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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 />Table 5.1. Summary of rating curve coefficients (Qs=aQ~ <br /> <br />Gage Total Suspended Sand Wash <br /> Load wad Load Load <br /> a b a b a b a b <br />Mayben NA NA NA NA <br />Lily 5.37e-2 1.62 0.0447 1.64 0.028 1.64 <br />Deerlodge 3.168 1.02 12.58 0.88 3.498 0.91 0.557 1.16 <br />Mathers 0.379 1.26 0.381 1.26 1.57e-4 2.01 3.61 0.951 <br />Jensen (pre-dam) 6.100-3 1.7 3.38e-7 2.62 2.100-4 1.88 <br />(Post-dam) 1.72e-2 1.58 2.04e..5 2.16 5.03e-6 2.26 <br />Note: Deerlodge and Mathers coefficients are bias corrected and were derived using data for <br />discharges greater than 2000 cfs. <br /> <br />Deerl0d2e Park G8ie <br /> <br />The USGS (Elliot, et al., 1984) defined rating curves for the Deerlodge Park gage based on <br />data colJected in 1982 and 1983. The rating curves were prepared for total sediment load, as well as <br />various components of the total load. Since the published report included the measured data, it was <br />possible to derive the bias correction coefficients. <br /> <br />Application of the bias correction caused some inconsistency in the rating relationships. <br />The bias correction tended to over correct for the expected underprediction of the mean value (see <br />Table 5.2). Additionally, the bias corrected suspended load rating curve plotted above the total load <br />rating curve, which did not occur with the uncorrected rating curves. Review of the raw data <br />indicated that there was a noticeable break in the data set between about 1000 and 2000 cfs, with a <br />smalJ cluster of points in the 1000 cfs range and a larger cluster of points above 2000 cfs. With bias <br />correction analysis based only on the upper cluster of points, more consistent rating relationships <br />resulted for the higher flows. Given that the transport rates were typically very low in the lower <br />cluster, and that the flows of significance in sediment transport are typically the higher flows, <br />regression on only the higher flows was justified. Figure 5.2 illustrates the fit of the various rating curves <br />against the raw data, and the preferred coefficients for use in computation of effective discharges are <br />summarized in Table 5.1. <br /> <br /> Table 5.2 Results of bias correction analysis for Deerlodge Park. <br /> Raw Original Corrected <br />aa Data No Obs. Mean of R"2 Correction Mean of <br />Os Mean n a b Pred. Coef. C a b Corr. Val. <br />TOTAL LOAD <br />Plows 0> 2000 36182 26 2.609E+OO 1.0198 3OS03 0.420 1.2141 3.168E+OO 1.0198 37032 <br />All Plows 30653 31 2.916E-01 1.2585 26652 0.787 1.2043 3.511E-01 1.2585 32fN7 <br />SUSPENDED LOAD <br />Plows Q > 2000 3SS5O 27 9.5S6E+OO 0.8750 19768 0.291 1.3168 1.2S8E+01 0.8750 37614 <br />All Plows 293S2 33 1.254E-01 1.3490 24902 0.757 1.4299 1.193E-01 1.3490 36119 <br />SAND LOAD <br />Plows Q > 2000 14154 26 2.937E+OO 0.9092 12310 0.389 1.1913 3.498E + 00 0.9092 14664 <br />All Plows 11939 31 1.678E-02 1.4712 1113S 0.808 1.2500 2.097E-02 1.4712 13918 <br />WASH LOAD <br />Plows Q > 2000 21212 26 3.301E-01 1.1642 12694 0.271 1.6878 S.572E-Ol 1.1642 24015 <br />All Plows 18129 31 4.879E-Ol 1.1220 10787 0.562 1.7022 8.30SE-01 1.1220 20729 <br /> 5-6 <br /> <br />I <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />
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