cites><orcidid>0000-0003-2818-2435 ; 0000-0002-4879-540X ; 0000-0003-0694-1322 ; 0000-0002-2553-7643</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11440-021-01263-0$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11440-021-01263-0$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51298</link.rule.ids></links><search><creatorcontrib>Fukushima, Yo</creatorcontrib><creatorcontrib>Higo, Yosuke</creatorcontrib><creatorcontrib>Matsushima, Takashi</creatorcontrib><creatorcontrib>Otake, Yu</creatorcontrib><title>Liquid bridge contribution to shear behavior of unsaturated soil: modeling and application to a micromechanics model</title><title>Acta geotechnica</title><addtitle>Acta Geotech</addtitle><description>Liquid bridges in unsaturated soils attach to grain contacts and contribute to strengthening microscopic bonding forces, which leads to macroscopic high strength and stiffness compared with dry or saturated soils. This study investigated microscopic liquid bridge behaviors in monodisperse granular media by combining X-ray micro-computed tomography and image analyses. Evaluating the anisotropy of grain contact orientation by fabric tensor revealed that fabric transitions under a triaxial process for both grain contacts and that with liquid bridges are equivalent, which indicates that the orientation of the liquid bridge contribution does not have unique anisotropy. The liquid bridge ratio (LBR) was defined as the ratio of the number of grain contacts with liquid bridges to the total number of grain contacts, representing the magnitude of the liquid bridge contribution. LBR distributions—the relationship of LBR to degree of saturation obtained by water retention tests for both dense and loose specimens—exhibited different peak positions depending on the void ratio and constant dispersion, which was then modeled using
β
distribution. A constitutive model on an experimental micromechanics basis for unsaturated soils was proposed by applying the liquid bridge contribution model as a combination of the LBR distribution model and the soil water characteristic curve model to a micromechanics model, in which spherical and monodisperse grains are assumed and the pendular saturation regime is focused. The proposed model qualitatively reproduced the macroscopic suction effect by describing the microscopic liquid bridge contribution.</description><subject>Anisotropy</subject><subject>Behavior</subject><subject>Bonding strength</subject><subject>Complex Fluids and Microfluidics</subject><subject>Computed tomography</subject><subject>Constitutive models</subject><subject>Distribution</subject><subject>Engineering</subject><subject>Fabrics</subject><subject>Foundations</subject><subject>Geoengineering</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Grain size</subject><subject>Granular materials</subject><subject>Granular media</subject><subject>Hydraulics</subject><subject>Laboratories</subject><subject>Liquid bridges</subject><subject>Mathematical models</subject><subject>Micromechanics</subject><subject>Moisture content</subject><subject>Orientation</subject><subject>Research Paper</subject><subject>Retention</subject><subject>Saturated soils</subject><subject>Saturation</subject><subject>Soft and Granular Matter</subject><subject>Soil</subject><subject>Soil investigations</subject><subject>Soil Science & Conservation</subject><subject>Soil suction</subject><subject>Soil water</subject><subject>Solid Mechanics</subject><subject>Stiffness</subject><subject>Tensors</subject><subject>Tomography</subject><subject>Unsaturated soils</subject><subject>Void ratio</subject><issn>1861-1125</issn><issn>1861-1133</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kE1LxDAQhosouK7-AU8Bz9WZJE1bbyJ-wYIXPYc0H7tZ2mY3aQX_vdX6cRMGZg7POzM8WXaOcIkA5VVC5BxyoJgDUsFyOMgWWAnMERk7_J1pcZydpLQFEIxysciGld-P3pAmerO2RId-iL4ZBx96MgSSNlZF0tiNevMhkuDI2Cc1jFEN1pAUfHtNumBs6_s1Ub0hardrvVY_eUU6r2PorN6o3us0w6fZkVNtsmfffZm93t-93D7mq-eHp9ubVa44VENeQg1GUGsbXvG6dKZwIFA4Wyo0qCvqylpj7ThqQGDFVFYLp5uqcRyKii2zi3nvLob9aNMgt2GM_XRS0kKwmtO6EhNFZ2p6NKVondxF36n4LhHkp10525WTXfllV8IUYnMoTXC_tvFv9T-pD1I_fmw</recordid><startdate>20210901</startdate><enddate>20210901</enddate><creator>Fukushima, Yo</creator><creator>Higo, Yosuke</creator><creator>Matsushima, Takashi</creator><creator>Otake, Yu</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><orcidid>https://orcid.org/0000-0003-2818-2435</orcidid><orcidid>https://orcid.org/0000-0002-4879-540X</orcidid><orcidid>https://orcid.org/0000-0003-0694-1322</orcidid><orcidid>https://orcid.org/0000-0002-2553-7643</orcidid></search><sort><creationdate>20210901</creationdate><title>Liquid bridge contribution to shear behavior of unsaturated soil: modeling and application to a micromechanics model</title><author>Fukushima, Yo ; Higo, Yosuke ; Matsushima, Takashi ; Otake, Yu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a408t-7090d62eeb48497fd5f0616fe7a1d1c82f79c19f41c01035035ec6fcb8bf40583</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Anisotropy</topic><topic>Behavior</topic><topic>Bonding strength</topic><topic>Complex Fluids and Microfluidics</topic><topic>Computed tomography</topic><topic>Constitutive models</topic><topic>Distribution</topic><topic>Engineering</topic><topic>Fabrics</topic><topic>Foundations</topic><topic>Geoengineering</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Grain size</topic><topic>Granular materials</topic><topic>Granular media</topic><topic>Hydraulics</topic><topic>Laboratories</topic><topic>Liquid bridges</topic><topic>Mathematical models</topic><topic>Micromechanics</topic><topic>Moisture content</topic><topic>Orientation</topic><topic>Research Paper</topic><topic>Retention</topic><topic>Saturated soils</topic><topic>Saturation</topic><topic>Soft and Granular Matter</topic><topic>Soil</topic><topic>Soil investigations</topic><topic>Soil Science & Conservation</topic><topic>Soil suction</topic><topic>Soil water</topic><topic>Solid Mechanics</topic><topic>Stiffness</topic><topic>Tensors</topic><topic>Tomography</topic><topic>Unsaturated soils</topic><topic>Void ratio</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Fukushima, Yo</creatorcontrib><creatorcontrib>Higo, Yosuke</creatorcontrib><creatorcontrib>Matsushima, Takashi</creatorcontrib><creatorcontrib>Otake, Yu</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Acta geotechnica</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Fukushima, Yo</au><au>Higo, Yosuke</au><au>Matsushima, Takashi</au><au>Otake, Yu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Liquid bridge contribution to shear behavior of unsaturated soil: modeling and application to a micromechanics model</atitle><jtitle>Acta geotechnica</jtitle><stitle>Acta Geotech</stitle><date>2021-09-01</date><risdate>2021</risdate><volume>16</volume><issue>9</issue><spage>2693</spage><epage>2711</epage><pages>2693-2711</pages><issn>1861-1125</issn><eissn>1861-1133</eissn><abstract>Liquid bridges in unsaturated soils attach to grain contacts and contribute to strengthening microscopic bonding forces, which leads to macroscopic high strength and stiffness compared with dry or saturated soils. This study investigated microscopic liquid bridge behaviors in monodisperse granular media by combining X-ray micro-computed tomography and image analyses. Evaluating the anisotropy of grain contact orientation by fabric tensor revealed that fabric transitions under a triaxial process for both grain contacts and that with liquid bridges are equivalent, which indicates that the orientation of the liquid bridge contribution does not have unique anisotropy. The liquid bridge ratio (LBR) was defined as the ratio of the number of grain contacts with liquid bridges to the total number of grain contacts, representing the magnitude of the liquid bridge contribution. LBR distributions—the relationship of LBR to degree of saturation obtained by water retention tests for both dense and loose specimens—exhibited different peak positions depending on the void ratio and constant dispersion, which was then modeled using
β
distribution. A constitutive model on an experimental micromechanics basis for unsaturated soils was proposed by applying the liquid bridge contribution model as a combination of the LBR distribution model and the soil water characteristic curve model to a micromechanics model, in which spherical and monodisperse grains are assumed and the pendular saturation regime is focused. The proposed model qualitatively reproduced the macroscopic suction effect by describing the microscopic liquid bridge contribution.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s11440-021-01263-0</doi><tpages>19</tpages><orcidid>https://orcid.org/0000-0003-2818-2435</orcidid><orcidid>https://orcid.org/0000-0002-4879-540X</orcidid><orcidid>https://orcid.org/0000-0003-0694-1322</orcidid><orcidid>https://orcid.org/0000-0002-2553-7643</orcidid></addata></record> |
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subjects | Anisotropy Behavior Bonding strength Complex Fluids and Microfluidics Computed tomography Constitutive models Distribution Engineering Fabrics Foundations Geoengineering Geotechnical Engineering & Applied Earth Sciences Grain size Granular materials Granular media Hydraulics Laboratories Liquid bridges Mathematical models Micromechanics Moisture content Orientation Research Paper Retention Saturated soils Saturation Soft and Granular Matter Soil Soil investigations Soil Science & Conservation Soil suction Soil water Solid Mechanics Stiffness Tensors Tomography Unsaturated soils Void ratio |
title | Liquid bridge contribution to shear behavior of unsaturated soil: modeling and application to a micromechanics model |
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