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<br />316 <br /> <br />material and significant quantities of material larger than 100 mm in diameter. <br />For these streams, II. bedload-transport rate was computed for each size class, <br />which then was multiplied by the fraction of the bed in the size class. The <br />bedload-transport rate for a given discharge at the gaging station was deter- <br />mined by summing the bedload-transport rates of the several size classes. Com- <br />puted bedload-transport rates were typically less than 20% of the total sedi- <br />ment load. Thus, although the uncertainty of the bedload-transport rate may <br />be large (:t50%) (White et al., 1975), the uncertainty in the total sediment <br />load introduced by computing rather than measuring the bedload-transport <br />rate is small. <br />The bedload-transport rate vs. discharge relation was determined by fitting <br />a curve to several computed bedload-transport rates for the range of discharges. <br />The total sediment-load vs. discharge relation (daily values) was determined <br /> <br /> <br />" <br />" <br />, <br />" <br />'\ <br />\ <br />~ <br /> <br />~ <br />\ <br />\ <br />\(,/l <br />\';. <br />\~ <Jl <br />\:1 ~ <br />... Ol <br />\0 cO <br />Ol (Il <br />\0- <br />\. <br />\ <br />\ <br />\ <br />\ <br />\ <br />\ <br />\ <br />\ <br />\ <br />'\ <br />'\ <br />0.1 <br />0.01 0.1 1 5 20 50 80 95 99 99.9 <br />PERCENTAGE OF TIME DISCHARGE AND SEDIMENT LOAD <br />ARE EQUALED OR EXCEEDED <br /> <br /> <br />o <br />z <br />o 50 <br />u <br />w <br /><J) <br />a: <br />w <br />ll.. <br /><J) <br />a: <br />w <br />I- <br />~ 10 <br /> <br />u <br />~ 5 <br />u <br />z <br /> <br /> <br />w <br />C) <br />lr- <br />< <br />:I: <br />U 1 <br /><J) <br /> <br />o <br />0.5 <br /> <br /> <br />10.000 <br /> <br />5000 <br /> <br />> <br /><{ <br />o <br />a: <br />w <br />1000 a.. <br /><J) <br />Z <br />o <br />500 I- <br />U <br />a: <br />I- <br />w <br />:E <br />Z <br /> <br />o <br />100 <{ <br />o <br />~ <br />l- <br />SO jj <br />:E <br />o <br />w <br /><J) <br /> <br />10 <br /> <br />5 <br /> <br />'V <br />Fig. 3. Streamflow and total sediment-load-duration curves for the Little Snake River <br />near Dixon, Wyoming. . <br /> <br />I <br />I <br />I <br />I <br />! <br />L_~__ <br /> <br />" <br /> <br />~ <br /> <br />I <br />I <br /> <br />L' <br />