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INTRODUCTION AND METHODS <br />The purpose of this report is to evaluate the physical, <br />chemical and biological characteristics of the Escalante Ranch <br />wetlands. This project is focused at determining how the <br />wetlands function at present, the history of these wetlands, and <br />the possibilities of using these wetlands for razorback sucker <br />habitat. <br />The studies reported here are original, based upon field and <br />laboratory analyses during June through September 1993. We <br />conducted investigations of site characteristics that would allow <br />us to determine if any problems existed which would make the site <br />suitable, or unsuitable for the fish recovery program. <br />We studied site history to understand the evolution of <br />landforms, hydrology, and vegetation over tiune. We examined <br />vertical aerial photographs obtained from the U.S. Soil <br />Conservation Service for the years 1937, 1952, 1954, 1961, 1980 <br />and 1987. A considerable amount of detail is visible on these <br />photographs, particularly how much land is dry vs wet and <br />distinctive vegetation patterns, such as the presence of <br />cottonwood trees. <br />For our hydrologic studies we established 4 staff gauges in <br />water bodies on site and also installed 7 ground water monitoring <br />wells. Wells were constructed of 1 inch PVC pipe. Holes were <br />hand augured to reach the water table. Our goal was to establish <br />wells which would allow us to determine the elevation of the <br />water table through our sample period. Machine slotted PVC pipe <br />was used in the lower portion of the well and unslotted PVC pipe <br />in the upper part. The well was capped on the bottom and top <br />ends and depth to water table was determined with a well-reader. <br />Surface and ground water levels were recorded regularly <br />during the sample period. Data on Green River stage was <br />determined at a staff gauge established by the Bureau of <br />Reclamation. River water levels are used to correlate with water <br />levels in the wetlands. This allowed us to determine whether <br />river and wetlands were hydrologically connected or whether the <br />wetlands are fed largely by another water source. The wells and <br />staff gauges also helped us to determine the duration of <br />inundation in wetlands. <br />Physical and chemical characteristics of water at staff <br />gauges (surface waters) and wells (groundwater) stations 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 and <br />the water ran clear. Surface and groundwater samples were <br />collected for chemical analysis from these same stations. For <br />1 <br />