Effect of wetting–drying–freezing–thawing cycles on the swelling behaviour of the Yanji mudstone
One of the most important characteristics of mudstones is their susceptibility to swelling upon absorption of water, which is influenced by climatic processes. This study investigated the swelling pressure and strain of the Yanji mudstone subjected to wetting–drying (W–D), freezing–thawing (F–T) and...
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description | One of the most important characteristics of mudstones is their susceptibility to swelling upon absorption of water, which is influenced by climatic processes. This study investigated the swelling pressure and strain of the Yanji mudstone subjected to wetting–drying (W–D), freezing–thawing (F–T) and wetting–drying–freezing–thawing (W–D–F–T) cycles. The swelling curves were analysed using a simulation of the logistic function, and the coefficient of initial swelling (
C
is
), coefficient of primary swelling (
C
ps
), coefficient of secondary swelling (
C
ss
), and ultimate swell were derived from the mathematical simulation. The results show that the cyclic treatments can significantly influence the swelling kinetics and ultimate swell. As the number of treatment cycles increases,
C
is
increases and then decreases due to the competition between the increasing permeability and the decreasing swelling potential induced by the propagation of cracks and large voids, while
C
ps
and
C
ss
decrease because of the compaction and contraction of the aggregates after cyclic treatments. The ultimate swelling pressure and ultimate swelling strain decrease with increasing treatment cycles and the relationships among these parameters were also established, allowing the ultimate swelling pressure and strain of the Yanji mudstone under the full range of seasonal variation to be predicted. |
doi_str_mv | 10.1007/s12665-019-8447-1 |
format | Article |
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C
is
), coefficient of primary swelling (
C
ps
), coefficient of secondary swelling (
C
ss
), and ultimate swell were derived from the mathematical simulation. The results show that the cyclic treatments can significantly influence the swelling kinetics and ultimate swell. As the number of treatment cycles increases,
C
is
increases and then decreases due to the competition between the increasing permeability and the decreasing swelling potential induced by the propagation of cracks and large voids, while
C
ps
and
C
ss
decrease because of the compaction and contraction of the aggregates after cyclic treatments. The ultimate swelling pressure and ultimate swelling strain decrease with increasing treatment cycles and the relationships among these parameters were also established, allowing the ultimate swelling pressure and strain of the Yanji mudstone under the full range of seasonal variation to be predicted.</description><identifier>ISSN: 1866-6280</identifier><identifier>EISSN: 1866-6299</identifier><identifier>DOI: 10.1007/s12665-019-8447-1</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Biogeosciences ; Coefficients ; Computer simulation ; Contraction ; Crack propagation ; Cracks ; Cycles ; Drying ; Earth and Environmental Science ; Earth science ; Earth Sciences ; Environmental Science and Engineering ; Freezing ; Geochemistry ; Geology ; Humidity ; Hydrology/Water Resources ; Investigations ; Kinetics ; Mathematical analysis ; Mathematical models ; Melting ; Mudstone ; Original Article ; Permeability ; Pressure ; Seasonal variation ; Seasonal variations ; Simulation ; Swell ; Swelling pressure ; Temperature ; Terrestrial Pollution ; Thawing ; Voids ; Wetting</subject><ispartof>Environmental earth sciences, 2019-08, Vol.78 (15), p.1-14, Article 435</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2019</rights><rights>Environmental Earth Sciences is a copyright of Springer, (2019). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-b67a4b153c7993af83e227746eddf9a77ec7ca9078d894e2b5ab8ef1fa946f883</citedby><cites>FETCH-LOGICAL-a339t-b67a4b153c7993af83e227746eddf9a77ec7ca9078d894e2b5ab8ef1fa946f883</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/s12665-019-8447-1$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12665-019-8447-1$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Zeng, Zhixiong</creatorcontrib><creatorcontrib>Kong, Lingwei</creatorcontrib><title>Effect of wetting–drying–freezing–thawing cycles on the swelling behaviour of the Yanji mudstone</title><title>Environmental earth sciences</title><addtitle>Environ Earth Sci</addtitle><description>One of the most important characteristics of mudstones is their susceptibility to swelling upon absorption of water, which is influenced by climatic processes. This study investigated the swelling pressure and strain of the Yanji mudstone subjected to wetting–drying (W–D), freezing–thawing (F–T) and wetting–drying–freezing–thawing (W–D–F–T) cycles. The swelling curves were analysed using a simulation of the logistic function, and the coefficient of initial swelling (
C
is
), coefficient of primary swelling (
C
ps
), coefficient of secondary swelling (
C
ss
), and ultimate swell were derived from the mathematical simulation. The results show that the cyclic treatments can significantly influence the swelling kinetics and ultimate swell. As the number of treatment cycles increases,
C
is
increases and then decreases due to the competition between the increasing permeability and the decreasing swelling potential induced by the propagation of cracks and large voids, while
C
ps
and
C
ss
decrease because of the compaction and contraction of the aggregates after cyclic treatments. The ultimate swelling pressure and ultimate swelling strain decrease with increasing treatment cycles and the relationships among these parameters were also established, allowing the ultimate swelling pressure and strain of the Yanji mudstone under the full range of seasonal variation to be predicted.</description><subject>Biogeosciences</subject><subject>Coefficients</subject><subject>Computer simulation</subject><subject>Contraction</subject><subject>Crack propagation</subject><subject>Cracks</subject><subject>Cycles</subject><subject>Drying</subject><subject>Earth and Environmental Science</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Environmental Science and Engineering</subject><subject>Freezing</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Humidity</subject><subject>Hydrology/Water Resources</subject><subject>Investigations</subject><subject>Kinetics</subject><subject>Mathematical analysis</subject><subject>Mathematical models</subject><subject>Melting</subject><subject>Mudstone</subject><subject>Original Article</subject><subject>Permeability</subject><subject>Pressure</subject><subject>Seasonal variation</subject><subject>Seasonal variations</subject><subject>Simulation</subject><subject>Swell</subject><subject>Swelling pressure</subject><subject>Temperature</subject><subject>Terrestrial Pollution</subject><subject>Thawing</subject><subject>Voids</subject><subject>Wetting</subject><issn>1866-6280</issn><issn>1866-6299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1UMtOwzAQtBBIVIUP4GaJc8CPxI8jqspDqsQFDpwsJ1m3qdKk2C5VOfEP_CFfgqMgOLGXHe3OzK4GoQtKrigh8jpQJkSREaozlecyo0doQpUQmWBaH_9iRU7ReQhrkopTromYIDd3DqqIe4f3EGPTLb8-Pmt_GIHzAO8jjCu7TwhXh6qFgPsOxxXgsIe2HcYlrOxb0-_84DRsXmy3bvBmV4fYd3CGTpxtA5z_9Cl6vp0_ze6zxePdw-xmkVnOdcxKIW1e0oJXUmtuneLAmJS5gLp22koJlaysJlLVSufAysKWChx1VufCKcWn6HL03fr-dQchmnX6qUsnDWOCUF6wgiQWHVmV70Pw4MzWNxvrD4YSMyRqxkRNStQMiRqaNGzUhMTtluD_nP8XfQOLL30_</recordid><startdate>20190801</startdate><enddate>20190801</enddate><creator>Zeng, Zhixiong</creator><creator>Kong, Lingwei</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope></search><sort><creationdate>20190801</creationdate><title>Effect of wetting–drying–freezing–thawing cycles on the swelling behaviour of the Yanji mudstone</title><author>Zeng, Zhixiong ; Kong, Lingwei</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a339t-b67a4b153c7993af83e227746eddf9a77ec7ca9078d894e2b5ab8ef1fa946f883</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Biogeosciences</topic><topic>Coefficients</topic><topic>Computer simulation</topic><topic>Contraction</topic><topic>Crack propagation</topic><topic>Cracks</topic><topic>Cycles</topic><topic>Drying</topic><topic>Earth and Environmental Science</topic><topic>Earth science</topic><topic>Earth Sciences</topic><topic>Environmental Science and Engineering</topic><topic>Freezing</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Humidity</topic><topic>Hydrology/Water Resources</topic><topic>Investigations</topic><topic>Kinetics</topic><topic>Mathematical analysis</topic><topic>Mathematical models</topic><topic>Melting</topic><topic>Mudstone</topic><topic>Original Article</topic><topic>Permeability</topic><topic>Pressure</topic><topic>Seasonal variation</topic><topic>Seasonal variations</topic><topic>Simulation</topic><topic>Swell</topic><topic>Swelling pressure</topic><topic>Temperature</topic><topic>Terrestrial Pollution</topic><topic>Thawing</topic><topic>Voids</topic><topic>Wetting</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zeng, Zhixiong</creatorcontrib><creatorcontrib>Kong, Lingwei</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</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>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science 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>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Environmental earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zeng, Zhixiong</au><au>Kong, Lingwei</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Effect of wetting–drying–freezing–thawing cycles on the swelling behaviour of the Yanji mudstone</atitle><jtitle>Environmental earth sciences</jtitle><stitle>Environ Earth Sci</stitle><date>2019-08-01</date><risdate>2019</risdate><volume>78</volume><issue>15</issue><spage>1</spage><epage>14</epage><pages>1-14</pages><artnum>435</artnum><issn>1866-6280</issn><eissn>1866-6299</eissn><abstract>One of the most important characteristics of mudstones is their susceptibility to swelling upon absorption of water, which is influenced by climatic processes. This study investigated the swelling pressure and strain of the Yanji mudstone subjected to wetting–drying (W–D), freezing–thawing (F–T) and wetting–drying–freezing–thawing (W–D–F–T) cycles. The swelling curves were analysed using a simulation of the logistic function, and the coefficient of initial swelling (
C
is
), coefficient of primary swelling (
C
ps
), coefficient of secondary swelling (
C
ss
), and ultimate swell were derived from the mathematical simulation. The results show that the cyclic treatments can significantly influence the swelling kinetics and ultimate swell. As the number of treatment cycles increases,
C
is
increases and then decreases due to the competition between the increasing permeability and the decreasing swelling potential induced by the propagation of cracks and large voids, while
C
ps
and
C
ss
decrease because of the compaction and contraction of the aggregates after cyclic treatments. The ultimate swelling pressure and ultimate swelling strain decrease with increasing treatment cycles and the relationships among these parameters were also established, allowing the ultimate swelling pressure and strain of the Yanji mudstone under the full range of seasonal variation to be predicted.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s12665-019-8447-1</doi><tpages>14</tpages></addata></record> |
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subjects | Biogeosciences Coefficients Computer simulation Contraction Crack propagation Cracks Cycles Drying Earth and Environmental Science Earth science Earth Sciences Environmental Science and Engineering Freezing Geochemistry Geology Humidity Hydrology/Water Resources Investigations Kinetics Mathematical analysis Mathematical models Melting Mudstone Original Article Permeability Pressure Seasonal variation Seasonal variations Simulation Swell Swelling pressure Temperature Terrestrial Pollution Thawing Voids Wetting |
title | Effect of wetting–drying–freezing–thawing cycles on the swelling behaviour of the Yanji mudstone |
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