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Last modified
7/14/2009 5:02:29 PM
Creation date
5/20/2009 10:12:26 AM
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UCREFRP
UCREFRP Catalog Number
7075
Author
Butler, M.
Title
Minimum Streamflow Hydrographs and Sediment Transport in the Yampa River Canyon Reaches
USFW Year
1988.
USFW - Doc Type
Draft.
Copyright Material
NO
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<br />PURPOSE OF TOTAL SEDIMENT TRANSPORT BUDGET <br />A FORTRAN program was developed for the Deerlodge Park to Mathers Hole reach of <br />the Yampa River. The purposes of the program are to: <br />1) Extend the analysis preformed by Elliott, focusing on the seasonal movement <br />of sediment in the Deerlodge Park-Mathers Hole reach, in addition to the <br />Deerlodge Park area. <br />12) Investigate changes in total load transport instead of suspended load. Bed <br />load rating curves may also be substituted where appropriate. <br />3) To help in evaluating specific water development projects and their impacts <br />upon total sediment transport through the reach and to the Green River. <br />4) Develop mean monthly hydrographs to maintain sediment transport through the <br />Deerlodge Park - Mathers Hole reach, given mean monthly project flow data. <br />SUMMARY OF TOTAL SEDIMENT BUDGET PROCEDURE <br />This section summarizes the basic procedures used within the sediment budget <br />program; details on the individual components and assumptions are explained <br />more fully in the next sections. <br />1) The mean daily discharges at the Little Snake near Lily and the Yampa River <br />near Maybell stations are summed and equated to the mean daily discharge at <br />Deerlodge Park and Mathers Hole. This synthetic record for the 1941 to <br />1986 water years is deemed the 'historic' record at Deerlodge Park. <br />2) Using the mean daily discharge, the total sediment rating curves for <br />Deerlodge Park and Mathers Hole are used to estimate the tons of sediment <br />transported at both sites for each day. Rating curves for bed load size <br />fractions where also used in separate runs, but curves for comparable size <br />fractions were not readily available. <br />3) The difference between the Deerlodge Park and the Mathers Hole daily <br />sediment load in tons is determined, and represents a surplus or deficit <br />for the Deerlodge Park - Mathers Hole reach for that day. <br />4) The surplus/deficit in the reach is summed on a daily basis, and the <br />'running balance' reported at the end of each month and water year for the <br />1941- 1986 period. The ending balance of one month is used as the <br />beginning balance of the next month.
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