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<br /> <br />4096 1024 256 <br />100 <br /> <br />64 <br /> <br />;g <br />E..- <br /> <br />80 <br /> <br />c:: <br />'" <br />.r:: <br />t- <br />~ <br />c:: <br />II: <br />E <br />" <br />o <br />~ <br />a. <br />" <br />> <br />"ia <br />'S <br />E <br />::> <br />() <br /> <br />60 <br /> <br />40 <br /> <br />20 <br /> <br />o <br />-12 <br /> <br />-8 <br /> <br />-6 <br /> <br />-10 <br /> <br />Particle Size (mm) <br /> <br />16 <br /> <br />0.25 0.063 <br /> <br />4 <br /> <br />- . - Debris flows <br /> <br />-4 <br /> <br />-2 <br /> <br />4 <br /> <br />o <br /> <br />2 <br /> <br />Particle Size ($) <br /> <br />Figure 14. Particle-size distributions of 41 historical debris flows in Grand Canyon. <br /> <br />range from 1.5 to 2.0 Mg/m3. The larger value of <br />this estimate most likely results from <br />underestimation of macro-pore spaces between <br />larger par1icles. We therefore used the upper limit <br />of measured densities, 2.0 Mg/m3 (60 percent solids <br />by volume), to calculate debris-flow sediment <br />yields. <br /> <br />Reworking of Debris Fans by the <br />Colorado River <br /> <br />Reworking of debris fans by the Colorado <br />River is a complicated process that has been rarely <br />documented in Grand Canyon (Kieffer, 1985; <br />Webb and others, 1999a, 1999b; Pizzuto and others, <br />1999). Reworking releases sediment stored in <br />debris fans - particularly sediment finer than <br />gravel size - into the river, which rearranges the <br />sediment into sandbars and debris bars. In order to <br />understand sediment yield to the Colorado River <br />from debris flows, some estimate must be made of <br />the amount of sediment that is stored in debris fans <br /> <br />versus what is expected to be released into the <br />Colorado River. The technique must be such that all <br />debris fans in Grand Canyon can be considered, if <br />only on a reach-average basis. In the pre-dam <br />Colorado River, the 10-yr flood had a discharge of <br />3,940 m3 Is, which is more than sufficient to overtop <br />and rework most historic debris fans in Grand <br />Canyon (Melis, 1997). Therefore, we assume that in <br />the pre-dam era all fine sediment delivered by <br />debris flow entered the river every decade. <br /> <br />After completion of Glen Canyon Dam, <br />discharges decreased substantially and powerplant <br />releases caused only minor reworking of debris fans <br />(Melis and others, 1994). Large dam releases, such <br />as the 1983 discharge and the 1996 controlled <br />flood, significantly reworked debris fans (Kieffer, <br />1985; Webb and others, 1989, 1999a, 1999b). The <br />10-yr flood on the post-dam river is 1,430 m3/s, <br />about the size of the 1996 controlled flood. Using <br />debris fan volume data contained in Kieffer (1985) <br />and Webb and others (1989, 1999a, and 1999b), we <br />estimated that 25:1:30 percent of the volumes of 13 <br /> <br />32 Sediment Delivery by Ungeged Tributaries of the Colorado River In Grand Canyon <br />