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WSP07709
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Last modified
1/26/2010 2:28:35 PM
Creation date
10/12/2006 2:33:00 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8281.300
Description
Colorado River Studies and Investigations -- Colorado River Consumptive Uses and Losses Reports
Basin
Colorado Mainstem
Water Division
5
Date
1/1/1977
Title
Colorado River System Consumptive Uses and Losses Report -- 1971-1975
Water Supply Pro - Doc Type
Report/Study
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<br /> <br />amenable to direct measurement. Theoretical <br />and indirect methods of estimating con- <br />, ' <br />sumptive use m~st be relied upon in the <br />tributary areas. t'n the New Mexico portion of <br />the Gila River Basin, the annual consumptive <br />use of water is r~ported by the New Mexico I n- <br />terstate Stream Commission, pursuant to arti- <br />cle VII of the Match 9, 1964, decree of the <br />United States Supreme Court in Arizona v. <br />California, et a/. ' <br /> <br />Agriculture: About 85 percent of the con- <br />sumptive use in t~e tributary area to the Col- <br />orado River main~tream is for irrigated agricul- <br />ture. The annual (rrigated acreage and crops <br />grown within eachj reporting area were esti- <br />mated principally :from information in the <br />yearly State Agriclj/ture Statistics. Irrigated <br />pasture and some minor crops not reported by <br />the statistics were\estimated from informa- <br />tion in the 1969 O!lnsus of Agriculture, sup- <br />porting informatioil from framework studies, <br />and various other Iqcal reports including county, <br />farm-agent intervieWs. In essence, the <br />county data from t~e statistics were dis- <br />aggregated into the( reporting areas and sub- <br />areas for computatibnal purposes. The <br />Blaney-Criddle emp;irical formula was utilized <br />to compute the ann~al rate of crop consump- <br />tion use. The formula is based on the assump- <br />tion of a full water supply, among other <br />things, and results i~ a theoretical water re- <br />quirement rather th~n actual use. Seasonal <br />crop consumptive uS;e factors' "K" for the <br />lower elevation deserlt areas were selected from <br />Technical Bulletin 1~9 "Consumptive Use of <br />Water by Crops in Arizona," issued September <br />1965 by the University of Arizona and the <br />U.S. Department of 19riculture. In the <br />higher areas, season<\1 factors from the Soil <br />Conservation Service jTechnical Release No. <br />21 were utilized. Effective precipitation, that <br />amount of rainfall which satisfies a portion of <br />consumptive use, is a:ccounted for by criteria <br />developed for this area by Wayne D. Criddle, <br />former Utah State En4ineer. Among the <br />many variables affecti(1g the actual use of wa- <br />ter, the most importar1t is individual farm <br />water supply and its nianagement. There is no <br />adequate method to a<ljust computed annual <br /> <br />requirements to actual water use over broad <br />areas. <br />. Past studies of the incidental consumptive <br />use of water associated with irrigation (water <br />surfaces and vegetative areas on rights-of- <br />way for canals, laterals, drains, roads, etc.) <br />suggest that this use may be accounted for by <br />adding 10 to 20 percent of the computed crop <br />consumptive use. A factor of 15 percent is <br />used herein to represent this use. In the <br />heavily irrigated central Arizona area of the <br />Gila River Basin, in-transit water may some- <br />times be considered a depletion. In-transit <br />water is potential ground water recharge <br />which, due to declining water tables, intercep- <br />tion by impervious beds (perched water), <br />etc., is presently irrecoverable. Although this <br />water is not truly consumed, it is not avail- <br />able for use. This temporary loss of water has <br />not been included in this report because of the <br />lack of pertinent information to estimate its <br />present magnitude. <br /> <br />Evaporation from Reservoirs, Lakes, and <br />Stockponds: Adequate data are available at <br />most of the major reservoirs in the tributaries <br />to estimate annual lake evaporation. Monthly <br />net evaporation rates were derived from nearby <br />climatic stations recording pan evaporation <br />and precipitation. Stockpond evaporation was <br />taken directly from framework study support- <br />ing data which were prepared by the Soil <br />Conservation Service. I n addition to major re- <br />servoirs and stockponds, there are many <br />other reservoirs about which I ittle information <br />exists. For the most part, these reservoirs are <br />small and are used for a number of joint pur- <br />poses. Using available listings of these im- <br />poundments and other data. a total average <br />surface area and a representative evaporative <br />loss were estimated. No attempt was made to <br />vary these losses or those from stockponds on a <br />year-by-year basis. <br /> <br />Municipal and Industrial: The base for estimat- <br />ing municipal and industrial uses is the <br />urban and rural population within the report- <br />ing areas. Preparation of annual population <br />estimates was guided by the 1970 Census, <br />and various State and county statistical reviews <br />and reports which include popUlation esti- <br /> <br />~ <br /> <br />~ <br />-j <br />. <br />~ <br />,,' <br /> <br />j <br /> <br />,. <br /> <br />:..:: <br /> <br />~ <br /> <br />13 <br /> <br />~ <br />.~ <br />1 <br /> <br />I <br />
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