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<br />Station AR-6 is about 100 m downstream of a <br />wooden bridge on the Pan-Ark property just east <br />of U.S. Highway 24. Sand and 31- to 119-mm- <br />diameter gravel and rubble compose most of the <br />substrate. <br /> <br />Station AR-7 is located about 200 m below the <br />inflow of Box Creek from the west. The river <br />parallels the railroad track in this area and has <br />been channelized. Steep bluffs confine the river <br />to a relatively deep, narrow channel. Sampling <br />was done in a riffle area of the river containing <br />primarily 30- to 148-mm-diameter gravel and <br />rubble. <br /> <br />Station AR-8 is immediately upstream of the <br />confluence with Lake Creek. This river section <br />also appears to have been channelized and the <br />channel is deep and narrOW. Large boulders <br />were present along the river's edge. Most of the <br />substrate sampled consisted of 81- to 291-mm- <br />diameter rocks. <br /> <br />Station AR-9 is located 0.8 km below the Lake <br />Creek inflow. Varying flows from Twin Lakes via <br />Lake Creek result in widely fluctuating flows at <br />this station in the Arkansas River. Lake Creek in- <br />flows usually freshen the Arkansas River consid- <br />erably at this station. The substrate consists pri- <br />marily of 42- to 139-mm-diameter gravel and <br />rubble. <br /> <br />Data Collection and Sampling Techniques <br /> <br />Data collection and sampling were done ap- <br />proximately twice monthly from March through <br />November 1979 and four times from April <br />through September 1980. On each sampling <br />date, physical water parameters were measured <br />and water samples for chemical analyses were <br />collected. Macroinvertebrate samples to deter- <br />mine density and diversity were collected at all <br />times except during the first and last surveys of <br />1979, during which slush and ice in the river <br />would not allow accurate sampling. Fish popula- <br />tion estimates were done by collecting fish at <br />selected stations during a low-flow period in the <br />fall of 1979 using a battery-operated backpack <br />electrofishing unit. Fish liver samples for <br />analysis of heavy metal content were later ob- <br />tained from these collections. In addition, on one <br />occasion during the fall of 1979, physical water <br />quality parameters were measured and water <br />samples for chemical analyses were collected <br />from four significant tributaries to the upper <br />Arkansas River. <br /> <br />The field parameters measured during this study <br />were temperature, dissolved oxygen, conduc- <br />tivity, pH, and oxidation-reduction potential. <br />These parameters were measured with a Hydro- <br />lab Corporation Surveyor multipara meter probe <br />(fig. 4) IHydrolab, 1972 1821). East Fork and <br />California Gulch flows were measured with a <br />Price current meter (fig. 5) and staff gages, <br />using techniques developed by the Bureau of <br />Reclamation 11967) 117]. Major Arkansas River <br />flows were obtained -from U.S. Geological <br />Survey and State of Colorado stream gaging sta- <br />tions. <br /> <br />Polyethylene plastic bottles were used to collect <br />all water samples. One-liter samples of water <br />were collected and refrigerated for major cation- <br />anion analyses. A 150-mL bottle was used to <br />collect water for the analyses of various heavy <br />metals. Approximately 1 mL of nitric acid was <br />added to the heavy metals samples to lower the <br />pH to less than 2.0 to maintain the metals in <br />solution. Thus, analytical results reflect the total <br />metal concentrations. Five-hundred-mL samples <br />of water were collected and frozen for analyses <br />of phosphorus and nitrogen compounds. <br /> <br />The substrate was measured on one sampling <br />date. The smallest diameter of the smallest sur- <br />face stone and the largest diameter of Ihe <br />largest stone within the enclosed area of three <br />Surber samples were m~"sured. This described <br />the ranges of substrate sizes at each station. <br /> <br />The macroinvertebrate community was sampled <br />using a Surber sampler (fig. 61. A description of <br />this sampler can be found in Welch 119481 <br />1163]. According to Cummins (1962) [31]. <br />the Surber sampler is the most widely accepted <br />macroinvertebrate sampler, particularly in <br />waters of less than 300-mm depth with <br />moderate flow. The sampler consists of two <br />nesting 300-mm-square brass frames attached <br />on one side to form a 900 angle when opened. <br />An attached conical net made of 1 -mm mesh is <br />attached to the vertical frame. The sampler is <br />placed on the stream bottom with the open end <br />of the conical net facing upstream. All substrate <br />within the 0.09 m' area defined by the <br />horizontal frame is washed by hand in front of <br />the open net. The current carries any dislodged <br />organisms into the net. Even though the opera- <br />tion of this sampler has some disadvantages, <br />such as the collection of drifting organisms, the <br />limitation to relatively shallow water, the dif- <br /> <br />16 <br />