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<br /> 2.0 <br /> <J) 1.75 <br />W ~ <br />d 1.5 <br />W <br />en ul 1.25 <br />00 CJ <br /> a: 1.0 <br /> <: <br /> I 0.75 <br /> () <br /> (f) 0.5 <br /> 0 <br /> 0.25 <br /> 0 <br /> <br />Dry Run <br /> <br /> '" <br /> 0 <br /> ~ <br /> >< () <br /> '- W <br /> 0> <br /> E ~ <br /> () <br /> (f) 0 <br /> If) <br /> 00 C 6ooC\J <br /> 0 ~ <br /> -.;::; >-0 <br /> ctl :t: ,.... <br /> ~ > >< <br /> C '-=E <br /> 00 CIl 400 g 0 <br /> 0 "O'U) <br /> C <br /> 0 Co <br /> () O..c <br /> - ()g; <br />EC Truck 200 C 200 Cii is. <br /> CIl 0 <br />J E ';:: <br /> is - <br /> 0 <br /> CIl (I) <br /> 0 (f) 0 W <br />30 35 <br /> <br />t."" "S <br />, '. <br />, , <br />, '. <br />, , <br />, , <br />.......) '. <br /> <br /> <br /> <br />...... <br />EC Runoff <br />....- '" /: <br />.... ....x--..... -----............7.-1.....' <br /> <br />...# <br />............ <br /> <br />5 <br /> <br />10 <br /> <br />15 <br /> <br />20 <br /> <br />25 <br /> <br />TIME FROM BEGINNING OF RAINFAll, min <br /> <br />Figure 5. Discharge, sediment concentration, and electrical conductivity over <br />time for dry runs on steep dissected Mancos shale upland. <br /> <br /> 2.0 <br /> 1.75 <br /><J) 1.5 <br />~ <br />d 1.25 <br />ul <br />CJ 1.0 <br />a: <br /><: 0.75 <br />I <br />() 0.5 <br />(f) <br />i5 0.25 <br /> 0 <br /> <br />Wet Run <br /> <br /> <br /> '" <br /> 0 <br /> x () <br /> '- W <br /> 0> <br /> E ~ <br /> () <br /> (f) . <br /> If) <br />600 6ooC\J <br /> C ~ <br /> 0 CO <br /> '-= <br /> ctl --~ <br /> >)0( <br /> '- 400g ~ <br /> - <br />400C <br /> CIl <br /> 0 ",- <br /> C c<J) <br /> 0 00 <br /> () ()..c <br /> E <br />200E 200 Cii :i. <br /> CIl 0 <br /> E -;:: <br /> - <br /> is 0 <br /> CIl <br /> (I) jjj <br />0 (f) 0 <br />35 <br /> <br />:~'......"... <br /> <br />'I._f'A.--X- <br /> <br /> <br />. <br /> <br /> <br /> <br />....... ........... .........i\............. <br />S <br />"EC Runoff <br />...X--x _-'"')(--------.. <br />'j..- --x___- <br /> <br /> <br />EC Truck <br />i <br /> <br />5 <br /> <br />10 <br /> <br />15 <br /> <br />20 <br /> <br />25 <br /> <br />30 <br /> <br />TIME FROM BEGINNING OF RAINFAll, min <br /> <br />Figure 6. Discharge, sediment concentration, and electrical conductivity over <br />time for wet runs on steep dissected Mancos shale upland. <br /> <br />21 <br /> <br />1.-1 <br /> <br />