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<br />1 10 <br />_ 4 7 0 11 <br />---__ 31\ 5 6 0 __~---------...---nn---n <br />;__-_._____n___..------------ 9 12 <br />04 <br />180 <br /> <br />O{)2208 <br /> <br /> 250 <br /> a: <br /> w <br />:;; f-- 200 <br />::>Z:J <br /><:lOa: <br />--'-W <br /><(~[L 150 <br />Oa:UJ <br />Of--:;; <br />WZ<( <br />>Wa: 100 <br />--'0(') <br />OZ- <br />UJO--' <br />(j)O:::! 50 <br />o :;; <br /> ~ <br /> <br />1 <br />A" ti. <br /> <br />, <br />, <br />",2 -i... <br /> <br />... " 6- <br />" 5 . ---- <br />'~----------~-- <br /> <br />o <br />230 220 <br /> <br />160 <br /> <br />140 <br /> <br />DISTANCE FROM MOUTH OF YAMPA RIVER, IN RIVER MILES <br /> <br />EXPLANATION <br /> <br />200 <br /> <br />__.__ Calcium at Yampa River site <br />--..-- Alkalinity al Yampa River site <br /> <br />L10 <br /> <br />UJ <br />:;; <br /><( OJ <br />a:0 <br /><!JO <br />-<( <br />::10 <br />~UJ <br />Z<( <br />-a: <br />-W <br />i'=t: <br />---' <br />~a: <br />--'w <br />~[L <br />--' <br /><( <br /> <br /> <br />--- <br />--- <br /> <br />11 12 <br />-~---------~~------------ <br /> <br />120 <br /> <br />80 <br /> <br />20 <br /> <br />o <br /> <br />60 <br /> <br />40 <br /> <br />100 <br /> <br />D Calcium at tributary site <br />6. Alkalinity at tributary site <br /> <br />Note: number by symbol is site number in tables 1 and 3 <br />Figure 4, Concentrations ot calcium and alkalinity at Yampa River and main tributary sites, August 16-19, 1999, <br /> <br />dissolved oxygen concentration that was 161 percent <br />of saturation (relative to the concentration that would <br />occur at equilibrium with the atmosphere)(fig, 5), <br />Calculations using the thermodynamic-speciation <br />program PHREEQC (Parkhurst, 1995) indicates that <br />dissolved carbon dioxide gas (C01) (fig, 5) was under- <br />saturated at 26 percent of the concentration that would <br />occur at equilibrium with the atmosphere, <br />Drever (1982) describes the formation of algae <br />(which represents microscopic and macroscopic plant <br />composition) by photosynthesis: <br /> <br />106 COl + 16 N03- + HPol- + 122 H10 + <br />18 H+ + (trace elements, energy) = <br />CI06H16301IONI6P,(algae) + 13801, <br /> <br />This equation explains the large pH value <br />measured at site 3 by the uptake of dissolved C01, <br />thus decreasing the concentration of carbonic acid <br />(H1C03) dissolved in the water, and by direct uptake <br />of H+ ions, which raises pH, Photosynthesis also <br />explains the large oversaturation with dissolved <br />oxygen, Equation 1 also shows that the formation of <br />plant biomass depends on the availability of dissolved <br />nitrogen and phosphorus, either of which can limit the <br />ability of the reaction to proceed, The sample from site <br />3 had the largest measured concentration of dissolved <br />phosphorus (0,06 mg/L) and the second largest (after <br />site I) measured concentrations of dissolved ammonia <br /> <br />(I) <br /> <br />plus organic nitrogen (0.30 mg/L) and dissolved <br />organic carbon (5,0 mg/L) of the main-stem and tribu- <br />tary river sites, These constituents are derived from <br />sewage effluent, livestock waste, excretions from <br />aquatic organisms, and other natural sources, <br /> <br />The effects of photosynthesis on pH and <br />dissolved oxygen concentration were attenuated at <br />Yampa River below diversion near Hayden (site 5) by <br />reaeration in the approximately 16,3-mile reach down- <br />stream from the SSRWWTP and by dilution with <br />fresher water from the Elk River (site 4), However, the <br />relatively large pH value at site 5 (8,70) was elevated <br />by photosynthesis, as is indicated by oversaturation <br />with dissolved oxygen (124 percent) and undersatura- <br />tion with COl (69 percent) (fig, 5), <br /> <br />The Yampa River below Craig (site 6) is located <br />about 6.2 miles downstream from the outfall from the <br />Craig Waste Water Treatment Plant (CWWTP), This <br />facility discharges about 1.9 ft3/s of treated sewage <br />effluent during daylight hours (Robert Frazier, Craig <br />Waste Water Treatment Plant, oral commun" 2000), <br />At site 6, the effects of photosynthesis were only <br />slightly greater than at site 5, Measured pH increased <br />slightly to 8,80, the second largest measured value <br />(after site 3), whereas dissolved oxygen was slightly <br />more oversaturated (131 percent) and COl was more <br />undersaturated (59 percent) than at site 5 (fig, 5), The <br />relatively minor effects of photosynthesis on water <br />quality at site 6 compared to the effects at site 3 were <br />(at least partially) due to the larger dilution of sewage <br /> <br />INTERPRETATION OF DATA COLLECTED FOR THIS STUDY 9 <br />