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<br />I) id':) 't <br /> <br />Chapter 1 <br /> <br />SUPPlemental Water <br /> <br />A. SUPPLEMENTAL WATER DEFINED <br /> <br />SUPPlemental Water IS additional water prOvided to <br />SUPply that which IS laCking, I,e.. needed or desired <br />Because Water is unevenly distributed In tIme and <br />space. Storage and transpol1atlon are the key elements <br />In any strategy to provide supplemental water In this <br />stUdy. SUpplemental Water IS consIdered to be water <br />which IS made available for use within a speCltlc area <br />by moving II tram one area to anOther and/or storing <br />It for use at a later time SUpplemental water can be <br />provided by constructing surface-waler reservoirs. by <br />adding to groundwater storage and by ImpOrting <br />groundwaler or surface water from anorher area' The <br />Objective of prOVIding Supplemental water IS 10 balance <br />the SUPPly from available SOurces for the variOUS uses. <br />The concept at SUPPlementing a local limited waler <br />SUPply IS as old as CIViliZation. The practices of adding <br />storage to enhance or augment waler SUPply from <br />another Source are equally old Knowledge and <br />technOlogy. however, Surely limited human habitatIon <br />to enVirons near surface-water Supplies from streams, <br /> <br /> <br />;' <br />'* <br />iy <br />" <br />. <br />j. <br />. --( <br /> <br />t-y' <br /> <br />lakes. and spnngs. Gourds and fabricated containers <br />permJlted excursions. not relocarlon of people. The <br />needs fa capture and SUpplement a given SUPPly <br />through storage undoubtedly led to the digging or <br />enlargement of depreSSions to Catch and hOld rain and <br />the construction of pnmitlve rock or earthen dams <br />across small streams. The firSt direct use of the grOund_ <br />water reServoir as a Sofe SOurce of wafer SUPply or as <br />a Supplement to a surface SUPPly prObably was trom <br />hana-dug shalJow holes In dry stream beds, TeChnOlogy <br />limited the Use of storage in either surface structures <br />or tram groundwater reservoirs unW hiStorical times. <br /> <br />B. SOURCES OF SUPPLEMENTAL WATER <br /> <br />ThiS report considers a vanety of SOurces and <br />methOds for SUPPlemenlrng Wafer Supplies. Those <br />whiCh were conSidered In the study period. but not in- <br />clUded in detail in this report, deserve some diSCUSSIon <br />here. These inClUde uSing the SOil profile as a waler <br />SOurce and a location for SUpplemental Storage through <br />conservation practices. reduction of evapotransPiration, <br />weather mOdificatIOn and reduction of lOsses from Sur- <br />face waler. <br />One SOurce of waler is that COntained Within the soil <br />profile. The soli zone. depth from the surface of two <br />to tlve feer, is a tYPe of storage reservoir. The SUPply <br />vanes depending UPon charactef/stlcs of the SOtl, time <br />and amount of preCipJtat1on, and other ClimatiC lactors <br />affecting evapOration or plant lranspiratlon. Various <br />conservation methOds have been used to Supplement <br />Or InCrease the SUPPly of Wafer In the soil profile. Land_ <br />Ireatment practices such as Contour PlOWing. terracing. <br />mulching. and ecofallow prOVide Supplemental water <br />by increasing fhe available soil mOiSture far plants. <br />These practices. along With land Shaping and leveling, <br />also COntribute to groundwater reCharge, Quantifying <br />the amounts of Supplemental water provided by these <br />methods IS dlffrcUl1. likeWise It IS difficult to measure <br /> <br />NOI conS'de,"" 10 Oe SUDPlemenlal Waf<" a'e nalu'al s"eam flow Ihal 's d,yen"" 10 npanan land and <br />groundwarer used Within one mile of the POint 01 Withdrawal. <br /> <br /> <br />,., <br /> <br />