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FLOOD08898
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Last modified
1/26/2010 10:07:03 AM
Creation date
10/5/2006 3:58:17 AM
Metadata
Fields
Template:
Floodplain Documents
County
Jefferson
Community
Golden, Lakewood
Stream Name
Lena Gulch
Basin
South Platte
Title
Lena Gulch Master Drainage Plan Volume 1
Date
6/1/1975
Prepared For
Golden, Lakewood, Wheatridge
Prepared By
UDFCD
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />111..11 <br /> <br />Another effect on peak flows Is channel ization, by which a clearer, <br />faster and more hydraul ically effecient channel Is cDnstructed <br />in or Dut of the existing channel al ignment. This suble prDcess which <br />has quite ofte~ caused unanticipated results In drainage improvements. <br />The basic concept is that Df an increased translatory wave effect which <br />cascades downstream and overtakes flO',N which was not combined befor'e. <br />As a result, the flow deepens and Increases in velocity, thereby increasing <br />the discharge rate. <br /> <br />This increases the flow 34 percent above the future developed conditions <br />for the discharge into Maple Grove Reservoir. This estimate is based on <br />a rough surface, hard-lined channel from the trailer CDurts In Reach 2 <br />to Clear Creek that has a slope approaching existing cDnditions. Below <br />Maple Grove the increase is not significant because of the storage/routing <br />effect of Maple Grove Reservoir. The flo^, increases sharply below Kipling <br />Street because the peak flDws from Basins 7, 8 and 9 cDmbine ",'ith Basin 10 <br />at a more coincident time. <br /> <br />On-Stream Storage. Part of any master plan is the investigation of effec- <br />tive on-stream storage and flow regulation measures. Several alternative <br />schemes were investigated to determine which measures would prove the most <br />beneficial. The most obvious alternate was the enlargement of Maple Grove <br />Reservoir by raising the existing dam crest to provide increased storage. <br /> <br />Unfortunately, this scheme only relieved the overtopping for the lOO-year <br />frequency event and did not significantly relieve flooding downstream. <br />The problem downstream is one of no significant outfall; that is, flow <br />from Basins 7, 8, and 9 would not be ,;ignlficantly altel'ed by a more con- <br />trolled discharge from Maple Grove Reservoir. The most significant and <br />efficient storage occurs with the first several feet of accumulation in <br />Maple Grove Reservoir. <br /> <br />An alternate scheme was an optimj.zat'ion of smal'ler detention reservoirs <br />along the gulch. The best apparent scheme was a larqer' pond below Basin <br />I and one or two other ponds below and possibly amonq the trailer courts. <br />This system of ponds results in a dec;'ease of 80 percent below the trailer <br />court, a decrease of 50 percent of the peak Inf'low to I~aple Grove Reservol r <br />and approximately the same sl ight decrease in f'low in 13asins 8 and 9 as <br />with enlarging Maper Grove Reservoir. This system requires about 100 acre" <br />feet in the upper pond and 150 acre-feet In the lower pond(s). The pecul i- <br />arlty here is that this reduced flow only si'lnificantly benefits the trailer <br />court areas and a few isolated residents. If the trai ler courts had been <br />designed with reasonable channel capacity, only a small detention pond <br />would be necessary for the debris collection and sedimentation basin pur" <br />poses. On-stream detention reservoirs also tend to fncrease major flood <br />hazard due to potential failure. Lar<ler ponds must be evaluated a<Jainst <br />increased hazards during large storm runoff periods. <br />
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