Characterizing nonrigid aggregated soil-water medium using its shrinkage curve
The properties of the soil-water medium are presented in the literature independent of its internal organization and operation. The objective of this study is to develop and test a conceptual model that used a continuously measured shrinkage curve (SC) to describe the functional organization of the...
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| Veröffentlicht in: | Soil Science Society of America journal 2004-03, Vol.68 (2), p.359-370 |
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| creator | Bradeau, E Frangi, J.P Mohtar, R.H |
| description | The properties of the soil-water medium are presented in the literature independent of its internal organization and operation. The objective of this study is to develop and test a conceptual model that used a continuously measured shrinkage curve (SC) to describe the functional organization of the soil-water medium. In this model, two functional porosities (micro and macro) are delineated and quantified by the SC. In addition, the equilibrium for four functional water pools is represented and parameterized by the SC. A set of eleven parameters was found necessary to model the seven phases of the SC and to describe the corresponding soil hydrostructural changes. A method to accurately obtain the parameters of this model by a specific analysis of the continuously measured SC is demonstrated. Examples of continuously measured and modeled SCs according to the pedostructure model (PS) are presented and discussed. |
| doi_str_mv | 10.2136/sssaj2004.3590 |
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The objective of this study is to develop and test a conceptual model that used a continuously measured shrinkage curve (SC) to describe the functional organization of the soil-water medium. In this model, two functional porosities (micro and macro) are delineated and quantified by the SC. In addition, the equilibrium for four functional water pools is represented and parameterized by the SC. A set of eleven parameters was found necessary to model the seven phases of the SC and to describe the corresponding soil hydrostructural changes. A method to accurately obtain the parameters of this model by a specific analysis of the continuously measured SC is demonstrated. Examples of continuously measured and modeled SCs according to the pedostructure model (PS) are presented and discussed.</description><identifier>ISSN: 0361-5995</identifier><identifier>EISSN: 1435-0661</identifier><identifier>DOI: 10.2136/sssaj2004.3590</identifier><identifier>CODEN: SSSJD4</identifier><language>eng</language><publisher>Madison: Soil Science Society</publisher><subject>Agronomy. Soil science and plant productions ; Biological and medical sciences ; clay loam soils ; clay soils ; Earth sciences ; Earth, ocean, space ; equations ; Exact sciences and technology ; ferralitic soils ; Fundamental and applied biological sciences. Psychology ; loam soils ; mathematical models ; Moisture content ; particle size distribution ; Pellustert ; Physical properties ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; Plinthustalfs ; Plinthustox ; shrinkage ; soil physical properties ; soil pore system ; Soil properties ; Soil science ; Soil sciences ; soil structure ; Soil water ; soil water content ; Soils ; Surficial geology ; Torrifluvents ; Vertisols ; Water ; Water and solute dynamics ; Xerofluvents</subject><ispartof>Soil Science Society of America journal, 2004-03, Vol.68 (2), p.359-370</ispartof><rights>Soil Science Society of America</rights><rights>2004 INIST-CNRS</rights><rights>Copyright American Society of Agronomy Mar/Apr 2004</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c5010-864d48cc32bea423d008520e5c009ed09c9d9007b0b7886198861742504985883</citedby><cites>FETCH-LOGICAL-c5010-864d48cc32bea423d008520e5c009ed09c9d9007b0b7886198861742504985883</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.2136%2Fsssaj2004.3590$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.2136%2Fsssaj2004.3590$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,27901,27902,45550,45551</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=15545066$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Bradeau, E</creatorcontrib><creatorcontrib>Frangi, J.P</creatorcontrib><creatorcontrib>Mohtar, R.H</creatorcontrib><title>Characterizing nonrigid aggregated soil-water medium using its shrinkage curve</title><title>Soil Science Society of America journal</title><description>The properties of the soil-water medium are presented in the literature independent of its internal organization and operation. The objective of this study is to develop and test a conceptual model that used a continuously measured shrinkage curve (SC) to describe the functional organization of the soil-water medium. In this model, two functional porosities (micro and macro) are delineated and quantified by the SC. In addition, the equilibrium for four functional water pools is represented and parameterized by the SC. A set of eleven parameters was found necessary to model the seven phases of the SC and to describe the corresponding soil hydrostructural changes. A method to accurately obtain the parameters of this model by a specific analysis of the continuously measured SC is demonstrated. Examples of continuously measured and modeled SCs according to the pedostructure model (PS) are presented and discussed.</description><subject>Agronomy. Soil science and plant productions</subject><subject>Biological and medical sciences</subject><subject>clay loam soils</subject><subject>clay soils</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>equations</subject><subject>Exact sciences and technology</subject><subject>ferralitic soils</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>loam soils</subject><subject>mathematical models</subject><subject>Moisture content</subject><subject>particle size distribution</subject><subject>Pellustert</subject><subject>Physical properties</subject><subject>Physics, chemistry, biochemistry and biology of agricultural and forest soils</subject><subject>Plinthustalfs</subject><subject>Plinthustox</subject><subject>shrinkage</subject><subject>soil physical properties</subject><subject>soil pore system</subject><subject>Soil properties</subject><subject>Soil science</subject><subject>Soil sciences</subject><subject>soil structure</subject><subject>Soil water</subject><subject>soil water content</subject><subject>Soils</subject><subject>Surficial geology</subject><subject>Torrifluvents</subject><subject>Vertisols</subject><subject>Water</subject><subject>Water and solute dynamics</subject><subject>Xerofluvents</subject><issn>0361-5995</issn><issn>1435-0661</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqFkc1PGzEQxS0EEinlypVVpcJp0_Hnrg8coqiFVqg9hJwtx-ssDptd6skWpX89XhJRiUO5jC3r9-aN5xFyRmHMKFdfENGuGIAYc6nhgIyo4DIHpeghGQFXNJday2PyAXEFQBMDI_Jzem-jdRsfw9_Q1lnbtTHUocpsXUdf242vMuxCkz-la8zWvgr9OutxYMMGM7yPoX2wtc9cH__4j-RoaRv0p_vzhMy_fb2b3uS3v66_Tye3uZNAIS-VqETpHGcLbwXjFUApGXjpALSvQDtdpfGKBSyKslRUD6UQTILQpSxLfkIud30fY_e797gx64DON41tfdejKQSnjAqlEnnxX5IWTEvOIYGf3oCrro9t-oVhVEEBkg--4x3kYocY_dI8xrC2cWsomCEF85qCGVJIgs_7rhadbZbRti7gP5WUQsLLmFc77ik0fvtOVzOb_GCz2VDT097nfKdf2s7YOiaP-YwB5WmhaRVS8WdxUaHP</recordid><startdate>200403</startdate><enddate>200403</enddate><creator>Bradeau, E</creator><creator>Frangi, J.P</creator><creator>Mohtar, R.H</creator><general>Soil Science Society</general><general>Soil Science Society of America</general><general>American Society of Agronomy</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7T7</scope><scope>7X2</scope><scope>7XB</scope><scope>88I</scope><scope>8AF</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FH</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</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>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>HCIFZ</scope><scope>L6V</scope><scope>M0K</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P64</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>R05</scope><scope>S0X</scope><scope>SOI</scope><scope>7UA</scope><scope>KR7</scope></search><sort><creationdate>200403</creationdate><title>Characterizing nonrigid aggregated soil-water medium using its shrinkage curve</title><author>Bradeau, E ; Frangi, J.P ; Mohtar, R.H</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c5010-864d48cc32bea423d008520e5c009ed09c9d9007b0b7886198861742504985883</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2004</creationdate><topic>Agronomy. Soil science and plant productions</topic><topic>Biological and medical sciences</topic><topic>clay loam soils</topic><topic>clay soils</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>equations</topic><topic>Exact sciences and technology</topic><topic>ferralitic soils</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>loam soils</topic><topic>mathematical models</topic><topic>Moisture content</topic><topic>particle size distribution</topic><topic>Pellustert</topic><topic>Physical properties</topic><topic>Physics, chemistry, biochemistry and biology of agricultural and forest soils</topic><topic>Plinthustalfs</topic><topic>Plinthustox</topic><topic>shrinkage</topic><topic>soil physical properties</topic><topic>soil pore system</topic><topic>Soil properties</topic><topic>Soil science</topic><topic>Soil sciences</topic><topic>soil structure</topic><topic>Soil water</topic><topic>soil water content</topic><topic>Soils</topic><topic>Surficial geology</topic><topic>Torrifluvents</topic><topic>Vertisols</topic><topic>Water</topic><topic>Water and solute dynamics</topic><topic>Xerofluvents</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bradeau, E</creatorcontrib><creatorcontrib>Frangi, J.P</creatorcontrib><creatorcontrib>Mohtar, R.H</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Agricultural Science Collection</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>STEM Database</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</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>Agricultural & Environmental Science Collection</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>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Engineering Collection</collection><collection>Agricultural Science Database</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Biotechnology and BioEngineering Abstracts</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>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>University of Michigan</collection><collection>SIRS Editorial</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Civil Engineering Abstracts</collection><jtitle>Soil Science Society of America journal</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bradeau, E</au><au>Frangi, J.P</au><au>Mohtar, R.H</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Characterizing nonrigid aggregated soil-water medium using its shrinkage curve</atitle><jtitle>Soil Science Society of America journal</jtitle><date>2004-03</date><risdate>2004</risdate><volume>68</volume><issue>2</issue><spage>359</spage><epage>370</epage><pages>359-370</pages><issn>0361-5995</issn><eissn>1435-0661</eissn><coden>SSSJD4</coden><abstract>The properties of the soil-water medium are presented in the literature independent of its internal organization and operation. The objective of this study is to develop and test a conceptual model that used a continuously measured shrinkage curve (SC) to describe the functional organization of the soil-water medium. In this model, two functional porosities (micro and macro) are delineated and quantified by the SC. In addition, the equilibrium for four functional water pools is represented and parameterized by the SC. A set of eleven parameters was found necessary to model the seven phases of the SC and to describe the corresponding soil hydrostructural changes. A method to accurately obtain the parameters of this model by a specific analysis of the continuously measured SC is demonstrated. Examples of continuously measured and modeled SCs according to the pedostructure model (PS) are presented and discussed.</abstract><cop>Madison</cop><pub>Soil Science Society</pub><doi>10.2136/sssaj2004.3590</doi><tpages>12</tpages></addata></record> |
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| subjects | Agronomy. Soil science and plant productions Biological and medical sciences clay loam soils clay soils Earth sciences Earth, ocean, space equations Exact sciences and technology ferralitic soils Fundamental and applied biological sciences. Psychology loam soils mathematical models Moisture content particle size distribution Pellustert Physical properties Physics, chemistry, biochemistry and biology of agricultural and forest soils Plinthustalfs Plinthustox shrinkage soil physical properties soil pore system Soil properties Soil science Soil sciences soil structure Soil water soil water content Soils Surficial geology Torrifluvents Vertisols Water Water and solute dynamics Xerofluvents |
| title | Characterizing nonrigid aggregated soil-water medium using its shrinkage curve |
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