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200 <br />100 <br />10 <br />v <br />F- <br />0 <br />a 1.0 <br />co <br />z <br />a <br />Cr <br />F- <br />0 <br />Q <br />0 <br />0.1 <br />w <br />m <br />LL <br />0 <br />F- <br />0 <br />z <br />? 0.01 <br />z <br />0.001 <br />0 0001 <br />T I I T i T T ? T TT-?T <br />'o f <br /> <br /> (Do <br />O <br />0% O <br /> Einstein bedload <br /> function (Brown <br />0 modification) <br />j O <br />8 ? <br />o° <br /> x <br /> Einstein bedload <br /> P( function <br />0 Q <br /> <br /> x O <br />? o <br /> x <br />° <br />e <br /> <br />6 e ° x <br />o <br />° <br /> <br />x <br />x <br />° <br /> x <br />v x <br /> <br />° x <br />° <br />x <br />° <br />El o <br />x <br /> HELLEY-SMITH BEDLOAD <br />O DATA: <br />C) East Fork River. Wyoming, <br />x Emmett ( 1979) <br />0 Tanana River. Alaska. Emmett <br /> and others ( 1978) <br /> Snake River near Anatone. <br />0 Washington. Emmett ( 1976) <br /> Big Sandy River. Wyoming <br />X Clearwater River at Spalding. <br /> Idaho. Emmett and Seitz <br /> (1974) <br />I I I 1 1 1 1 1 1 I I I I I I I 1 1 I I I I I I I I <br />0.01 0.1 1.0 10 <br />INVERSE OF INTENSITY OF SHEAR ON PARTICLE (-L) <br />Figure 26.--Comparison of Helley-Smith bedload data with the Einstein <br />bedload function. <br />38