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<br />~SGS <br /> <br />Concentrations of nitrogen and phosphorus were measured during the summer <br />of 1985 at multiple locations and depths in the reservoir. Total-nitrogen <br />concentrations at Pueblo Reservoir ranged from less than 0.2 to 1.2 mg/L and <br />had an average concentration of 0.6 mg/L. The predominant nitrogen form was <br />organic nitrogen, which, as in the Arkansas River, comprised about 60 percent <br />of the total nitrogen. The average total-inorganic-nitrogen concentration <br />near the reservoir surface was about 0.2 mg/L; near the reservoir bottom, the <br />average concentration was about 0.3 mg/L. Concentrations of total phosphorus <br />ranged from less than 0.01 to 0.05 mg/L near the reservoir surface and ranged <br />from less than 0.01 to 0.22 mg/L near the reservoir bottom. Concentrations of <br />total phosphorus were largest near the reservoir bottom. <br /> <br />Concentrations of major ions in samples collected near the reservoir <br />bottom at transect 2 varied greatly during the summer of 1985, whereas the <br />concentrations of the ions changed very little in samples collected near the <br />reservoir surface at transect 7 (nearest the dam) during the summer of 1985. <br />Variations in ion concentrations were consistent with changes in specific <br />conductance that occurred with depth and demonstrate the effects of chemical <br />stratification and inflow on concentrations of specific ions. Dissolved- <br />solids concentrations at the Arkansas River at Portland, as indicated by <br />specific-conductance measurements, usually are largest from January to March <br />and smallest during June and July. <br /> <br />Concentrations of most trace elements generally were small and were less <br />than the established water-quality standards for Pueblo Reservoir. However, <br />in 1985, concentrations of total iron occasionally exceeded the aquatic-life <br />standard (1,000 ~g/L) near the reservoir bottom at transect 2, and dissolved- <br />manganese concentrations exceeded the standard for public water supply near <br />the reservoir bottom at transect 2. Trace elements that occurred in the <br />largest concentrations at the Arkansas River at Portland are barium, iron, <br />manganese, strontium, and zinc. Trace elements primarily occur in association <br />with suspended material. <br /> <br />Diatoms, green algae, blue-green algae, and cryptomonads comprised the <br />majority of the phytoplankton in Pueblo Reservoir in the summer and fall of <br />1985. The maximum average concentration of phytoplankton was 41,000 cells/mL <br />and occurred in July. Blue-green algae dominated from June to September; <br />diatoms dominated in October. The average concentrations of phytoplankton <br />drastically decreased from July to October. Zooplankton densities ranged from <br />a few thousand organisms/m3 at transects 1 and 2 to about 80,000 organisms/m3 <br />at transect 5 during August. <br /> <br />A list of potential inbasin contaminants and transportation-related <br />contaminants was compiled and included in the section in the back of the <br />report titled "Supplemental Information Related to Potential Contaminants to <br />Pueblo Reservoir." Currently (1986), the greatest threat of contamination in <br />the upper Arkansas River basin probably is from metal mines that discharge to <br />the streams in the vicinity of Leadville. Flammable liquids, combustible <br />liquids, and flammable gases accounted for 71 percent of the hazardous mater- <br />ials and 71 percent of the loads terminated in Colorado. Flammable liquids, <br />combustible liquids, corrosives, oxidizers, and petroleum materials frequently <br />are transported by rail. Depending on the specific compounds, location, and <br />quantity of material spilled, a spill could pose a threat to the quality of <br />water in Pueblo Reservoir. <br /> <br />48 <br />