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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 />I <br />II <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />...~ <br /> <br />,.~) <br /> <br />1.0 INTRODUCTION <br /> <br />~ <br />C'J <br />(.:.:) <br />c-) As part of the Phase IB studies for the San Luis Valley Confined Aquifer <br />Study, the study team of HRS Water Consultants, Inc., and Robert Moran, has <br />performed analyses of selected data sets from the San Luis Valley. These data <br />sets analyzed were part of several earlier (Phase IA) investigations for the <br />Confined Aquifer Study, The analyses performed were as follows: <br />1. Analysis of deep-well aquifer test data <br />2. Analysis of deep-well geophysical logs <br />3. Analysis of satellite imagery of the Valley <br /> <br />The aquifer test data analyzed were acquired during the summer of 1986 as <br />part of the Phase lA, Task 5 activities. Three deep confined aquifer wells <br />(the Hooper Pool Well, the Carroll Well, and the Owens Well) were tested at <br />that time. The Owens Well did not yield usable data, due to background noise <br />problems with constant use of the well. The Carroll Well and the Hooper Pool <br />Well yielded transmissivity estimates on the confined aquifer, but, due to <br />well construction, it is felt that the estimates are more representitive of <br />HSU-2 than of HSU-3. <br /> <br />Geophysical logs were run in the Hooper Pool Well, the Carroll Well, and <br />the Alamosa Geothermal Well. The logging probes could not penetrate below a <br />depth of about 280 feet in the Hooper Pool Well, due to the condition of the <br />well. The Carroll Well and the Alamosa Geothermal Well both were logged to <br />their total depths (2620 feet and 6075 feet, respectively). Both wells yielded <br />logs which have been useful in determining the hydrologic, lithologic, and <br />thermal properties of the confined aquifer. <br /> <br />Also included in this report is an interpretation of geological and <br />geophysical data from a new oil test well, No. 1-19 San Francisco Creek, <br />located about five miles south of Del Norte, The data from this new test well <br />were obtained through a data exchange agreement between the Colorado Water <br />Resources and Power Development Authority (through HRS Water Consultants, <br />Inc.) and Waggoner-Baldridge Energy Co. of Dallas, Texas. <br /> <br />1-1 <br />