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<br />1 <br /> <br />the land within project boundaries in 1977, which indicated about 40,000 acres <br />of wetlands were within the 138,500 acres of project-included lands. <br /> <br />1 <br /> <br />More detailed studies indicated that between 26,000 and 47,000 acres of wetlands <br />and wetland habitat were present depending on the year the analysis was made. <br />The primary difference between these two wetland acreages was in the delineation <br />of ephemeral wetlands. <br /> <br />J <br /> <br />I <br /> <br />In 1978 the FWS initiated the National Wetlands Inventory for the San Luis <br />Valley and Closed Basin Division wetlands under a memorandum of agreement with <br />the Bureau. The inventory indicated that 43,122 acres of wetlands were present <br />within the proposed project boundary. These wetland acreages are similar to <br />those of the Bureau studies and have been accepted for use in this supplemdnt. <br /> <br />I <br /> <br />Wetlands and wetland habitat in some parts of the project will be affected where <br />existing ground water tables are less than 2-1k feet. Lowering of the water <br />table through pumping of the unconfined aquifer will alter existing vegetation. <br />An increase in loss of free-standing water due to seepage could also occur in <br />some areas. <br /> <br />I <br /> <br />I <br /> <br />Map overlays of the top of the unconfined aquifer in relation to the natural <br />ground surface were developed for 1978-1980 using ground water depth readings <br />from observation wells scattered throughout the project. Ground water table <br />maps of this nature were used to determine the potential effects of lowering the <br />water table on existing vegetation and general location of wetlands and wetland <br />habitats. These overlays also indicated the seasonal variation in water tables <br />and the general trend toward deeper water tables. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Readings from about 60 observation wells were used. The shallowest and greatest <br />readings, regardless of date, during a given year were plotted on overlays on <br />USGS 7.5-minute topographic bases. In general, the shallowest water table <br />depths occurred during late winter and spring before the growing season and <br />increased total evapotranspiration, while the greatest water table depths <br />occurred in the late summer and fall. <br /> <br />I <br /> <br />I <br /> <br />Using data supplied by the Bureau, the USGS conducted computer modeling analysis <br />of the Closed Basin to develop the well field systems to be installed for proj- <br />ect pumping. The analysis also provided estimated drawdown of the existing <br />unconfined aquifer in 2-foot increments within the project boundaries after more <br />than 50 years of pumping. <br /> <br />I <br /> <br />2. Effects. <br />8,460 of the existing <br />ect boundaries. <br /> <br />Construction and operation of the project will affect <br />43,122 acres of wetlands (wetland habitats) within proj- <br /> <br />I <br /> <br />I <br /> <br />An overall reduction of total plant (biomass) production may occur in wetlands <br />which are located over shallow water tables of 5 feet or less below the natural <br />ground surface. Also, the retention time of spring surface snowmelt runoff in <br />wetlands that normally receive annual runoff may be decreased. Lowering the <br />shallow water table beneath these wetlands could result in an increased soil <br /> <br />I <br /> <br />I <br /> <br />f <br /> <br />...._./1 /"\ _...", <br />( .l;J'J <br />~j . 4>-- <br /> <br />I <br /> <br />I <br />