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<br /> <br />INTRODUCTION <br /> <br />:hure is one of a series prepared by the <br />ctors of the Southeastern Colorado Water <br />District, with the hope it, along with the <br />~lp to portray the absolute importance of <br />levelopment of the Arkansas Valley served <br />rvancy District. <br /> <br />tber=:; of the board are keenly aware of the <br />Ie from all walks of life are becoming in- <br />water problems in our world. As new <br />on is studied, water programs developed, <br />'o/'eels approved, additional exposure to <br />il be a daily process, It is the hope of the <br />,f the board that this very brief "Glossary <br />ms" might enable more people to take an <br />the fascinating programs involving water. <br />IS quoted here are but a small part of the <br />vocabulary" used by water authorities, but <br />ones most frequently used in public discus- <br /> <br />:>ch ures in' the series describe the Frying- <br />Proiect, Colorado State Statutes Govern- <br />ern 'Colorado Water Conservancy District, <br />nciples and Contract Between the United <br />ment and the District, and Excerpts from <br />er Publications. <br /> <br />Ir better understanding of you r most es- <br />ldity - WATER <br /> <br />OF COMMON WATER RESOURCE TERMS <br /> <br />A term used in measuring the volume of water, <br />lantity of water required to cover 1 acre 1 foot <br />,,560 cubic fe~t. <br />I geology, applied to rocks formed of windbome <br /> <br />A stream or river flowing into a larger river or <br />ributar)' system. <br />)N - (I) The geologic process by means of <br />l?arts of lhe surface of the earth are raised in <br />llt up by the deposition of material eroded from <br />md transporled thereto by water or wind. It is <br />. degradation. (2) The increase or rise of bed <br />pecific discharge of a channel al a given site. <br />Certain soluble salts, principally of sodillm, <br />Llesium, and calcium that occur in water or soils. <br />ry, :my substance having marked basic properties. <br />\-Vater or soils which contain a sufficient amount <br />nces present to raise the pH-value above 7.0 or <br />o the growth of crops. <br />Referring to silt, sand, gra~'e1 or similar detrital <br />h::ls been deposited by running water. <br />A devialion from a norm for which an explana- <br />lTent on the basis of available data. <br />- A conduit, usually of considerable size, used to <br />The conduit may consist of one or more of the <br /> <br />2 <br /> <br />followin~: Ca,l(al, pipe line, tunnel, siphon, or sD-called "in- <br />\'erted Siphon. <br />AQUIFER - A porous water-bearing geDlogic formation. <br />AREA, CATCHMENT - (1) The area tributary to a lake, <br />stream, Dr drain. (2) The intake Df an aquifer, and all areas t.hat <br />contribute surface walers to the intake area. (3) In tropical <br />island zones, a hard surfaced area, upon which rain is collected <br />and then conducted to a reservoir. <br />AREA, DEPRESSION, PUMPING. The surface area over- <br />lying the cone of influence or pressure-relief C01Ie. <br />AREA, DISCHARGE, GROUND-WATER - (I) An area <br />wherein ground water is disch::lrged through springs, wells, per- <br />colation, etc., evaporated from the soil, or transpired frum vege- <br />tation. (2) The crDss-sectional ::Irea of nDW of ground water at <br />any point below the surface. <br />AREA, INFLUENCE. The surface area surrounding a well, <br />or group of wens, during pumping, within which the water <br />table or other piezometric smface is lowered by withdrawal. of <br />the water. The area varies in extent with the rale and dural10n <br />Df pumping. <br />AREA, IRRIGABLE The pornon Df the arable area of an <br />irrigation development which is subject to Irngated farm use. <br />It excludes lands required fDr nonproduclive uses. <br />ARID - (l)A term applied tD regions where precipatation is 5? <br />deficient in quantity, or occurs at such times that agriculture IS <br />impractic::lble withDut irrigation. (2) In climatDlogy, a term <br />applied to climalcs which have insufficient rainfall to support <br />vegetatiDn. <br />ARROYO - A SHearn channel or gully usually rarher small with <br />steep banks, and dry much of the time. <br />ATMOMETER - An instrument for measuring evaporation; <br />also called an atmidometer or evaporimecer. Four main classes <br />of atmometers may be distinguished; (a) Large evaporation tanks <br />sunk in the ground or noating on protected Waters; (b) Small <br />open evaporation pans; (c) Porous porcelain bc.dies, mainly used <br />by plant phYSiologists in studying e....aporation from plants; <br />(d) AtmDmeters with wet paper surfaces. <br />ATMOSPHERE - The ouler part of the earth surrounding the <br />lithosphere and hydrosphere, and consisting predominantly of <br />ait. It contains DthCT matter such as water vapor and dust <br />particles. <br />AVULSION - (I) The act perfDrmed by a stream when il <br />suddenly breaks through its banks in an unexpeCled manner, <br />and fonus another channel or cuts off a lar~e quantity of land <br />from one Dwner and adds jt 10 anolher. (2) Rapid erosion Df <br />shoreland from waves during a stann. <br />BALANCE, SALT - The difference between the IOta I dissolved <br />sDlids brought to the land annually by the irrigation water and <br />the total solids carried away annually by the drainage water. <br />BARRAGE - A dam provided with a series of gates. erected <br />across a river tD regulate the water surface level and flDW up- <br />SlTeam. It is dislinguished from a weir in Ihal it is gated over <br />its enlire width and may not have a raised sill. <br />BASIN, DRAINAGE - (1) An area from which surface runDff <br />is carried aW::IY by ::I single drainage system. Also called catch- <br />m~t area, \Vatersh~~, .and draitlage. area (2) The largesr natural <br />dramage area subdlvlslon Df a contment. The United States has <br />been divided at one rime or another for ~'acious adminisrraril'e <br />purpDses into some 12 to 18 drainage basins. <br />BEDDING (GEOLOGY) - (I) The depos;'ion of sedimentary <br />material in layers, due 10 the SOIling actiDn of water from which <br />the material was deposited. Also called stratification arid in the <br />case of finer sediments, lamination. (2) (pipe laying) The earth <br /> <br />3 <br />