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Redistribution of water and solute following infiltration from a surface drip source
Laboratory, observations of the redistribution of water and solute, following one-dimensional and three-dimensional constant flux infiltration, reveal distinctly different paterns of water and chemical transport. The geometry-induced enhancement of capillarity, over gravity in three dimensions is th...
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| Published in: | Water resources research 1991-08, Vol.27 (8), p.2091-2097 |
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| Main Authors: | , , |
| Format: | Article |
| Language: | English |
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| cited_by | cdi_FETCH-LOGICAL-c3596-2ba88dacdf40689bb75809ae7a41430cc08fe801efab02971c86bd4c7c4f30303 |
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| cites | cdi_FETCH-LOGICAL-c3596-2ba88dacdf40689bb75809ae7a41430cc08fe801efab02971c86bd4c7c4f30303 |
| container_end_page | 2097 |
| container_issue | 8 |
| container_start_page | 2091 |
| container_title | Water resources research |
| container_volume | 27 |
| creator | Clothier, Brent Sauer, Tom Scotter, Dave |
| description | Laboratory, observations of the redistribution of water and solute, following one-dimensional and three-dimensional constant flux infiltration, reveal distinctly different paterns of water and chemical transport. The geometry-induced enhancement of capillarity, over gravity in three dimensions is thought responsible for the rapid attainment during redistribution of a near-constant water content, some radial distance r around the dripper. This renders simple the prediction of the maximum radial extent of convective solute redistribution, r. Nevertheless, molecular diffusion about r is the dominant mode of solute transport during the weak convective redistribution in three dimensions. |
| doi_str_mv | 10.1029/91WR00938 |
| format | article |
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The geometry-induced enhancement of capillarity, over gravity in three dimensions is thought responsible for the rapid attainment during redistribution of a near-constant water content, some radial distance r around the dripper. This renders simple the prediction of the maximum radial extent of convective solute redistribution, r. Nevertheless, molecular diffusion about r is the dominant mode of solute transport during the weak convective redistribution in three dimensions.</description><identifier>ISSN: 0043-1397</identifier><identifier>EISSN: 1944-7973</identifier><identifier>DOI: 10.1029/91WR00938</identifier><language>eng</language><publisher>Blackwell Publishing Ltd</publisher><subject>infiltracion ; infiltration ; irrigation goutte a goutte ; mouvement de l' eau dans le sol ; movimiento del agua en el suelo ; procesos de transporte en el suelo ; riego por goteo ; sandy soils ; soil transport processes ; soil water movement ; sol sableux ; solute ; solutes ; soluto ; suelo arenoso ; textural soil types ; tipos texturales de suelos ; transport dans le sol ; trickle irrigation ; type de sol textural</subject><ispartof>Water resources research, 1991-08, Vol.27 (8), p.2091-2097</ispartof><rights>Copyright 1991 by the American Geophysical Union.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3596-2ba88dacdf40689bb75809ae7a41430cc08fe801efab02971c86bd4c7c4f30303</citedby><cites>FETCH-LOGICAL-c3596-2ba88dacdf40689bb75809ae7a41430cc08fe801efab02971c86bd4c7c4f30303</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F91WR00938$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F91WR00938$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1416,27924,27925,46049,46473</link.rule.ids></links><search><creatorcontrib>Clothier, Brent</creatorcontrib><creatorcontrib>Sauer, Tom</creatorcontrib><creatorcontrib>Scotter, Dave</creatorcontrib><creatorcontrib>Escola Superior de Agricultura Luiz de Queiroz, Piracicaba, SP (Brazil)</creatorcontrib><creatorcontrib>DSIR Fruit and Trees, Palmerston North, New Zealand</creatorcontrib><title>Redistribution of water and solute following infiltration from a surface drip source</title><title>Water resources research</title><addtitle>Water Resour. 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Res</addtitle><date>1991-08</date><risdate>1991</risdate><volume>27</volume><issue>8</issue><spage>2091</spage><epage>2097</epage><pages>2091-2097</pages><issn>0043-1397</issn><eissn>1944-7973</eissn><abstract>Laboratory, observations of the redistribution of water and solute, following one-dimensional and three-dimensional constant flux infiltration, reveal distinctly different paterns of water and chemical transport. The geometry-induced enhancement of capillarity, over gravity in three dimensions is thought responsible for the rapid attainment during redistribution of a near-constant water content, some radial distance r around the dripper. This renders simple the prediction of the maximum radial extent of convective solute redistribution, r. Nevertheless, molecular diffusion about r is the dominant mode of solute transport during the weak convective redistribution in three dimensions.</abstract><pub>Blackwell Publishing Ltd</pub><doi>10.1029/91WR00938</doi><tpages>7</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0043-1397 |
| ispartof | Water resources research, 1991-08, Vol.27 (8), p.2091-2097 |
| issn | 0043-1397 1944-7973 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_13719116 |
| source | Wiley Online Library Backfiles Complete |
| subjects | infiltracion infiltration irrigation goutte a goutte mouvement de l' eau dans le sol movimiento del agua en el suelo procesos de transporte en el suelo riego por goteo sandy soils soil transport processes soil water movement sol sableux solute solutes soluto suelo arenoso textural soil types tipos texturales de suelos transport dans le sol trickle irrigation type de sol textural |
| title | Redistribution of water and solute following infiltration from a surface drip source |
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