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WSP04560
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Last modified
1/26/2010 12:56:04 PM
Creation date
10/12/2006 12:25:59 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8271.300
Description
Colorado River Basin Salinity Control Program - General Information and Publications - Reports
Basin
Colorado Mainstem
Water Division
5
Date
2/9/1994
Author
John Hedlund
Title
Salt Primer - Water and Salt Budgets
Water Supply Pro - Doc Type
Report/Study
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<br />" <br /> <br />5 <br /> <br />COLORADO RIVER SETTING <br /> <br />~ Much of the irrigated land in the west has been irrigated only 50 <br />(D to 100 years. This is a relatively short time period when <br />~. compared to the Nile Valley and parts of India and China where <br />~ irrigation has been going on for over 4000 years. Concentration <br />of salinity in the subsurface return flow remains essentially <br />constant as the geo-hydro-chemical interaction of water passing <br />through the underlying aquifer has reached a steady state <br />condition. The salinity concentration can be a few hundred mg/L <br />to several thousand mg/L depending on the characteristics of the <br />aquifer. Soil lab analysis of saline soils(SCS, ) indicate <br />concentrations of up to 35 , gypsum and lime in the soil profile <br />after 50 to 100 years of irrigation. Soluble salts are leached <br />quickly from the soil profile but the less soluble salts are <br />leached slowly. The less soluble salts precipitate out first <br />from irrigation or soil water, and gypsum and lime are what is <br />usually visible on irrigated fields when they appear white. <br /> <br />Highly soluble salts are leached out of the root zone soil in the <br />first two or three years of initial reclamation when adequate <br />drainage is provided. The supply of less soluble salt in the <br />underlying aquifers is essentially unlimited for the next several <br />thousand years, where irrigation is over ancient lake and <br />seabeds. "In these cases, reducing the drainage water may be <br />expected to reduce the salt emissions proportionately. II (Tanji <br />1990 p.477)." <br /> <br />Therefore, the salt pickup from irrigation is directly <br />proportional to amount of deep percolating return flow. <br />Irrigation water management by the farmer is key to how much salt <br />is added to downstream streamflow. In several drainages of the <br />Colorado River, applied irrigation water carries less than 0.5 <br />ton of salt per acre foot(100 to 400 mg/L) and drainage return <br />flows can carry about 5 tons of salt in each acre-foot(3000 to <br />4000 mgfL). The objective of the salinity control program is to <br />reduce the salt pickup by irrigation return flow by one and a <br />half million tons per year or 30 percent. <br /> <br />The beautiful and rugged Colorado River provides water for life <br />to over 18 million people. However, due to heavy withdrawals, the <br />River stopped flowing to the Gulf of California in 1964. Salts <br />are concentrated by irrigation consumptive use and exports from <br />the basin in the upper reaches. The Republic of Mexico receives <br />the last 10% of the flow of the river with severe salinity <br />pollution. In 1973 the U.S. agreed with Mexico to reduce <br />salinity. This led to passage of The Colorado River Basin <br />salinity Control Act of 1974, Public Law 93-320, without a <br />dissenting vote in Congress. The Act illustrates the pUblic's <br />awakening to the significance of off-site effects of irrigated <br />agriculture. Water quality standards for salinity have been set <br />by the states on the Colorado River to reduce present and future <br />downstream salinity damages and to meet the requirements of the <br />Clean Water Act, PL 92-500. <br />
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