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<br />~'-I <br /> <br />ANALYSIS OF SALT BALANCE <br /> <br />-.-:.~ <br />"' <br /> <br />:;?j <br /> <br />AND <br /> <br />SALT-BURDEN DATA ON THE RIO GRANDE <br /> <br />by <br /> <br />L. V. WILCOX <br /> <br />Assistant Director, Salinity Laboratory, Agricultural <br />Research Service, U. S. Department of Agriculture, <br />Riverside, California <br /> <br />.,-; <br /> <br />~:j <br /> <br />7'":iJ <br /> <br />:::j <br />, ~ <br />-'--1 <br /> <br />The Rio Grande is one of the more important <br />streams of the add West. Essentially all of the <br />water is diverted and most of it is used for irrigation. <br />Agriculture issuccessfulwhere drainage is adequate, <br />but where drainage is impaired, salinity conditions <br />restrict crop growth. These problems were recog- <br />. nized more than 20 fears ago when the present in- <br />vestigation was started. This investigation has <br />been a cooperative pwject between the United States <br />Section of the International Boundary and Water <br />Commission, the U. S. Bureau of Reclamation and the <br />U. S:Geological Swvey of the Department of Intedm, <br />and the U. S. Salinity Laboratory of the U. S. De- <br />partment of Agriculture. This paper summarizes the <br />findings of certain phases of the study to 1955, but <br />it is not a final report. <br /> <br />:;:1 <br /> <br />"J <br />~ <br /> <br />DEFINITION OF TERMS <br /> <br />Salt balance is defined as the relationship between <br />the quantity of dissolved salts carried to an area in <br />irrigation water and the quantity of dissolved salts <br />removed by the dminage water. Scofield' odginated <br />the term in the statement: "If the mass of the salt <br />input exceeds the mass of the salt output, the salt <br />balance is regarded as adverse, beca use this trend <br />is in the direction of the accumulation .of salt in the <br />area and such a trend is manifestly undesirable." <br />The results are expressed as quantities of salts or <br />in terms of percentages as "Output as percent of <br />Input" . <br />Salt burden is the quantity of salt passing a sta- <br />tion on a stream in a given period of time. It is <br />usually expressed as tons or ton-equivalents per <br />year. <br /> <br />J <br /> <br />METHODS AND ACCURACY <br /> <br />The basic data of this investigation include meas- <br /> <br />urements of stream flow and the chemical analyses <br /> <br />of related water samples. Discharge measurements <br /> <br />were made at seven gaging stations on the main stem <br /> <br />IS cofield, Carl 5., 1940. Salt Balance in Irril1ated Areas. <br />]oumal of Agr. Res. 61: 17~39. <br /> <br />of the Rio Grande and on several -irrigation and <br />drainage canals in the Rio Grande Project. The <br />measurements were made by engineers of the co- <br />operating agencies. "Provisional Records" were <br />furnished cunently and ahead of publication and are <br />the values used in this study. <br />The water samples were collected at the gaging <br />stations by the engineers who made the discharge <br />measurements. During the early years of the in- <br />vestigation, all of the water samples were analyzed <br />by the Salinity Laboratory. Since 1946, the samples <br />from Otowi Bridge and San Marcial have been ana~ <br />lyzed by the U. S. Geological Survey. The samples <br />analyzed by the Salinity Laboratory were composited <br />on the basis of the discharge of the stream. Those <br />analyzed by the Geological Survey were composited <br />on the basis of equal aliquots, but in both cases the <br />total volume of water represented by each sample is <br />known. The salt-burden and salt-balance conditions <br />have been calculated from these discharge measure- <br />ments and chemical analyses. a <br /> <br />The "Provisional Records" of discharge that <br />have been used may vary slightly from the final pub- <br />lished figures. For purposes of statistical analysis, <br />these values have been used in terms of Uthousands <br />of acre feet" which reduces the number of signifi- <br />cant figures to three or four. The chemical analyses <br />are reported to four significant figures. It is be- <br />lieved that final results should be accurate to three <br />significant figures. <br /> <br />RESULTS <br />SALT BURDEN <br /> <br />The locations of the seven gaging stations on the <br />Rio Grande are shown in Figure 1. The station at <br />Otowi 8ridge is above the irrigated area in New <br />Mexico. The San Luis Valley in Colorado is above <br />this point but there is no return flow of drainage <br />water. The Middle Rio Grande Valley Pwject .is <br /> <br />2Discharge measurements and some of the water analyses are <br />published in the Water Supply Papers of the U. S. Geological <br />Surveyor in the Water Bulletins of the International Boundary <br />and Water Commission. <br /> <br />39 <br /> <br />.-\. r.-' ,.. .r <br />t, .~I':;; L t.l i1 <br />