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REP24312
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Last modified
8/24/2016 11:56:20 PM
Creation date
11/27/2007 3:56:10 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Report
Doc Date
10/2/2000
Doc Name
PRE-MINING STREAM CHANNEL CONDITIONS ON DEEP CREEK
From
WRIGHT WATER ENGINEERS INC
To
MOUNTAIN COAL CO
Permit Index Doc Type
SUBSIDENCE REPORT
Media Type
D
Archive
No
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1 <br /> <br />lJ <br />1 <br />1 <br />1 <br />1 <br /> <br />1 <br /> <br />1 <br />1 <br /> <br />1 <br />1 <br /> <br /> <br />1 <br />Memorandum to Henry Bazbe, MCC <br />July 28, 2000 <br />Page 3 <br />assigned values the average velocity can be computed by use of Manning's Equation for <br />turbulent flow as follows: <br />v _ 1.486 R~S~ 1 <br />J 2 / <br />h / + <br />n <br />where: <br />v =velocity, ft/sec <br />Rh =hydraulic radius, approximated as the depth, = 1.0 ft <br />St =friction slope, approximated as the water surface slope, = 0.049 fr/fr <br />n = Manning's "n" roughness coefficient = 0.065 <br />Applying Manning's equation the velocity for the dominant dischazge is 5.1 fr/sec. With the <br />assumed hydraulics, the critical velocity for dominant discharge is 5.8 ft/sec, which provides <br />good support for subcritical flow with a 5.1 fUsec velocity. A summary tabulation of the channel <br />hydraulic characteristics for the Deep Creek study reach at dominant discharge are: <br />Discharge <br />cfs Width <br />ft Depth <br />ft Slope <br />ft/fr Velocity <br />ft/sec <br />55.6 9.0 1.0 0.049 5.1 <br />A test for possible predictive purposes was the application of the Leopold Equations for the <br />hydraulic characteristics. Leopold describes a stable channel configuration by the follo+ving <br />relationships: <br />w=aQh d=cQf v=kQm <br />(2) <br />where: +v is width. Q is discharge, d is depth, v is mean velocity, the letters b, f, m are <br />exponents, and a, c, k are coefficients. <br />In these three relationships, Q = w*d*v and, thus, the sum of the exponents is one. The most <br />common values for these exponents are b = 0.50, f = 0.40, and m = 0. ] 0. Coefficients used on <br />man}~ streams in the Colorado area are, a = 2.7, c = 0.14, and k = 2.5. Based on the dominant <br />discharge hydraulics, the coefficients for Deep Creek are, a = 1.5, c = 0.20, and k = 3.4. <br />SEDIMENT YIELD <br />An estimate was made of the average annual sediment load of Deep Creek through the study <br />reach by use of the methods described in the report by John G. Elliott, "Regionalizztion of Mean <br />Annual Suspended-Sediment Loads in Streams, Central, Northwestern and Southwestern <br />Colorado," a 1988 U.S. Geological Survey, Water-Resources Investigations Report 87-4193. A <br />Wright Water Engineers, Inc , 2490 W. 26°' Avenue, Ste. 100A, Denver, CO 60211 <br />7e1. 303/460-1700; Fax. 303/460-1020, e-mail:knvright~vrtightwater corn <br />1 <br />
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