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<br />I <br /> <br />I <br /> <br />22 <br /> <br />07/16/99 <br /> <br /> <br />I <br /> <br />I <br /> <br />Table 2. Sediment transport formulas and dassifications. <br /> <br />I <br /> <br /> "'ldllll< III II !IhlHHI 1'111111 , <br /> 0- <br /> '" <br /> '" <br /> - ~ <br /> - 00 <br /> 0- il "" ~ <br /> a- <- <br /> '" 0 - 0- '" <br /> a- ... - '" ~ ~ <br /> - '0 .ll ~ ~ - "' <br /> il ~ N <- <br /> '0 "5 00 d a- <br /> 0 c ~ ~ ~ <br /> fi' 1J ~ <br /> :0- ... u ; <br /> <- '0 '" - II 3 <br /> "' ~ - e ~ <br /> 00 a- u B <i :I: ~ N <br /> :::. - '" '" u '" ." <- a- <br /> ~ - c c .,. .s .. c ~ <br /> ;>, ~ 'jj .~ - E ~ - <br /> C '0 - B ;>, <br /> 1;; ~ ~ u .. <br /> '!l <l ~ .5 .. c -" <br /> :E c c u c ~ -0 <br />Criteria Grouping 0 '" Oil Oil =- "' "- "' <( ,.. U <br />Approach Shear Stress " " " " " " <br /> Power " v' " <br /> Parametric " <br />Load Component Bed Load v' .,' .,' .,' .,' .,' <br /> Suspended Load .,' <br /> Bed-Material Load .,' v' .,' .,' <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Despite the intense efforts expended in the development of these formulas, evaluation against field <br />data indicates that they commonly overpredict or underpredict sediment loads by orders of <br />magnitude of actual measured sediment transport rates. This discrepancy is likely due to imperfect <br />knowledge of the physics of sediment transport and also to the extensive variability and <br />heterogeneity in hydrologic and geologic factors. For these reasons, no one formula is better than <br />the others. Selection of a sediment transport formula must be dictated by how well the conditions <br />of the problem at hand match the assumptions underlying the formula. If possible, applicability of <br />the formula should be verified with site-specific field data. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />