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dc.contributor.authorGay, Lloyd W.
dc.contributor.authorSammis, Theodore W.
dc.date.accessioned2013-09-04T21:49:36Z
dc.date.available2013-09-04T21:49:36Z
dc.date.issued1977-04-16
dc.identifier.issn0272-6106
dc.identifier.urihttp://hdl.handle.net/10150/300993
dc.descriptionFrom the Proceedings of the 1977 Meetings of the Arizona Section - American Water Resources Assn. and the Hydrology Section - Arizona Academy of Science - April 15-16, 1977, Las Vegas, Nevadaen_US
dc.description.abstractPhreatophyte transpiration on the Colorado River floodplain in western Arizona was evaluated under hot, dry, midsummer weather conditions. The simple transpiration model used related transpiration to the vapor pressure deficit of the air and to the area and the diffusion resistance of the transpiring foliage. There were no independent transpiration measurements for verification of the results. On a relative basis, however, mesquite (Prosopis sp.) transpired more rapidly per unit of leaf area than did saltcedar (Tamarix chimensis, Lour.).
dc.language.isoen_USen_US
dc.publisherArizona-Nevada Academy of Scienceen_US
dc.rightsCopyright ©, where appropriate, is held by the author.en_US
dc.subjectHydrology -- Arizona.en_US
dc.subjectWater resources development -- Arizona.en_US
dc.subjectHydrology -- Southwestern states.en_US
dc.subjectWater resources development -- Southwestern states.en_US
dc.titleEstimating Phreatophyte Transpirationen_US
dc.typetexten_US
dc.typeProceedingsen_US
dc.contributor.departmentSchool of Renewable Natural Resources, The University of Arizona, Tucsonen_US
dc.contributor.departmentDepartment of Agricultural Engineering, New Mexico State University, Las Crucesen_US
dc.identifier.journalHydrology and Water Resources in Arizona and the Southwesten_US
dc.description.collectioninformationThis article is part of the Hydrology and Water Resources in Arizona and the Southwest collections. Digital access to this material is made possible by the Arizona-Nevada Academy of Science and the University of Arizona Libraries. For more information about items in this collection, contact anashydrology@gmail.com.en_US
refterms.dateFOA2018-05-18T10:49:28Z
html.description.abstractPhreatophyte transpiration on the Colorado River floodplain in western Arizona was evaluated under hot, dry, midsummer weather conditions. The simple transpiration model used related transpiration to the vapor pressure deficit of the air and to the area and the diffusion resistance of the transpiring foliage. There were no independent transpiration measurements for verification of the results. On a relative basis, however, mesquite (Prosopis sp.) transpired more rapidly per unit of leaf area than did saltcedar (Tamarix chimensis, Lour.).


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