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<br />NAU Sand Bar Studies <br /> 1100 0.12 <br /> A water discharge <br /> 1000 . suspended-sill and clay <br /> ... suspended-sand (') <br /> 900 0 <br />'" 0,08 " <br />;;0- n <br /> <D <br />~ ... " <br />800 - <br />.. ;;; <br />~ .. 5' <br /><D 700 " <br />.s::: <br />" . 0,04 <- <br />,!!l .. 0 <br />C 600 . <br /> .. <f'. <br /> 500 .. <br /> .. <br /> . 0,00 <br /> 400 <br /> 0.11 0,31 <br />E <br />E B '" <br /> <D <br />,!;; . . 0,30 c. <br />'" .... '" <br /> <D <br />,!::! c. <br />'" 0,10 0,29 3' <br />,!;; <D <br />e " <br />0> .. <br /> 0,28 "" <br />'C ;;; <br />" <br />ClI 5' <br />'" '" <br />'C 0,09 ... 0.27 N' <br />'" <D <br />'C <br />" . Channel Bad Sand 5' <br />'" <br />c. .. Suspendad.Sand 0,26 3 <br />'" 3 <br />" <br />en <br /> 0,08 0,25 <br /> 11.2.97 11-3-97 11-4.97 11.5.97 11-6.97 11.7-97 <br /> <br />Final Report <br /> <br />~ . <br />" <br /> <br />~ <br />~ <br /> <br />, <br /> <br /> <br /> <br />',' <br /> <br /> <br />" <br /> <br />.'~ <br />" <br />.~ <br />;~ <br />r~ <br />", <br />~, <br /> <br />~I <br />.,. <br />, <br /> <br />;...' <br /> <br />'< <br /> <br /> <br />To" <br />:::~ <br /> <br />Figure 6, Suspended sediment concentrations and instantaneous discharge at the lower Marble <br />Canyon gage during the 1997 test flow in A. Suspended sediment grain size and bed sediment grain <br />size in B. <br /> <br />r:: <br />;," <br />~r <br />~~~ <br />~ <br /> <br />" <br />':~. <br />~~ <br /> <br />the 1997 Test Flow the median grain size of suspended sediment was still finer than that observed at <br />the start of the 1996 Controlled Flood but the bed material grain size had nearly equaled the size <br />measured towards the end of the 1996 Controlled Flood (Topping et ai" 2000b), <br />There was one important difference that existed in sand transport characteristics at the Lower <br />Marble Canyon gage between the controlled high releases in 1996 and 1997, During the 1996 <br />Controlled Flood, the suspended-sand concentrations at the Lower Marble Canyon gage were <br />approximately half those measured at the Grand Canyon gage, located 42 kIn further downstream <br />(Topping et ai" 2000b), However, during the 2 days of the lesser magnitude 1997 Test Flow, the sand <br />concentrations measured at the Lower Marble Canyon gage equaled those measured at the Grand <br /> <br />~ <br />~~ I <br />':'! <br />;1; <br />~~~ <br />?; <br />,,' <br /> <br />.~ .~ <br /> <br />22 <br />