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Last modified
7/14/2009 5:02:34 PM
Creation date
5/20/2009 10:53:21 AM
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UCREFRP
UCREFRP Catalog Number
8259
Author
Kircher, J. E.
Title
Sediment Transport and Source Areas of Sediment and Runoff, Big Sandy River Basin, Wyoming.
USFW Year
1982.
USFW - Doc Type
Water-Resources Investigations 81-72,
Copyright Material
NO
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aWAIA- r <br />REPORT DOCUMENTATION <br />I. KPORT No. <br />L <br />& Recipient's Accession No. <br />PAGE <br />4. Title and Subtitle & Report Date <br />SEDIMENT TRANSPORT AND SOURCE AREAS OF SEDIMENT AND RUNOFF, may 1982 <br />BIG SANDY RIVER BASIN, WYOMING & <br />7. Author(s) 8 Performing Organization Rept. No. <br /> USGS/WRI 81-72 <br />James E. Kircher <br />9. Performing Organization Nana and Address IQ Project/Task/Work Unit No. <br />U.S. Geological Survey <br />Water Resources Division 11. Contract(C) or Grant(G) No. <br />2120 Capitol Avenue (C) <br />Cheyenne, Wyoming <br />(G) <br />12. Sponsoring Organization Name and Address 13. Type of Report & Period Covered <br />U.S. Geological Survey Final <br />Water Resources Division <br />2120 Capitol Avenue 14. <br />Cheyenne, Wyoming <br />15. Supplementary Notes <br />I& Abstract (Limit: 200 words) <br />A study was conducted for the resolution of sediment source areas in the Big <br />Sandy River basin, southwestern Wyoming. Suspended-sediment and bedload data were <br />collected in order to determine total sediment transport at several locations within <br />the basin. <br />The bedload data were compared to the Einstein bedload function and total load data <br />were compared to the Colby method. The bedload comparison showed a higher estimation of <br />transport rates with Helley-Smith sampler measurements than with the Einstein bedload <br />function. The Colby method yielded higher transport rates at high flows and lower <br />transport rates at low flows than the measured total transport rate. <br />The Big Sandy Reservoir acts as a control in the basin. The area upstream of <br />the reservoir was interpreted separately from the area downstream for source-area <br />determination. In the arid plains upstream of the reservoir, the amount of <br />sediment transported increased 98 percent with an increase in runoff of only <br />1 percent. <br />17. Document Analysis a. Descriptors <br />Water resources, surface waters, erosion, runoff, channel erosion, bank erosion, <br />banks, beds, hydraulics, sedimentation, rivers, bedload, sediment load, aggradation, <br />degradation, regression analysis, total load <br />b. Identifiers/Open-Ended Terms <br />U.S. Geological Survey, Green River Basin, Big Sandy River basin, Green River Basin <br />project, Wyoming <br />e. COSATI Field/Group <br />l& Availability Statement 19. Security Class (This ReporO 21. No. of Pages <br />No restriction on distribution 20. Security Class (This Page) 22. Price <br />(See ANSI-Z39.18) See instructions on Reverse OPTIONAL POKIN Z/Z trim <br />(Formerly NTIS-35) <br />Department of commerce
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