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Last modified
7/14/2009 5:02:36 PM
Creation date
6/1/2009 11:56:52 AM
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UCREFRP
UCREFRP Catalog Number
9505
Author
Cooper, D. J. and C. Severn.
Title
Wetlands of the Escalante State Wildlife Area on the Gunnison River, Near Delta, Colorado
USFW Year
1994.
USFW - Doc Type
Hydrology, Water Chemistry, Vegetation, Invertebrate Communities, and Restoration Potential.
Copyright Material
NO
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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 />
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