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Last modified
7/14/2009 5:02:36 PM
Creation date
5/20/2009 3:40:52 PM
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UCREFRP
UCREFRP Catalog Number
9568
Author
Resource Consultants Inc.
Title
Sediment Transport Studies of the Little Snake, Yampa, and Green River Systems.
USFW Year
1991.
USFW - Doc Type
Fort Collins, CO.
Copyright Material
NO
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<br />I <br />I <br /> <br />from telemetry data (T) of the stream flow. Total suspended concentration (CoI3) uses the results from <br />the DH-48 and DH-49 sampling. The percent silt/clay (Col 2) was established by wet sieving the <br />suspended sample. Wash load fractions (Col 4, 7) and suspended sand load fractions (Col 5,8) were <br />determined by the percent silt/clay. <br /> <br />I <br />I <br />I <br />I <br /> <br />A comparative plot of the measured wash load (Col 7) and suspended sand load (CoI8) at seven <br />sites is shown in Fig. 3.6. This plot indicates that in the Yampa River the wash load is greater than the <br />suspended sand load, while in the Little Snake River the opposite is true (suspended sand load greater than <br />wash load). <br /> <br />The Helley-Smith data, which may be considered indicative of bed load, is reported in Col 9, and a <br />corresponding concentration (CollO) computed for comparison. The ratio of the HeIley-Smith load to <br />total suspended sand (Colll) was found to vary widely due to the local characteristics of the flow at the <br />various sites. <br /> <br />I <br />I <br /> <br />Fig. 3.7 shows the estimated bed material load (CoI12). This plot demonstrates the recognized <br />importance of the lower Little Snake River as a sediment source area for sand sized material. During <br />higher flows the sediment discharge in the upper Little Snake (Dixon and Baggs) and in the Yampa River <br />above the Little Snake confluence (Juniper Hot Spring and the site immediately above the confluence) are <br />insignificant compared to the discharge in the lower Little Snake (Route 4, Highway 318 and Lily). <br /> <br />Helley Smith samples were dry sieved, providing the gradation curves shown in Fig. 3.8. The <br />material in transport for the various sites is very consistent over time. <br /> <br />I <br /> <br />Note that the Little Snake results reported above compare favorably with USGS data collected in <br />1983 at the Lily gage (Table 3.2). In both cases, sand load transport reaches values as high as 10,000 to <br />15,000 tons/day. The similarity of these results conftrms the data collection and analysis procedures. <br />28.000 <br /> <br />I <br /> <br /> 26.000 <br /> 24.000 <br />}:' <br /><{ 22.000 <br />0 <br />"- <br />lJl 20.000 <br />z <br />0 <br />t, 18.000 <br /> <br />Y AMPA RIVER <br /> <br />LITTLE SNAKE <br />RIVER <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />Ul,-.. <br />O.:g 16.000 <br />w ~ <br />() Ul 14.000 <br />a:: ::J <br /><{ 0 <br />is ~ 12.000 <br />lJl~ <br />o 10.000 <br /> <br />I <br /> <br />f- <br />Z 8.000 <br />w <br />:;? <br />0 6.000 <br />w <br />lJl <br /> 4.000 <br /> 2.00d <br /> 0.000 <br /> <br />HWY 3 <br /> <br />LILY G <br /> <br />I <br /> <br /> <br />1 2 3 <br /> <br />123 <br /> <br />123 <br /> <br />123 <br /> <br />123 <br /> <br />123 <br /> <br />1 2 3 <br /> <br />I <br />I <br />I <br /> <br />1989 FIELD SEASON <br />[ZZ] WASH LOAD IS:sJ SUS SAND LOAD <br />Figure 3.6 Comparison of 1989 measured wash load and suspended sand load. <br /> <br />3-7 <br />
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