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WSP10994
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Last modified
1/26/2010 3:15:34 PM
Creation date
10/12/2006 4:39:06 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8210.470
Description
Pacific Southwest Interagency Committee
State
CO
Basin
Colorado Mainstem
Water Division
5
Date
3/1/1962
Author
PSIAC
Title
Stock Water Facilities Guide - March 1962
Water Supply Pro - Doc Type
Report/Study
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<br /> <br />001519 <br /> <br />LOSSES OF WATER <br /> <br />Evaporation <br /> <br />Evaporation constitutes one of the major losses of water frol;n <br />stock ponds. The drop in the level of stored water due to this cause is <br />equivalent to the annual evaporation less the precipitation on the water <br />surface, and the total evaporation loss in acre-feet from the pond can <br />readily be calculated by applying the net evaporation rate to the average <br />area of the water surface. The average annual evaporation in the Pacific <br />Southwest area, as measured in class A evaporation pan, and as deter- <br />mined from lake surface, has been compiled by the Weather Bureau as <br />previously noted. Experience has shown that because of the shallow <br />depths, evaporation from stock ponds may exceed that in most lakes and <br />at times it probably approaches that in the standard clas s A pan. Mea- <br />surements of evaporation losses from stock ponds by the Geological, <br />Survey (Langbein, 1951; Culler, 1961) suggested a coefficient of O. 85 <br />times pan evaporation. Generally the figure will probably fall somewhere <br />between 0.70 and 0.95. <br /> <br />Using a coefficient of O. 85, evaporation from stock ponds in the <br />Pacific Southwest area will vary from a minimum of about 42;inches in <br />the higher elevation northern areas to a maximum of about 85 inches in <br />the lower Gila and Colorado River basins in Arizona and parts of south- <br />eastern Nevada. The summer (May-October) evaporation ranges from <br />80 percent of the annual evaporation in the Green River Bas in, in parts of <br />the mountainous area of east-central California, (Weather Bureau, 1959) <br />and in the northern Utah and Nevada sections of the Great Basin, to 68 <br />percent in southern Arizona and 62 percent along the coast in southern <br />California. Thus, summer evaporation is highest in those areas where <br />grazing generally is limited to the summer season. Stock ponds should <br />be planned and des igned accordingly. In the southern latitudes, where <br />year-long grazing is practiced, the evaporation is more evenly distributed <br />although a major part again occurs in the summer season. <br /> <br />Reduc ing evaporat ion <br /> <br />Evaporation losses may be reduced by an appreciable amount <br />through proper design of the stock pond and possibly to some extent by <br />application of monomolecular films. An obvious and desirable design <br />criteria for reducing losses is a low ratio of pond surface area to volume. <br />Unfortunately, most stock pond sites do not permit much leeway in this <br />regard but in selecting sites the possibilities should be recognized and <br /> <br />29 <br /> <br />;'~i.~\*~ <br /> <br />,''',>- <br /> <br />,'~ '- ~"l: <br /> <br />-,." ...-.... <br /> <br />!~{~~~ <br /> <br />~./.::../} <br /> <br />~f~~l <br /> <br />'';'' <br /> <br />(1 ,_ <br />''''';.'' <br />
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