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WSP05690
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Last modified
1/26/2010 2:19:28 PM
Creation date
10/12/2006 1:11:42 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8407
Description
Platte River Basin - River Basin General Publications
State
CO
Basin
South Platte
Water Division
1
Date
1/1/1978
Author
Toups Corp
Title
Water Resources Investigation in the South Platte River Valley - Reach Number 2
Water Supply Pro - Doc Type
Report/Study
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<br /> ~t\~,,,,,,~ <br />I ~/ '. :.." .~, '1' , <br />I <br />I <br />I <br />'I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Losses associated with large channel flows are very great in the <br /> <br /> <br />reach of the South Platte River from Masters downstream to <br /> <br /> <br />aRproximately Orchard. Depth of flow at high water and at high <br /> <br /> <br />flood stage is such that flows which otherwise would remain in the <br /> <br /> <br />stream or recharge underlying alluvium actually spill into the <br /> <br />valley fill deposits of the ancient stream channel of the South <br /> <br /> <br />ptatte. This ancient channel meanders near the Wiggins and Bijou <br /> <br /> <br />No'. 2 Reservoir areas, and occasionally crosses the existing <br /> <br /> <br />r1ver at right angles. <br /> <br />Water budget analyses conducted for the South Platte have failed <br /> <br /> <br />to account for the tremendous losses incurred in channel losses <br /> <br /> <br />during high flow conditions. Magnitudes of unaccountable losses <br /> <br /> <br />ar~ substantial. For example, on May 9, 1969, inflow at Kersey <br /> <br /> <br />wak 18,000 cfs. Outflow at Balzac, considering travel time, was <br /> <br /> <br />111800 cfs. Diversions during this period amounted to only <br /> <br /> <br />380 cfs. The balance of river inflow, 5,820 cfs, represents a <br /> <br /> <br />10$s to the river. Hydrologic lnventories have failed to <br /> <br /> <br />determine the fate of losses; .they definitely do not serve to <br /> <br /> <br />retharge reaches of the South Platte downstream to the Nebraska <br /> <br /> <br />stAte line. It is conjectured that river outflow serves to <br /> <br /> <br />re9harge the ground water basins in the Wiggins area. Flows <br /> <br /> <br />typically don't return to the river because they are extracted and <br /> <br /> <br />diriJinished in quantity by well irrigation systems. <br /> <br />2-18 <br /> <br />~, ,- -'''''~ ;,. . - ,--;"" . <br /> <br /> <br /> <br />'i,f,. <br /> <br />,1; <br /> <br />'j. <br /> <br />- ~"- , . <br /> <br />
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