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<br />0018i9 <br /> <br />The Helley-Smith bedload sampler has a well-established sediment-trapping efficiency. <br />Extensive field calibration (Emmett, 1980) was conducted by comparing the transpon rate as <br />measured with the Helley-Smith bedload sampler to the transpon rate as established by a stream- <br />wide bedload trap. That study indicated a 'near-perfect' sediment trapping efficiency for panicle <br />sizes between 0.5 and 16 mm, the panicle sizes in transpon at the calibration facility and the vast <br />majority, by weight, of panicle sizes presented herein. For the present data, a sediment-trapping <br />efficiency of 100 percent was assumed for all panicle sizes. <br /> <br />In association with the field calibration of the Helley-Smith sampler. multiple sampling <br />traverses were conducted (Emmett, 1980). These showed that about 20 cross-sectional sampling <br />locations account for the spatial variation in transport rate, and showed that more than two <br />traverses did not greatly change the estimated mean value of bedload transpon. <br /> <br />The sampling procedures employed in the collection of bedload data were based upon the <br />Single Equal Width Increment (SEWI) method (Edwards and Glysson, 1988). Multiple samples <br />at equal width intervals across the channel were collected. There were 20 or more subsamples <br />taken during each of two each traverses of the channel, although in earlier years at the Forest <br />Service sites fewer subsamples were collected during a single traverse of the channel. For Forest <br />Service sites, a criterion was established requiring at least 10 subsamples. Each subsample lasted <br />for 30 or 60 seconds unless high transpon rates forced shorter sampling times. The sampling <br />time was constant across a given traverse. <br /> <br />To assure that adequate field, laboratory, and office techniques were used in collection <br />and analysis of bedload data, W.W. Emmett routinely met, and/or otherwise corresponded, with <br />those personnel responsible for assembling the sediment data sets presented herein. During his <br />several decades with the USGS, Emmett pioneered research into bedload samplers and <br />proceduresJor their use and was responsible for many of the guidelines that led to standard <br />techniques in bedload sampling. This collaboration assured consistent application of state-of- <br />the-science guidelines. <br /> <br />Suspended sediment was also collected at sites though it was not used in quantifying the <br />claims. Suspended-sediment samplers, developed and distributed by the Federal Interagency <br />Sedimentation Project (FISP), are standard in design and use throughout the United States <br />(Edwards and Glysson, 1988; Williams et al., 1988). For use in collecting the suspended- <br />sediment data presented herein, the wading version of the depth integrating sampler is the <br />USDA-48 or USDA-8I, the suspension version of the depth integrating sampler is the USD-74, <br />and the suspension point sampler, albeit used sparingly, is the USP-61. <br /> <br />For suspended load, about 10 cross-channel locations are adequate; generally, every other <br />bedload-sampling location sufficed as the cross-channel locations for suspended-load sampling. <br />The vertical transit rate of lowering and raising the suspended-sediment sampler was everywhere <br />an Equal Transit Rate (ETR) to maintain the equal-discharge weighting. Sampling procedures <br />for suspended sediment are quite standard and are well documented (e.g., Edwards and Glysson, <br />1988; Williams et al., 1988). <br /> <br />United States' Expert Report Disclosing Methodologies for Quantification of Organic Act Claims Consolidated Subcase No. 63-25243 <br /> <br />29 <br />