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Last modified
7/14/2009 5:02:31 PM
Creation date
5/20/2009 9:32:20 AM
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UCREFRP
UCREFRP Catalog Number
7930
Author
Ketcheson, G. L.
Title
Sediment Rating Equations
USFW Year
1986.
USFW - Doc Type
An Evaluation for Streams in the Idaho Batholith.
Copyright Material
NO
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360 <br />>. 300 <br />? rn <br />m E <br />p 240 <br />JZ <br />w_O <br />} a 180 <br />Hm <br />ZO <br />ww <br />G Z 120 <br />w - <br />y W <br />60 <br />1- <br />0 <br />SEDIMENT YIELD USING <br />RATING EQUATIONS, mg/YR <br />Figure 6-Comparison of sediment yield esti- <br />mates from two methods: (1) by using sedi- <br />ment rating equations and (2) by time- <br />integration between hand samples. Data <br />from stream monitoring on the Boise <br />National Forest. <br />120 <br />100 <br />80 <br />60 <br />40 <br />20 <br />0 <br />SEDIMENT YIELD USING RATING EQUATIONS, mg/YR <br />Figure 7-Comparison of total sediment <br />yield estimates from two methods: (1) by <br />using sediment rating equations and (2) by <br />time-integration between hand samples. Data <br />from streams in the Silver Creek study area. <br />Five estimates of sediment yield were made from the <br />data in Silver Creek (table 2). The first method used a <br />sediment rating curve for total sediment from the hand <br />samples and mean daily streamflow. The second method <br />time-integrated total sediment as described above for the <br />Boise National Forest data. The third and fourth <br />methods were the same as the first two with the excep- <br />tion that the automatic pumping sampler sediment data <br />were used. The fifth method estimated sediment yield <br />based on the volume of sediment in sediment dams. <br />The equivalency of the rating equation method and <br />integration method for the hand samples was tested <br />with a paired t test. The hypothesis that the two <br />methods give the same estimates was accepted at the <br />95 percent level. However, as with the Forest monitoring <br />data, the time-integration method averaged slightly <br />higher yields than the rating equation method (fig. 7). <br />The sediment yields from these two methods are com- <br />pared with the sediment dam yields (fig. 8), and neither <br />tested different from the sediment dam yields at the 95 <br />percent level. But the yield estimates from the rating <br />equations did test different at the 90 percent level. <br />Although the differences were not significant by the <br />paired t test, the sediment dam yields were somewhat <br />less for years of low sediment yields and greater for high <br />sediment years than the estimates by rating curves and <br />integration. The paired t test only tests the means, so <br />the variances could be different. <br />m <br />} <br />IM 140 <br />E <br />p 120 <br />U) •TIME INTEGRATION <br />H <br />Q <br />100 <br />W <br />F <br />Z <br />80 <br />cW <br />C <br />~ 60 <br />} <br />m <br />40 <br />W <br />} <br />Z 20 <br />W <br />g <br />D <br />W 0 <br />*RATING EQUATIONS <br />tiA <br />JPy <br />O <br />O1 • <br />• ? • As • •• ? / <br />• /? <br />•• • <br />J <br />140 <br />120 <br />100 <br />80 <br />60 <br />40 <br />20 <br />20 40 60 80 100 120 140 <br />SEDIMENT YIELD FROM SEDIMENT DAMS, mg/YR <br />Figure 8-Comparison of sediment yield esti- <br />mates using time-integration, rating equa- <br />tions, and sediment dams from Silver Creek <br />data. <br />8 <br />60 120 180 240 300 360 <br />20 40 60 80 100
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