Laserfiche WebLink
100 <br />10 <br />,pn? <br />'O' <br />I- <br />1.0 <br />O <br />(L <br />U) <br />Z <br />Q <br />H <br />0 <br />a <br />0 0.1 <br />0 <br />w <br />M <br />o0 <br />8 ?. <br />o° <br />p p <br />O <br />o` <br />LL. <br />O <br />r <br />F- <br />U) <br />Z 0.01 <br />W <br />I- <br />Z <br />0.001 <br />d <br />v <br />13 <br />0 <br />0 <br />Einstein bedload <br />function (Brown <br />modification) <br />O <br />Einstein bedload <br />function <br />X <br />J 00 O <br />X O <br />X <br />O <br />0 X <br />X ? <br />Xp X <br />X <br />A <br />X <br />x <br />HELLEY-SMITH BEDLOAD <br />DATA: <br />East Fork River. Wyoming. <br />Emmett ( 1979) <br />v Tanana River. Alaska. Emmett J <br />and others ( 1 978) <br />Q Snake River near Anatone. <br />Washington. Emmett ( 1 976) <br />p Big Sandy River. Wyoming _ <br />X Clearwater River at Spalding. <br />Idaho. Emmett and Seitz <br />(1974) <br />0.00011 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 x 1 1 <br />0.01 0.1 1.0 10 <br />INVERSE OF INTENSITY OF SHEAR ON PARTICLE (f <br />Figure 27.--Comparison of Helley-Smith bedload data with the Einstein <br />bedload function using Colby's modification of the bedload <br />intensity. <br />O <br />X <br />40