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establish wells which would allow us to determine the elevation <br />of the water table through the sample period. Machine slotted <br />PVC pipe was used in the lower portion of the well and unslotted <br />PVC pipe in the upper part. The well was capped on the bottom <br />and top ends and depth to water table was determined with a well- <br />reader. <br />Surface and ground water levels were recorded regularly <br />during the sample period. Data on Gunnison River stage was <br />derived from the Whitewater gauge located downstream from the <br />study area. River water levels from our staff gauge 7 are used <br />to correlate with water levels in the wetlands. This correlation <br />allowed us to determine whether river and wetlands were <br />hydrologically connected or whether the wetlands are fed largely <br />by another water source. The wells and staff gauges also helped <br />us to determine the duration of inundation in wetlands. <br />Physical and chemical characteristics of water at staff <br />gauges (surface waters) and in wells (groundwater) were <br />determined in the field and laboratory. We determined pH, <br />conductivity, DO and temperature at sample times using a ICM <br />water analyzer Model 51601. For well samples, water was pumped <br />using a hand pump, until several well volumes had been removed <br />and the water ran clear. Surface and ground water samples were <br />collected for chemical analysis from these same stations. For <br />surface water and ground water collections, samples were filtered <br />through a 0.45 micron filter, and split into subsamples, one of <br />which was acidified using nitric acid, and one of which was <br />unacidified. Water .samples were kept cold until transfer to the <br />Denver Office Chemistry and Petrography Laboratory of the Bureau <br />of Reclamation. <br />The analyses were carried out under the supervision of Doug <br />Craft. Acidified samples were analyzed using inductively coupled <br />plasma spectrometry for the following metals; V, Si, Zn, Sb, Ag, <br />A1, As, B, Ba, Be, Cd, Co, Cr, Cu, Fe, Li, Mn, Mo, Pb, Ca, Na, <br />Mg, and K. In addition, Se (selenium} was determined using <br />graphite furnace atomic absorption spectrometry by Barringer <br />Laboratories in Golden, CO. Unacidified samples were analyzed <br />for HCO'3, SOZ'4, and Cl', along with alkalinity, lab conductivity, <br />lab pH, and TDS. <br />The water chemistry data are used for two purposes; (1) to <br />determine if any element occurs in concentrations that could be <br />of biological importance to razorback suckers, and (2) to help <br />identify distinct water sources feeding the wetlands. Water <br />quality standards published by the State of Utah are used in this <br />report as guidelines for elemental concentrations that exceed the <br />numeric criteria for aquatic life (State of Utah 1993). <br />Vegetation patterns were determine to allow us to analyze <br />the major aquatic habitats in the study area wetlands. Five <br />2 <br />