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<br />0023 <br /> <br />DISCUSSION <br /> <br />The primary objectives of the study were to <br />identify the types and abundance of aquatic <br />macrofauna in the upper Arkansas River and to <br />determine the effects of heavy metals pollution <br />on macrofauna distribution. Physical parameters <br />of the river water that were considered included <br />temperature, current, substrate, conductivity, <br />and oxidation-reduction potential. Chemical <br />parameters included pH. dissolved oxygen. ma- <br />jor anion and cation content, nitrogen and phos- <br />phorus compounds, and the selected heavy <br />metals manganese. iron, copper. zinc, lead, <br />molybdenum, and cadmium. The macrofauna <br />represented were considered with respect to <br />their physical and chemical tolerances. <br /> <br />Temperature <br /> <br />Water temperature generally increased down- <br />stream from stations EF-l to AR-9. Also, at any <br />given station temperature increased throughout <br />the year until late summer. Low, shallow flows. <br />warm tributaries, and the relative absence of <br />shade would account for higher temperatures <br />reached during the late summer. An increase in <br />temperature is usually correlated with an in- <br />crease in numbers and diversity of aquatic in- <br />vertebrates (Armitage, 1958 [4J l. The results <br />of this study did not totally support these find- <br />ings due to the variations in water quality. Tem- <br />peratures found were acceptable for the survival <br />of brown, brook, and rainbow trout, as well as <br />longnose and white suckers (Scott and <br />Crossman. 1973 [136]. ). <br /> <br />Dissolved Oxygen (D.O.) <br /> <br />Dissolved oxygen concentrations at all stations <br />in the upper Arkansas River were greater than <br />90-percent saturation and on occasion slightly <br />exceeded 100 percent. These levels of dissolv- <br />ed oxygen would provide suitable conditions for <br />aquatic macro invertebrates and fish. Therefore. <br />oxygen was not a limiting factor. <br /> <br />pH <br /> <br />The pH in the river throughout the study indi- <br />cated the water was slightly alkaline. and was <br /> <br />generally higher during the late summer and fall <br />when primary production was greatest. ThiS <br />higher pH was also reflected in a higher total <br />dissolved solid (TDSI concentration. The pH was <br />nearly always within a range considered op- <br />timum for fish production and for the survival of <br />most aquatic macroinvertebrates. McKee and <br />Wolf (19631 [1 05J cited data that indicate that <br />the upper pH limit for trout is 9.2. This level was <br />reached on one occasion at AR-3 due to the in- <br />fluence of California Gulch, and may be a reason <br />why no fish were collected at this station. <br />However. this high reading may have been In <br />error due to interference by overhead power <br />lines which may have affected the electronics in <br />the meter. The pH values generally found in the <br />river throughout the study indicated that most of <br />the heavy metals would likely not be in a highly <br />toxic ionic form. <br /> <br />Conductivity <br /> <br />The conductivity of the river water was always <br />at a level conducive to supporting fish and <br />aquatic macroinvertebrates. The Leadville Drain <br />and California Gulch had conductivity values <br />considerably higher than the river, but levels <br />lower than those that would likely cause an <br />osmotic imbalance in aquatic organisms (McKee <br />and Wolf, 1963 [1051). Conductivity was <br />generally highest during the low flows of late fall <br />and winter due to high concentrations of <br />dissolved solids, and lower during the high flows <br />of spring and summer because of the dilution ef- <br />fect of snowmelt. <br /> <br />Oxidation-Reduction Potential (Ehl <br /> <br />A moderately low pH and a reducing environ- <br />ment generally favor the bioavailable soluble and <br />exchangeable chemical forms of metals, while <br />soluble metal oxides and hydroxides predom- <br />inate at higher pH and oxidation levels (Gambrell <br />et aI., 1976 [60J I. All Eh values measured dur- <br />ing the study would indicate that the river was in <br />an oxidized state except during periods of late <br />winter. Eh corrected to E, measurements show <br />that. on occasion. reducing conditions existed in <br />California Gulch, which resulted in lower Eh <br />values at AR-3. <br /> <br />33 <br />