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WSP10224
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Last modified
1/26/2010 2:57:51 PM
Creation date
10/12/2006 4:13:32 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8270.100
Description
Colorado River Basin Water Quality/Salinity -- Misc Water Quality
Basin
Colorado Mainstem
Water Division
5
Date
1/1/1993
Author
USDOI
Title
Quality of Water - Colorado River Basin - Progress Report No. 16 - January 1993
Water Supply Pro - Doc Type
Report/Study
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<br />10 Chap/ar S-Cau.as and Impacts of Salinity <br /> <br />'" <br />c.u <br />'"" <br />00 <br /> <br />Colorado River <br /> <br />IRRIGATED <br />FIELD <br /> <br />IRRIGATION <br />DITCHES <br /> <br /> <br />Figure 3,-Agricuitural sources of salinity, <br /> <br />Basin but was slow due to the difficulty of <br />diverting water from the Colorado River with its <br />widely fluctuating flows, Development of the <br />Gila area began in 1875 and the Palo Verde area <br />in 1879, Construction of the Boulder Canyon <br />Project in the 1930's, and other downstream <br />projects since that time, has provided for a <br />continued expansion of the irrigated area, In <br />1970, an additional 21,800 acres were irrigated <br />by private pumping either directly from the <br />Colorado River or from wells in the flood plain, <br />In 1980, nearly 400,000 acres were being <br />irrigated along the Colorado River mainstream; <br />total irrigated lands for the entire Lower Basin <br />were about 1.5 million acres, <br /> <br />Natural Sources of Salinity <br /> <br />Flow and quality records reveal that along <br />certain reaches ofthe Colorado River,large <br />increases in salt loads occur that cannot be <br />attributed to irrigation or other development- <br />related activities, These increases are mainly <br />due to natural diffuse sources and saline <br />springs, <br /> <br />Natural, diffuse sources of salt occur gradually <br />over long reaches of the river system, Salt <br />pickup occurs over large surface areas from <br />underlying soils, geologic formations, and from <br />stream channels and banks, Salt pickup is <br />difficult to identify, measure, or control; yet, <br />diffuse sources contribute the largest overall <br /> <br />share of the salts to the Colorado River, The <br />natural salt load for the Colorado River at Lees <br />Ferry, Arizona, was estimated to be about <br />5,3 million tons per year[2,3], Natural point <br />sources are saline springs where the <br />contribution of salt and water is easily <br />identified, issuing from single or concentrated <br />sources, The Glenwood-Dotsero Springs Unit <br />and the Paradox Valley Unit are two examples <br />of point source salinity control. <br /> <br />Municipal and Industrial Sources <br />of Salinity <br /> <br />Salts contributed to the Colorado River system <br />by M&I sources are generally minor, totaling <br />about 1 percent ofthe Basin salt load (or <br />3 percent of the salinity), Iorns[2] estimates <br />that M&I users increased salinity by about <br />100 tons per 1,000 people in the Basin, The <br />population reported for 1985 for the Upper <br />Basin was 645,000 people, At the present rate of <br />population increase, M&I sources will be <br />increasing salinity by approximately <br />133,000 tons per year by the year 2010, <br />However, most municipal wastes are relatively <br />low in salt concentration in comparison with <br />natural, industrial, and agricultural sources, <br />Complete elimination of such waste discharges <br />would be expensive when compared to other <br />salinity control methods, <br />
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