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FLOOD00770
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Last modified
1/29/2010 10:15:21 AM
Creation date
10/4/2006 9:27:38 PM
Metadata
Fields
Template:
Floodplain Documents
Designation Number
45
County
Adams
Arapahoe
Douglas
Community
Denver Metro Region
Stream Name
Big Dry Creek
Title
Major Drainageway Master Plan Big Dry Creek, Volume I
Date
6/1/1975
Designation Date
7/1/1975
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />Values for Manning's "n" were taken from t!lC "Design of Hoadside <br /> <br /> <br />Drainage Channels," !.!.zQr.:lUlic Desi~li-'.cri~)s _.No ~~.' May 1%5. (Table 2, <br /> <br /> <br />Manning Roughness Coefficients). For the initial hydraulics calculations <br /> <br /> <br />for the channel under existing conch tions, the following "n" values <br /> <br /> <br />were used. <br /> <br />From <br />Source <br />County Line Road <br />E. Arapahoe Road <br />Orchard Road <br /> <br />To <br />County Line Road <br />E. Arapahoe Road <br />Orchard Road <br />S. Platte ]1.iver <br /> <br />~Jja_~~_!2B_~~._~~~_'. <br /> <br />o.o~o <br />0.035 <br />O. cns <br />0.030 <br /> <br />The above values of "n" are composite values and therefore, no <br /> <br /> <br />attempt was made to vary "n" with water profile stage or cbannel con- <br /> <br /> <br />fi.guration. The single values of "n" are justified in this initi.al <br /> <br /> <br />study for a combination of hydrauliC reasons, the first bcing that for <br /> <br /> <br />the greater flood flows, the stream channel characteristics are such <br /> <br /> <br />that overbank flows appear to be a minor part of the floodway. The <br /> <br /> <br />maJn channel is well defined with l.imj~:(,d vegetative gro1Yth providing <br /> <br /> <br />little flow resi stance. The second reason is that in the greater f1 ooeL-; <br /> <br /> <br />tho depth of flow is greater and the channcl surface influence diminishe'i. <br /> <br /> <br />Finally, thc width of the flood plain from the inspection of the topo- <br /> <br /> <br />graphic maps indicates a rather steep channel indicative of a single <br /> <br /> <br />value roughness coefficient. <br /> <br /> <br />Cross sections \Vere taken along the basin channel where changes <br /> <br /> <br />occurred in slope, cross sectional area, channel roughness, locations <br /> <br /> <br />\Vhere levecs begin or end, and at hridges. Cross section data was <br /> <br />obtained by digitizing from mapping (scale: <br /> <br />I" = 100'. th'O foot contour <br /> <br />-11.1- <br />
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