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Converting Reference Evapotranspiration Into Turf Water UseBrown, Paul, Kopec, Dave 02 1900 (has links)
5 pp. / Originally published 2000; revised 2014. / Introduction: Accurate estimates of turf water use are required to effectively manage a turf irrigation system. In Volume I of this series entitled “Basics of Evaporation and Evapotranspiration (ET),” we indicated that actual turf water use (ETt) is rarely measured in the real world. Instead, we use meteorological data and a mathematical model known as the Penman-Monteith Equation to estimate reference evapotranspiration (ETos) — the ET from a tall, cool-season grass that is supplied with adequate water. In the lower elevations of Arizona the ETos value would seem of limited value since we rarely grow turf that is equivalent to the reference surface. However, we get around this problem by adjusting the ETos value to account for differences in turf type, quality and stage of development. This document describes the procedures used to adjust ETos for use on managed turf surfaces in Arizona.
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L'évapotranspiration potentielle et le bilan de l'eau du bassin de la rivière Eaton, P.Q.Proulx, Robert January 1974 (has links)
No description available.
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Potential evapotranspiration in different climatic regions of GuyanaPersaud, Chander. January 1974 (has links)
No description available.
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A study of evapotranspiration over muskeg in a sub-arctic environment /Payant, Michel January 1976 (has links)
No description available.
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The microenvironment of a desert hackberry plant (Celtis pallida)Sammis, Theodore W. January 1974 (has links) (PDF)
Thesis (Ph. D. - Hydrology and Water Resources)--University of Arizona. / Includes bibliographical references.
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The influence of climatic, hydrologic, and soil factors on evapotranspiration rates of Tamarisk (Tamarix pentandra Pall.)Mace, Arnett C. January 1968 (has links) (PDF)
Thesis (Ph. D. - Watershed Management)--University of Arizona. / Includes bibliographical references (leaves 99-104).
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Penman-Monteith formulation for direct estimation of maize evapotranspiration in well watered conditions with full canopyFlores-Magdaleno, Héctor. January 1900 (has links)
Thesis (Ph.D.)--University of Nebraska-Lincoln, 2007. / Title from title screen (site viewed June 17, 2008). PDF text: 131 p. : ill. (some col.) ; 1 Mb. UMI publication number: AAT 3294284. Includes bibliographical references. Also available in microfilm and microfiche formats.
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L'évapotranspiration potentielle et le bilan de l'eau du bassin de la rivière Eaton, P.Q.Proulx, Robert January 1974 (has links)
No description available.
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A study of evapotranspiration over muskeg in a sub-arctic environment /Payant, Michel January 1976 (has links)
No description available.
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Evaluating the Influence of Vegetation on Evapotranspiration from Waste Rock Surfaces in the Elk Valley, British ColumbiaFraser, Stephanie 11 1900 (has links)
Coal mines operated by Teck Coal Ltd., in the Elk Valley, British Columbia, utilize the method of surface mining, resulting in large waste rock piles that affect water quality. In order to limit the influence that these waste rock piles have on water-rock interaction, alternate management strategies are being explored. In this study, the influence of vegetation on evapotranspiration is examined, as potential benefits exist in using vegetation to reduce the infiltration and percolation of water into waste rock. During the 2013 growing season, energy and water balance components were measured using the eddy covariance technique at a bare waste rock surface, a waste rock surface with a vegetated grass cover, and a waste rock surface with a reclaimed forest cover. In addition, other water balance components were measured, such as soil water storage and precipitation. The placement of vegetation atop the waste rock pile allowed for increased evapotranspiration compared to the bare waste rock surface. From 23 May 2013 to 30 September 2013, the reclaimed forest and reclaimed grasses site experienced 305 mm and 272 mm of ET, respectively, while the bare waste rock site had only 140 mm of ET. This increase in evapotranspiration suggests less deep percolation at vegetated sites, estimated as 148 mm, 172 mm and 246 mm for the grass, forest and bare rock sites respectively. ET at the vegetated sites was dominantly controlled by the net radiation, while the near surface moisture was the dominant control on ET at the bare rock site.
Results from this study suggest future reclamation projects should consider placing surface vegetation as a potential method to reduce deep percolation into waste rock piles. / Thesis / Master of Science (MSc)
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