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Last modified
7/14/2009 5:02:30 PM
Creation date
5/20/2009 10:40:47 AM
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UCREFRP
UCREFRP Catalog Number
7641
Author
U.S. Department of the Interior.
Title
Quality of Water, Colorado River Basin.
USFW Year
1987.
USFW - Doc Type
Progress Report No. 13,
Copyright Material
NO
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<br />suggests the decline of salinity concentrations may have been in part caused <br />by the transition from a relatively drier period (1955-65) with an annual <br />virgin (undepleted) flow of 13.23 million acre-feet at Lees Ferry, to a <br />relatively wetter period (1965-75) with an annual virgin flow of 14.76 million <br />acre-feet. This is an increase in the flow of approximately 10 percent and may <br />be responsible for a portion of the decrease in the salinity concentration <br />observed at Imperial Dam. <br /> <br />The more recent period (1983-86) was even more extreme with some <br />flows well above those ever recorded. This was probably the major cause of <br />the near 200 mg/L drop in salinity over the last few years. A statistical <br />analysis of the CRSS projections for salinity indicates that salinity will <br />usually range between 635 and 1,035 mg/L, with an average of 820 mg/L under <br />the present level of development; however, about 5 percent of the time <br />salinity could vary outside this range, as it did in 1985 with a salinity of <br />607 mg/L. <br /> <br />2. Reservoir Effects <br /> <br />One of the most significant changes which has occurred to the <br />salinity of the Colorado River is due to the regulation of the natural flow of <br />the river basin. One study [3] shows that storage in Lake Powell reduced the <br />month to month variation from the mean salinity below Glen Canyon Dam from 299 <br />mg/L to 72 mg/L. This is readily apparent in a plot of the data, Figure V-3. <br /> <br />~ 1400 <br />~ 1200 <br />r 1000 <br />"'"' <br />.t' 800 <br />~ 600 <br />rtJ 400 <br />200 <br /> <br /> <br />. <br /> <br />. . . <br />. . . . <br />). .,. . <br />I,: · ... .-:........ <br />.. . ..., 1"-.. .,... <br />. . e. ... .... <br />.. .:--: . . ... ..... ... .. <br />;J'... " .. ......... ..... <br />. . : '"' . oS.....", · <br />~.. , .... · A. <br />. . . .,., <br />- ..... .,e I <br />.. .. ." <br />· .. . .. ~.Q4Aa"lLJ~ <br />· ... ,.. · .~';r"'~ · <br />.. .... ~. . . ~:.. .... . <br />.. ... . <br />e.. .. .... . <br />. . . ... , <br />, . \. ... <br /> <br />1940 <br /> <br />1950 <br /> <br />1960 <br /> <br />1970 <br /> <br />1980 <br /> <br />1990 <br /> <br />Year <br /> <br />Figure V-3. Monthly salinity below Lake Powell (1941-85). <br /> <br />The period of 1963-80 represents the most significant period of <br />reservoir storage in the history of water development on the Colorado River. <br />Storage in Flaming Gorge Reservoir, Lake Powell, and Lake Mead increased from <br />less than 20 mcillion acre-feet in 1963 to over 50 million acre-feet by 1980. <br />The spill of Glen Canyon Dam in 1980 ended the initial filling of the major <br />reservoirs on the Colorado River. Water which was being used to fill the <br />mainstem reservoirs is now being released. This has increased the flow to the <br /> <br />v-3 <br />
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