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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />II <br />I <br />I <br />I <br />I <br />I <br />II <br />I <br />I <br /> <br />0") <br />) <br /> <br />r- <br />C"J <br /> <br />2.0 DEEP-WELL TESTING AND LOGGING <br /> <br />{:::J <br /> <br />;~,;l <br /> <br />2.1 INTRODUCTION <br />Aquifer testing and geophysical logging of four confined-aquifer wells <br />was performed and supervised by members of the Phase IA study team during the <br />week of August 24, 1986. The logging and testing was performed on wells <br />selected during the deep-well inventory part of the confined aquifer study <br />(see Interim Task 2 Report, this study). The four wells, which are depicted <br />on Figure 2.1, are as follows: <br />1. Hooper Pool Well (reported total depth of 4308 ft.) <br />2. Carroll Well (reported total depth of 2585 ft.) <br />3. Owens Well (reported total depth of 3080 ft.) <br />4. Alamosa Geothermal Well (reported total depth of 6084 ft.) <br /> <br />The purpose of the logging and testing was to supplement the existing <br />database regarding the aquifer characteristics and water quality of the deep <br />confined aquifer, particularly hydrostratigraphic unit 3 (HSU-3). <br /> <br />Flow tests and/or shut-in tests were performed on the Hooper Pool Well, <br />the Carroll Well, and, to a limited extent, the Owens Well. The Alamosa <br />Geothermal Well was not tested, because it does not flow, and because it is <br />doubtful whether a pumping test of that well would yield reliable aquifer <br />parameters due to indications of inadequate well development following <br />drilling and well completion. <br /> <br />Geophysical logs were run in the Carroll Well and the A1amosa Geothermal <br />Well. No logs were run in the Owens Well, due to its proximity (1880 feet) <br />to the Carroll Well, and because logging would have caused several dozen homes <br />and businesses to be without water for the duration of the logging. An <br />attempt to log the Hooper Pool Well was only marginally successful due to <br />problems with the condition of the well. <br /> <br />2-1 <br />