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s <br />F-3 <br /> water-qual[ty canpln collected during law ec reamf for occur more by [re<ex dilution. :! the we lie de acribetl in the Drat[ E16 w <br /> <br />frequently em <br />sampled in <br /> (low flow duration usually laa[a Cor mnnehs'r while conr'ent raclons conjunction rich co lie ctlon o! tracer 1nFOZma[ion, e <br /> Eoz eonprehensiva Baca eec <br /> conac icuenrc collected du clog pe riodc o[ xaznEall or snow melt characterizing exleting conditions could be developed <br />Thi <br /> <br />['unoEE occur . <br />s aor[ <br />oC <br /> lees frequently Iperiode of runoff usually ]acts [or a day (e) or iniozmat ion <br /> weeks]. cnu ld be obta load fot the zange of atreamt lows. <br /> In addition, th¢ delta preeeneed [epreeent hydrologic condltlane 7 ~. I we9 unab:e to Eicd any tats reuse in [he Drat E15 !oi <br />F-'~ <br /> Ecr water Year . <br />water-quality <br /> 199]. watax-quality data has been collected at these el tee since menltaring In Piceance Creek upstream end dom st ream o[ the <br /> 13]0 on a p[gpvaatl <br /> rmncinuoua baste far epecillc conductance and racer temperature dews lopnwnt. A poaelbla place to monit of upstream eE the ' <br /> end a periodic development would be <br /> bnale Eer mej or ions, tratt me to le, nu czienta. Conatdetatl on cf et the historic scceangege 09)06700 Piceance Creek below Ayan <br /> she blecvriC LLlch. <br /> data would pprovide sddltlvnal chars ccex Sxetion of racer-quelf[y Because of <br /> conditl ono In uncertainty aaa oclaced with the ground-water boundary of the <br /> Plceance Creek. propoee0 <br /> tlevel opment, the downstream monitoring el to would hove to be <br />F3 <br />4 a' ]n edd_tion to [he data collected at [he three eftes cuuside and after <br />. rn ferenced, et reemElow some reconnaieeence of the at ream mach and surrounding Brea. <br /> noel votes-quality data ace nvelleble stet lone 09306061 Plceauce <br /> Creek above ge[erencea~ <br /> duntet Creek, 09]06]02 Ho[ae Dzaw neat Rangely, and 09)0620] Rimbell, B.A., 199. Vee of trace[ injectlone and synoptic <br /> gorse Dcaw at camp ling co meaeuxe <br /> Nuuth near Rangely. metal loading [tom acid mine Orainage~ U.S. Gaol ogf sal Survey <br /> Pact Sheet. <br />F-3 <br />5 5. On page ]-17 there Ss a reference to a 199] USGS Kntet-Ouallcy <br />. Stst ion <br /> ]evcx tp[ion for Paceunce Cteek at Mhf to Aiver City. The reference tf you have any qua atione about these co~mienea please contact me. <br /> on page ]-B <br /> Sndicaeea [het the ileac rlptlan raa preps[atl by K.N. tlutche i. The <br /> dear r'_p cior. Slncaxe ly, <br /> was prepared by Bab Boulger In 1990 end revi eed by K.N. Butcher <br /> in 197'1. 7tia <br /> coeument is part of the station record Srtentletl for general <br /> descx:pt lve Paul von Guerazd <br /> pu rDOSee acd 1s oat a formal publication of [he USGS. Neatern Slops Subdiatriec Chief <br /> y6a Horiaon Drive, Room 125 <br />F <br />3 <br />6 6. On page 9-15 [he [e ie mention aC Deaalble diacherge of Grand Junction, CY: !1506 <br />- <br />. croundrater rith <br /> <levecetl rote] Di eaolved So11tla Snto Piceence Creek. If theta is PH 970-2t 5-575] ext ]O1< <br /> no recdn[ PA% 9T0-215.10]6 <br /> Sn [otmatior, on ba eellne lore prejeetl et ream[low gain/lose and teal] pbvonweaugga.gov <br /> aneocf ated <br /> xa[er-quality Eor Picean ce Czeek. A wethotl tlevelopetl by Rimbal] <br /> 1199]1 <br /> provides <br /> a method to characierl xe the q'uancity and quality of exleting <br /> gtoundrater <br /> inf love Into PScaance Creek. the nu![hod allora for a measurement <C. 'Paul Vonguera rd, Subdiec ric[ ChleE, Crand Junctlo... <br /> o[ acream(low <br />• • • <br />