Hydromechanical behavior of unsaturated soil with different initial densities over a wide suction range
Many civil engineering projects are related to hydromechanical behavior of unsaturated soils over a wide suction range, which was investigated by imposing suctions on clayey silt specimens using the axis translation technique and the vapor equilibrium technique with saturated salt solution in this p...
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Veröffentlicht in: | Acta geotechnica 2019-04, Vol.14 (2), p.417-428 |
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description | Many civil engineering projects are related to hydromechanical behavior of unsaturated soils over a wide suction range, which was investigated by imposing suctions on clayey silt specimens using the axis translation technique and the vapor equilibrium technique with saturated salt solution in this paper. Firstly, the effect of void ratio or density on the water retention behavior was discussed based on the measured data. The test data indicate that shear tests under constant water content can be considered as those under constant suction in high suction range. Secondly, the mercury intrusion porosimetry tests were also performed to observe the pore-size distribution of compacted specimens with different void ratios. The experimental results show that the inter-aggregate pores of compacted specimens decrease with increasing the initial void ratio, but the intra-aggregate pores remain unaffected, which can explain the water retention behavior of compacted specimens with different initial void ratios over a wide suction range. Finally, for triaxial shear tests, the shear strength increases with increasing the suction until a maximum strength is reached at a specific suction value. When the suction is higher than the specific suction value, the tendency of strength change depends on the density in high suction range. |
doi_str_mv | 10.1007/s11440-018-0662-5 |
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Firstly, the effect of void ratio or density on the water retention behavior was discussed based on the measured data. The test data indicate that shear tests under constant water content can be considered as those under constant suction in high suction range. Secondly, the mercury intrusion porosimetry tests were also performed to observe the pore-size distribution of compacted specimens with different void ratios. The experimental results show that the inter-aggregate pores of compacted specimens decrease with increasing the initial void ratio, but the intra-aggregate pores remain unaffected, which can explain the water retention behavior of compacted specimens with different initial void ratios over a wide suction range. Finally, for triaxial shear tests, the shear strength increases with increasing the suction until a maximum strength is reached at a specific suction value. When the suction is higher than the specific suction value, the tendency of strength change depends on the density in high suction range.</description><identifier>ISSN: 1861-1125</identifier><identifier>EISSN: 1861-1133</identifier><identifier>DOI: 10.1007/s11440-018-0662-5</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Aggregates ; Civil engineering ; Complex Fluids and Microfluidics ; Engineering ; Foundations ; Geoengineering ; Geotechnical Engineering & Applied Earth Sciences ; Hydraulics ; Intrusion ; Mercury ; Moisture content ; Pores ; Porosity ; Research Paper ; Retention ; Shear strength ; Shear tests ; Silt ; Size distribution ; Soft and Granular Matter ; Soil ; Soil compaction ; Soil investigations ; Soil Science & Conservation ; Soil suction ; Solid Mechanics ; Tests ; Unsaturated soils ; Void ratio ; Water content</subject><ispartof>Acta geotechnica, 2019-04, Vol.14 (2), p.417-428</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2018</rights><rights>Acta Geotechnica is a copyright of Springer, (2018). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a382t-7e351d34d448e802c07711483703a9f30d77062cf6d6c62a7895f8932e8f7d193</citedby><cites>FETCH-LOGICAL-a382t-7e351d34d448e802c07711483703a9f30d77062cf6d6c62a7895f8932e8f7d193</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11440-018-0662-5$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11440-018-0662-5$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids></links><search><creatorcontrib>Gao, You</creatorcontrib><creatorcontrib>Sun, De’an</creatorcontrib><creatorcontrib>Zhu, Zancheng</creatorcontrib><creatorcontrib>Xu, Yongfu</creatorcontrib><title>Hydromechanical behavior of unsaturated soil with different initial densities over a wide suction range</title><title>Acta geotechnica</title><addtitle>Acta Geotech</addtitle><description>Many civil engineering projects are related to hydromechanical behavior of unsaturated soils over a wide suction range, which was investigated by imposing suctions on clayey silt specimens using the axis translation technique and the vapor equilibrium technique with saturated salt solution in this paper. Firstly, the effect of void ratio or density on the water retention behavior was discussed based on the measured data. The test data indicate that shear tests under constant water content can be considered as those under constant suction in high suction range. Secondly, the mercury intrusion porosimetry tests were also performed to observe the pore-size distribution of compacted specimens with different void ratios. The experimental results show that the inter-aggregate pores of compacted specimens decrease with increasing the initial void ratio, but the intra-aggregate pores remain unaffected, which can explain the water retention behavior of compacted specimens with different initial void ratios over a wide suction range. Finally, for triaxial shear tests, the shear strength increases with increasing the suction until a maximum strength is reached at a specific suction value. When the suction is higher than the specific suction value, the tendency of strength change depends on the density in high suction range.</description><subject>Aggregates</subject><subject>Civil engineering</subject><subject>Complex Fluids and Microfluidics</subject><subject>Engineering</subject><subject>Foundations</subject><subject>Geoengineering</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Hydraulics</subject><subject>Intrusion</subject><subject>Mercury</subject><subject>Moisture content</subject><subject>Pores</subject><subject>Porosity</subject><subject>Research Paper</subject><subject>Retention</subject><subject>Shear strength</subject><subject>Shear tests</subject><subject>Silt</subject><subject>Size distribution</subject><subject>Soft and Granular Matter</subject><subject>Soil</subject><subject>Soil compaction</subject><subject>Soil investigations</subject><subject>Soil Science & Conservation</subject><subject>Soil suction</subject><subject>Solid Mechanics</subject><subject>Tests</subject><subject>Unsaturated soils</subject><subject>Void ratio</subject><subject>Water content</subject><issn>1861-1125</issn><issn>1861-1133</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</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>eNp1kE9LAzEUxIMoWKsfwFvA82r-7CbZoxS1guBFzyFuXtqUNqlJttJvb0pFT57eHOY3jxmErim5pYTIu0xp25KGUNUQIVjTnaAJVYI2lHJ--qtZd44ucl4RIjhrxQQt5nub4gaGpQl-MGv8AUuz8zHh6PAYsiljMgUsztGv8ZcvS2y9c5AgFOyDL74yFkKuCjKOO0jYVJ8FnMeh-BhwMmEBl-jMmXWGq587Re-PD2-zefPy-vQ8u39pDFesNBJ4Ry1vbdsqUIQNRMraTHFJuOkdJ1ZKItjghBWDYEaqvnOq5wyUk5b2fIpujrnbFD9HyEWv4phCfakZ4Uxw1XWyuujRNaSYcwKnt8lvTNprSvRhT33cU9c99WFP3VWGHZlcvbVR-kv-H_oGS9F4UA</recordid><startdate>20190401</startdate><enddate>20190401</enddate><creator>Gao, You</creator><creator>Sun, De’an</creator><creator>Zhu, Zancheng</creator><creator>Xu, Yongfu</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></search><sort><creationdate>20190401</creationdate><title>Hydromechanical behavior of unsaturated soil with different initial densities over a wide suction range</title><author>Gao, You ; 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Firstly, the effect of void ratio or density on the water retention behavior was discussed based on the measured data. The test data indicate that shear tests under constant water content can be considered as those under constant suction in high suction range. Secondly, the mercury intrusion porosimetry tests were also performed to observe the pore-size distribution of compacted specimens with different void ratios. The experimental results show that the inter-aggregate pores of compacted specimens decrease with increasing the initial void ratio, but the intra-aggregate pores remain unaffected, which can explain the water retention behavior of compacted specimens with different initial void ratios over a wide suction range. Finally, for triaxial shear tests, the shear strength increases with increasing the suction until a maximum strength is reached at a specific suction value. When the suction is higher than the specific suction value, the tendency of strength change depends on the density in high suction range.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s11440-018-0662-5</doi><tpages>12</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Aggregates Civil engineering Complex Fluids and Microfluidics Engineering Foundations Geoengineering Geotechnical Engineering & Applied Earth Sciences Hydraulics Intrusion Mercury Moisture content Pores Porosity Research Paper Retention Shear strength Shear tests Silt Size distribution Soft and Granular Matter Soil Soil compaction Soil investigations Soil Science & Conservation Soil suction Solid Mechanics Tests Unsaturated soils Void ratio Water content |
title | Hydromechanical behavior of unsaturated soil with different initial densities over a wide suction range |
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