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<br /> <br />12 <br /> <br />:i. <br />o <br />~ 10 <br />> <br />w <br />~ <br />~l- 8 <br />~~ <br />~ z 6 <br />,,- <br />V> <br />:; <br />" <br />w <br />'" <br />... <br />V> <br /> <br />o Streambed flux <br />- Stream surface elevation <br />~ Riffle-greaterthan l-percentslope <br /> <br /> <br />4 <br /> <br />2 <br /> <br />U I- 0.0002 <br />mg <br />,,~ 0 <br />~ ffi 0.0001 <br />~~ <br />"z <br />i8 <br />Ow <br />wv> <br />"'", <br />~ ~-o.ooo' <br />~tu <br />"'w <br />fJ) LL-O.OOO2 <br />o <br /> <br />o <br /> <br />o <br />od" <br /> <br />'" 0 <br />o 00 ~_ <br />o -~-""~.#':--~-~~---o----- <br />00 ~o . <br />o <br />o <br />o <br /> <br />33 66 99 <br />DOWNSTREAM DISTANCE, IN FEET <br /> <br /> <br />A study in Colorado indicated that hyporheic exchange <br />in mountain streams is caused to a large extent by the irreg- <br />ular topography of the streambed, which creates pools and <br />riffles characteristic of mountain streams. Ground water enters <br />streams most readily at the upstream end of deep pools, <br />and stleam water flows into the subsurface beneath and to <br />the side of steep sections of streams (riffles) (Figure H-2), <br />Channel irregularity, therefore, is an important control on the <br />location of ground-water inflow to streams and on the size of <br />the hyporheic zone in mountain streams because changes in <br />slope determine the iength and depth of hyporheic fiow paths, <br /> <br />j <br />Subsurface <br />to stream <br />Stream to <br />subsurface <br />I <br /> <br />Figure H-2. In mountain streams characterized <br />by pools and riffles, such as at Saint Kevin Gulch <br />in Colorado, inflow of water from the hyporheic <br />zone to the stream was greatest at the downstream <br />end of riffles, (Modified from Harvey, J. w., and <br />Bencala, K.E., 1993, The effect of streambed <br />topography on surface-subsurface water exchange <br />in mountain catchments: Water Resources <br />Research, v, 29, p, 89-98.) <br /> <br />'" <br /> <br /> <br />Chalk Creek, Colorado, (Photograph by Briant Kimball.) <br /> <br />The source and fate of metal contaminants in streams <br />receiving drainage from abandoned mines can be determined <br />by using solute tracers, In addition to surface drainage from <br />mines, a recent study of Chalk Creek in Colorado indicated <br />that contaminants were being brought to the stream by <br />ground-water inflow, The ground water had been contami- <br />nated from mining activities in the past and is now a new <br />source of contamination to the stream, This non point ground- <br />water source of contamination will very likely be much more <br />difficuit to clean up than the point source of contamination <br />from the mine tunnel. <br /> <br />37 <br />