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WSPC110
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Last modified
1/26/2010 4:15:49 PM
Creation date
4/22/2007 10:20:26 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8230.400.21.B.5.B
Description
CO River Lit - Div 4 Water Court - Steamboat RICD - Water Court Filing - 26-a-2 Disclosures-Reports
State
CO
Basin
Colorado Mainstem
Water Division
5
Date
12/22/2003
Author
Various
Title
26-a-2 Disclosure Reports and Exhibits 2003-2004 - RE-Steamboat RICD - Case Number 03-CW-86 - 12-22-03 through 05-19-04
Water Supply Pro - Doc Type
Report/Study
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<br /> <br />n 0"27 ',6 . <br /> <br />. <br /> <br />~~...~.~,.. . ;'.~~:,., <br /> <br />.......". - .... <br /> <br />. <br /> <br />. <br /> <br />. .:=~ia_..... .';':-'..,,:~'o.:'O:....:l <br /> <br />. Figure 6. The U-structure at Charlie's Hole in Steamhoat shown at 1850 cfs. <br /> <br />Depth of flow <br /> <br />The specific dimensions of the V-structure are tailored by the designer to create the <br />desired in stream features. One of the most important variables that is controlled is the depth. <br />The depth is described by the Weir Equation, which can be expressed as, <br /> <br />Q = Cbh1.5 <br /> <br />(1) <br /> <br />where C is an empirically determined constant, b .is the river width as defuled in the analysis <br />section and h is the height ofthe flow. The weir equation can be used todetennine the <br />approximate depth of the flow in the specific channels. Note that this Equation is an <br />approximation and does not represent an exact relationship. The actual depth at the top of the <br />structure canvary due to a number of variables such as upstream current velocity, roughness of <br />the riverbed or variances in the structures geometry. . <br /> <br />The City of Steamboat Springs Boating Park was designedto function at a variety of <br />levels. During high flows the structures were designed separately such that each structure has <br />unique characteristics at differing flow rates. The depth and width of the structures at high flows <br />is shown in Table 1: . <br /> <br />-11- <br />
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