Experimental and modeling study of water-retention behavior of fine-grained soils with dual-porosity structures
Dual-porosity structures of fine-grained soils can noticeably affect their ability to retain water. This work jointly employs axis translation technique, filter paper method, and vapor equilibrium technique to study the soil–water retention curve (SWRC) over a wide suction range of Nanyang expansive...
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Veröffentlicht in: | Acta geotechnica 2022-08, Vol.17 (8), p.3245-3258 |
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description | Dual-porosity structures of fine-grained soils can noticeably affect their ability to retain water. This work jointly employs axis translation technique, filter paper method, and vapor equilibrium technique to study the soil–water retention curve (SWRC) over a wide suction range of Nanyang expansive soil characterized by double porosity. Mercury intrusion porosimetry tests are carried out to investigate the correlations between the aforementioned water-retention response and underlying pore structure characteristics. The test data show that dual-porosity distribution leads to bimodal SWRC. The change in void ratio mainly affects the median size of the inter-aggregate pores and consequently the portion of SWRC at low suction range. Based on these experimental observations, this work presents an SWRC equation for fine-grained soils with dual-porosity structures. Attracting water through capillary and adsorptive processes is explicitly distinguished. The capillary water is described by a relation that includes the characteristics of both inter- and intra-aggregate pore size distributions as parameters for representing bimodal characteristics. The adsorbed water is modeled by a relation that considers capillary condensation within intra-aggregate pores and allows for the decoupling between adsorptive water-retention mechanism and void ratio change. The latter feature is the foundation for the model to include the void ratio effect on SWRC in a way consistent with how it affects the pore structures of soils. By simulating test data in this work and in the literature, the proposed model is shown to be capable of representing the water-retention behavior of fine-grained soils with dual-porosity structures under different void ratios. To include the aforementioned key factors that influence the SWRC of fine-grained soils, seven parameters are required in the proposed model. This feature can reduce the practical applicability of the model. Future directions to enhance this aspect are discussed. |
doi_str_mv | 10.1007/s11440-022-01483-y |
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This work jointly employs axis translation technique, filter paper method, and vapor equilibrium technique to study the soil–water retention curve (SWRC) over a wide suction range of Nanyang expansive soil characterized by double porosity. Mercury intrusion porosimetry tests are carried out to investigate the correlations between the aforementioned water-retention response and underlying pore structure characteristics. The test data show that dual-porosity distribution leads to bimodal SWRC. The change in void ratio mainly affects the median size of the inter-aggregate pores and consequently the portion of SWRC at low suction range. Based on these experimental observations, this work presents an SWRC equation for fine-grained soils with dual-porosity structures. Attracting water through capillary and adsorptive processes is explicitly distinguished. The capillary water is described by a relation that includes the characteristics of both inter- and intra-aggregate pore size distributions as parameters for representing bimodal characteristics. The adsorbed water is modeled by a relation that considers capillary condensation within intra-aggregate pores and allows for the decoupling between adsorptive water-retention mechanism and void ratio change. The latter feature is the foundation for the model to include the void ratio effect on SWRC in a way consistent with how it affects the pore structures of soils. By simulating test data in this work and in the literature, the proposed model is shown to be capable of representing the water-retention behavior of fine-grained soils with dual-porosity structures under different void ratios. To include the aforementioned key factors that influence the SWRC of fine-grained soils, seven parameters are required in the proposed model. This feature can reduce the practical applicability of the model. Future directions to enhance this aspect are discussed.</description><identifier>ISSN: 1861-1125</identifier><identifier>EISSN: 1861-1133</identifier><identifier>DOI: 10.1007/s11440-022-01483-y</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Adsorptivity ; Aggregates ; Capillary water ; Complex Fluids and Microfluidics ; Decoupling ; Engineering ; Expansive soils ; Filter paper ; Fine-grained soils ; Foundations ; Geoengineering ; Geotechnical Engineering & Applied Earth Sciences ; Hydraulics ; Mathematical models ; Mercury ; Moisture content ; Parameters ; Pore size ; Pores ; Porosity ; Research Paper ; Retention ; Soft and Granular Matter ; Soil ; Soil porosity ; Soil Science & Conservation ; Soil structure ; Soil water ; Solid Mechanics ; Structures ; Void ratio ; Water ; Water purification</subject><ispartof>Acta geotechnica, 2022-08, Vol.17 (8), p.3245-3258</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022</rights><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a272t-95c03eb2d68fa927c972de12b261d6e6071647ecfffcc39864df504e96afef343</citedby><cites>FETCH-LOGICAL-a272t-95c03eb2d68fa927c972de12b261d6e6071647ecfffcc39864df504e96afef343</cites><orcidid>0000-0002-7071-1567</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/s11440-022-01483-y$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11440-022-01483-y$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27922,27923,41486,42555,51317</link.rule.ids></links><search><creatorcontrib>Qian, Jiangu</creatorcontrib><creatorcontrib>Lin, Zhiqiang</creatorcontrib><creatorcontrib>Shi, Zhenhao</creatorcontrib><title>Experimental and modeling study of water-retention behavior of fine-grained soils with dual-porosity structures</title><title>Acta geotechnica</title><addtitle>Acta Geotech</addtitle><description>Dual-porosity structures of fine-grained soils can noticeably affect their ability to retain water. This work jointly employs axis translation technique, filter paper method, and vapor equilibrium technique to study the soil–water retention curve (SWRC) over a wide suction range of Nanyang expansive soil characterized by double porosity. Mercury intrusion porosimetry tests are carried out to investigate the correlations between the aforementioned water-retention response and underlying pore structure characteristics. The test data show that dual-porosity distribution leads to bimodal SWRC. The change in void ratio mainly affects the median size of the inter-aggregate pores and consequently the portion of SWRC at low suction range. Based on these experimental observations, this work presents an SWRC equation for fine-grained soils with dual-porosity structures. Attracting water through capillary and adsorptive processes is explicitly distinguished. The capillary water is described by a relation that includes the characteristics of both inter- and intra-aggregate pore size distributions as parameters for representing bimodal characteristics. The adsorbed water is modeled by a relation that considers capillary condensation within intra-aggregate pores and allows for the decoupling between adsorptive water-retention mechanism and void ratio change. The latter feature is the foundation for the model to include the void ratio effect on SWRC in a way consistent with how it affects the pore structures of soils. By simulating test data in this work and in the literature, the proposed model is shown to be capable of representing the water-retention behavior of fine-grained soils with dual-porosity structures under different void ratios. To include the aforementioned key factors that influence the SWRC of fine-grained soils, seven parameters are required in the proposed model. This feature can reduce the practical applicability of the model. Future directions to enhance this aspect are discussed.</description><subject>Adsorptivity</subject><subject>Aggregates</subject><subject>Capillary water</subject><subject>Complex Fluids and Microfluidics</subject><subject>Decoupling</subject><subject>Engineering</subject><subject>Expansive soils</subject><subject>Filter paper</subject><subject>Fine-grained soils</subject><subject>Foundations</subject><subject>Geoengineering</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Hydraulics</subject><subject>Mathematical models</subject><subject>Mercury</subject><subject>Moisture content</subject><subject>Parameters</subject><subject>Pore size</subject><subject>Pores</subject><subject>Porosity</subject><subject>Research Paper</subject><subject>Retention</subject><subject>Soft and Granular Matter</subject><subject>Soil</subject><subject>Soil porosity</subject><subject>Soil Science & Conservation</subject><subject>Soil structure</subject><subject>Soil water</subject><subject>Solid Mechanics</subject><subject>Structures</subject><subject>Void ratio</subject><subject>Water</subject><subject>Water purification</subject><issn>1861-1125</issn><issn>1861-1133</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</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>eNp9kEtPwzAQhC0EEqXwBzhZ4mzwq05yRFV5SJW4wNly43WbKo2D7VDy73EpghunWWlnZlcfQteM3jJKi7vImJSUUM4JZbIUZDxBE1YqRhgT4vR35rNzdBHjllIluFQT5BefPYRmB10yLTadxTtvoW26NY5psCP2Du9NgkACpGxqfIdXsDEfjQ-HnWs6IOtgslgcfdNGvG_SBtvBtKT3wccmjbkqDHUaAsRLdOZMG-HqR6fo7WHxOn8iy5fH5_n9khhe8ESqWU0FrLhVpTMVL-qq4BYYX3HFrAJFC6ZkAbVzrq5FVSpp3YxKqJRx4IQUU3Rz7O2Dfx8gJr31Q-jySc1VJVhRCcGyix9ddX40BnC6zyxMGDWj-gBWH8HqDFZ_g9VjDoljKGZzt4bwV_1P6gsYuH7D</recordid><startdate>20220801</startdate><enddate>20220801</enddate><creator>Qian, Jiangu</creator><creator>Lin, Zhiqiang</creator><creator>Shi, Zhenhao</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/0000-0002-7071-1567</orcidid></search><sort><creationdate>20220801</creationdate><title>Experimental and modeling study of water-retention behavior of fine-grained soils with dual-porosity structures</title><author>Qian, Jiangu ; Lin, Zhiqiang ; Shi, Zhenhao</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a272t-95c03eb2d68fa927c972de12b261d6e6071647ecfffcc39864df504e96afef343</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Adsorptivity</topic><topic>Aggregates</topic><topic>Capillary water</topic><topic>Complex Fluids and Microfluidics</topic><topic>Decoupling</topic><topic>Engineering</topic><topic>Expansive soils</topic><topic>Filter paper</topic><topic>Fine-grained soils</topic><topic>Foundations</topic><topic>Geoengineering</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Hydraulics</topic><topic>Mathematical models</topic><topic>Mercury</topic><topic>Moisture content</topic><topic>Parameters</topic><topic>Pore size</topic><topic>Pores</topic><topic>Porosity</topic><topic>Research Paper</topic><topic>Retention</topic><topic>Soft and Granular Matter</topic><topic>Soil</topic><topic>Soil porosity</topic><topic>Soil Science & Conservation</topic><topic>Soil structure</topic><topic>Soil water</topic><topic>Solid Mechanics</topic><topic>Structures</topic><topic>Void ratio</topic><topic>Water</topic><topic>Water purification</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Qian, Jiangu</creatorcontrib><creatorcontrib>Lin, Zhiqiang</creatorcontrib><creatorcontrib>Shi, Zhenhao</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>Qian, Jiangu</au><au>Lin, Zhiqiang</au><au>Shi, Zhenhao</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Experimental and modeling study of water-retention behavior of fine-grained soils with dual-porosity structures</atitle><jtitle>Acta geotechnica</jtitle><stitle>Acta Geotech</stitle><date>2022-08-01</date><risdate>2022</risdate><volume>17</volume><issue>8</issue><spage>3245</spage><epage>3258</epage><pages>3245-3258</pages><issn>1861-1125</issn><eissn>1861-1133</eissn><abstract>Dual-porosity structures of fine-grained soils can noticeably affect their ability to retain water. This work jointly employs axis translation technique, filter paper method, and vapor equilibrium technique to study the soil–water retention curve (SWRC) over a wide suction range of Nanyang expansive soil characterized by double porosity. Mercury intrusion porosimetry tests are carried out to investigate the correlations between the aforementioned water-retention response and underlying pore structure characteristics. The test data show that dual-porosity distribution leads to bimodal SWRC. The change in void ratio mainly affects the median size of the inter-aggregate pores and consequently the portion of SWRC at low suction range. Based on these experimental observations, this work presents an SWRC equation for fine-grained soils with dual-porosity structures. Attracting water through capillary and adsorptive processes is explicitly distinguished. The capillary water is described by a relation that includes the characteristics of both inter- and intra-aggregate pore size distributions as parameters for representing bimodal characteristics. The adsorbed water is modeled by a relation that considers capillary condensation within intra-aggregate pores and allows for the decoupling between adsorptive water-retention mechanism and void ratio change. The latter feature is the foundation for the model to include the void ratio effect on SWRC in a way consistent with how it affects the pore structures of soils. By simulating test data in this work and in the literature, the proposed model is shown to be capable of representing the water-retention behavior of fine-grained soils with dual-porosity structures under different void ratios. To include the aforementioned key factors that influence the SWRC of fine-grained soils, seven parameters are required in the proposed model. This feature can reduce the practical applicability of the model. Future directions to enhance this aspect are discussed.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s11440-022-01483-y</doi><tpages>14</tpages><orcidid>https://orcid.org/0000-0002-7071-1567</orcidid></addata></record> |
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subjects | Adsorptivity Aggregates Capillary water Complex Fluids and Microfluidics Decoupling Engineering Expansive soils Filter paper Fine-grained soils Foundations Geoengineering Geotechnical Engineering & Applied Earth Sciences Hydraulics Mathematical models Mercury Moisture content Parameters Pore size Pores Porosity Research Paper Retention Soft and Granular Matter Soil Soil porosity Soil Science & Conservation Soil structure Soil water Solid Mechanics Structures Void ratio Water Water purification |
title | Experimental and modeling study of water-retention behavior of fine-grained soils with dual-porosity structures |
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