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Last modified
1/26/2010 12:50:17 PM
Creation date
10/11/2006 11:43:14 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8407.400
Description
Platte River Basin - River Basin General Publications - Nebraska
State
NE
Basin
South Platte
Water Division
1
Date
8/1/1950
Author
BOR
Title
Braziel Dam and Reservoir - Nebraska
Water Supply Pro - Doc Type
Report/Study
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<br />001025 <br /> <br />. <br /> <br />RESERVOIR OPEJU,T IONS <br /> <br />Net Effcct <br /> <br />Brrczicl Rc scrvoir would store m:cter "hich !oi,~ht othernise be <br />w~sted on the Ft. Lrr~.ie Division of the North Pl~tte Project, By <br />n~king 1~nd5 to be served by the reservoir ne~rly independent of <br />furtLer relee.ses fron the Ft. L'.rm;de Ce.Ilnl during periods of "enk <br />denr,nd, it ;'Iould he.ve the net effect of incrensing the effective <br />crcp~city of tha Ft, 1o.ro,'.lie C~nCtl in thCtt wnter noW ce,rried for t~le <br />l~nds under Br~ziel Reser:oir could be used on other lands in the <br />Ftll LC\.r~.:r_1ie DivisionQ <br /> <br />Reser'7oir Sl..l!'fn.cl3 Losses <br /> <br />. <br /> <br />The free \V~tf)r surfo.ce evuporc,tion of Br"ziel Reservoir wc.S <br />Gstipmted ~ to~ be equf11 to tn.". t. d.t- the- St~te- ExperiJ:1entnl F"m, elevu- <br />tion 4,080, 6 !Jiles eust of Mitchell end 20 niles eaot of Br"ziel <br />Reservoir, The c.verage Experimente,l F"r!J evaporc.tion for ;.;1ril <br />through Septer,ber W'eS obtc,ined fron the 1946 Nebr'.skll ClinCttologico.l <br />D"tr: of the U. S. ;"oo.ther Buree.",; the October t!Jrough M,'rch evcporll- <br />tion wUs estimated to be 25 percent Qf unnuo.l evupor"tion, by <br />reference to studies of evnp0ration distribution trcnsnitted to ,,11 <br />field offices by the Regionnl Offie.e under dc,te of Jlme 10, 1947, <br />The roservoir surface loss in feet depth was calcule,ted as shOlm in <br />Tnble 12. Reservoir surf~ce loss in "cro-feet nus conputed by o.pply- <br />ing surfo.ue loss in foet of depth to the o.reu curve fl.S obtllined fron <br />the o.rec._cc.pc,ci ty curve o.nd the con tan"\; shown for the nonth in <br />Table 13. The Clrea-cupncity curve wus adjust8d to :".llon for 750 <br />c.cre-feet of sedir.lent expected to o.CClll;tub.to durir.g the first 50 yec.rs <br />of oporc.tion. <br /> <br />It is recor;nized the.t c.t ti:!18s nhen the res8rvoir is not full <br />there ,.;ould be Cl denuded o.reo. betueen tho \"later surfe'.ce '.nd tho <br />no.ximU",\ water surfo.ce elevation. There would be losses to bnnk <br />stor~r;a ut tipes when the water surface rises, und not ~ll of these 10ss~e <br />would be regllined as yie Id fron bunk storo.ge when t.he we.ter sClrfc.ce <br />dealinGs bec::,.usc of e'"T['.2or~:tion fror.1 tbD wot, denuded rlren. However, <br />in the p~st there has been n loss by consun}tive use Gf vegeta~ion <br />in t.his fringe C.reC, and it is estii:'!C.ted in these studies the.t such <br />past loss to cunsunptive use is cquivalent to the futuro loss which <br />'l,ilould result; from eva.por~,tion in t~1a denuded fringe .':\rer",s. <br /> <br />. <br /> <br />so <br />
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