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<br />(( <br /> <br />(( <br /> <br />l( <br /> <br />()j <br />- <br />r- <br /> <br />Hi <br /> <br />.~ p' <br /> <br />(~-I <br />~ <br />c::: <br /> <br />ABSTRACT <br /> <br />The purpose of the Phase II investigation of the Glenwood-Dotsero <br />Springs unit was to evaluate the feasibility of collecting saline <br />waters from the Glenwood and Dotsero Springs and piping these <br />waters to a series of evaporation ponds west of Mack, Colorado. <br />This plan was originally developed in the Phase I investigation <br />in which it was estimated that 13.8 mgd of saline waters could be <br />collected at the springs and piped to evaporation ponds covering <br />an area of approximately 5,700 acres for a period of 100 years. <br /> <br />'The Phase II investigation incorporates the findings of this <br />initial study into a more detailed investigation. This report <br />considers th€ influence of the geologic conditions at the Contour <br />Ponds Site on development of ponds for the evaporation of saline <br />water. The scope of the investigation included drilling <br />exploratory holes at 23 locations. Soil sampling, rock coring, <br />and permeability testing of surfical soils and bedrock were <br />performed. Selected samples were tested in the laboratory for <br />classification and to identify their recompacted engineering <br />properties. In addition, a geologic reconnaissance of the site <br />was performed. <br /> <br />The geologic conditions at the site, as determined from the <br />investigation, are characterized by shallow (2 to 31 feet thick) <br />Quaternary deposits overlying 500 to 1,400 feet of Cretaceous age <br />Mancos shale. The primary Quaternary deposits consist of <br />pediments (2 to 31 feet thick), alluvium, and alluvium-colluvium <br />mixed (1 to 10 feet thick), and residuum (0 to 4 feet thick). <br />With the exception of the more gravelly materials within the <br />pediments and less weathered residuum, all of the materials are <br />suitable for use as compacted clay liners. The permeability of <br />these materials when recompacted ranged from 3 x 10-7 to 2.2 <br />x 10-9 cm/sec (4.3 x 10-4 to 3.1 x 10-6 in/hr). Overall, <br />Overall, the materials do not have a high shrink-swell potential, <br />however, when designing liners consideration of their shrinkage <br />potential will be necessary. <br /> <br />On-site gravels within the pediment deposits are suitable for <br />bedding material for pipeline construction, but will require some <br />selective sorting. The soundness of the gravels is questionable <br />due to the presence of shale and therefore they probably cannot <br />be used as concrete aggregate. All near surface soils contained <br />high levels of soluble sulfates and use of Type V cement in <br />concrete used on-site will be necessary. <br />