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Last modified
1/25/2010 6:26:55 PM
Creation date
10/4/2006 11:38:36 PM
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Floodplain Documents
County
Denver
Basin
South Platte
Title
Drop Structures in the Denver Metropolitan Area
Date
12/1/1986
Prepared For
UDFDC
Prepared By
McLaughlin Water Engineers, Ltd.
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />The check structure is categorized here because the performance characteristics are <br />considered similar to the overflow jet and plunge pool concept, Illustrated by Figure <br />lll-l. <br /> <br />I <br />I <br />II <br />I <br />I <br />I <br /> <br />This rehabll1tatlve maIntenance project was designed for a flow rate of 500 cfs. It <br /> <br /> <br />has experienced flows on the order of 1100 cfs. Rock was originally desIgned with <br /> <br /> <br />a minimal safety factor In mInd; thus, one can see the displacement of rock, the <br /> <br /> <br />resulting scour hole, and the secondary drop downstream. The structure appears to <br /> <br /> <br />be stable but we suspect that future maintenance Will require either heavier rock to <br /> <br /> <br />be installed utilizing UDFCD guidelines for vertical loose rlprap drops, the Corps' <br /> <br /> <br />Derrick Stone Approach, or a grouted rock basin. <br /> <br />I <br /> <br />We note that trickle flow scour exists downstream of the drop and aggradation <br /> <br /> <br />occurs upstream of the drop. The observation here is that the grass-lined channels <br /> <br /> <br />will naturally agrade or degrade to form a stable trickle channel configuration, and <br /> <br /> <br />that trickle channels and corresponding invert elevations will rise to stay above the <br /> <br /> <br />effective crest elevation. (Minor not~hes do not prOVide sufficient capacIty to <br /> <br /> <br />prevent aggradation). The trickle channel should be stabilized between checks. <br /> <br />I <br />I <br />I <br /> <br />Case 31 - Spring Creek (trIbutary to little Dry Creek) downstream of County line <br /> <br /> <br />Road, Arapahoe County <br /> <br />These vertical rlprap drops were originally desIgned to comply wIth UDFCD interim <br /> <br /> <br />standards (Figure lll-2). Unfortunately, the rock prOVided was Rhyolite which has a <br /> <br /> <br />low speCIfIc gravity, it had to be grouted to be stabIlized. Thus, It was debatable <br /> <br /> <br />whether thiS drop was in a vertical rlprap or vertical hard basIn category. The <br /> <br /> <br />grouting was sub-standard In our OpiniOn, thus It was categorized here. Also, the <br /> <br /> <br />rock is deteriorating. It IS IrOniC that very large granIte rock was used for Ithe <br /> <br /> <br />retaining wall whIch had a speCific gravity of 2.7. <br /> <br />I' <br />I <br />I <br />I <br /> <br />The basins appear stable, however, the trickle and main channels upstream show <br /> <br /> <br />signs of aggradation. Also, the loose riprap is not well graded or placed properly <br /> <br /> <br />and problerTlll are likely. The design flow was 1160 cfs. <br /> <br />I <br />I <br /> <br />I <br /> <br />1lI-2 <br /> <br />I <br />I, <br />
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