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WSP05903
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Last modified
1/26/2010 2:20:25 PM
Creation date
10/12/2006 1:21:13 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8583
Description
Rio Grande Decision Support System
State
CO
Basin
Rio Grande
Water Division
3
Date
2/1/1998
Author
Dr. John W. Hernande
Title
Evaluation Of Salvage Well Production Problems In The Closed Basin Of The San Luis Valley Colorado
Water Supply Pro - Doc Type
Report/Study
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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 />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />00169,. <br /> <br />Siebenthal does not provide any extensive description of the nature of the fill in the <br /> <br /> <br />unconfined shallow aquifer that makes up the top 80 to 90 feet of the Closed Basin, He does <br /> <br /> <br />report on the Quaternary deposits as being comprised of sand dunes, alluvial fans, alluvium, and <br /> <br /> <br />alkali-lake deposits (USGS, 1910, page 47), One alkali-lake that he discusses is a one-acre lake <br /> <br /> <br />in the Bureau's Project area, just east of San Luis Lake (Section 30, T. 40 N" R. 12 E,),The lake <br /> <br /> <br />is described as being "practically solid crystallized sodium carbonate" from which the mineral <br /> <br /> <br />was harvested (USGS, 1910, page 50), <br /> <br /> <br />Water Quality in the Closed Basin Shallow Aquifer <br /> <br /> <br />The San Luis Valley probably had its origin as a depression of the earlier Santa Fe <br /> <br /> <br />formation and a "down warping" of its center to allow the formation of an extensive lake that <br /> <br /> <br />was subsequently filled by a series of depositions of clay and sand (USGS, 1910, page 52), <br /> <br /> <br />During dry periods this lake diminished in size and due to evaporation formed alkaline zones <br /> <br /> <br />where high total dissolved solids in the shallow ground-water is likely to be found today, The <br /> <br /> <br />lake evidently supported the growth of vegetation such as mosses and algae, resulting in the <br /> <br /> <br />deposition of organic matter in the valley fill, <br /> <br /> <br />While probably more representative of the artesian zones than the shallow aquifer, <br /> <br /> <br />Siebenthal reports that fresh-water shells, fish bones, bird bones, and bits of wood, roots, leaves, <br /> <br /> <br />seeds and peat-moss are recovered from wells all over the basin, This report of organic matter in <br /> <br />the artesian formations coincides with the finding of methane in the deeper wells, The contour <br /> <br />map in Siebenthal's report shows a closed loop that covers much of the Closed Basin as the area <br /> <br /> <br />where methane is found in Valley wells, The methane production area has a north-south length <br /> <br /> <br />of about 30 miles, and an east-west width of about 8 miles, split along the two sides of the trough <br /> <br /> <br />of the Valley (USGS, 1910, page 81), <br /> <br />10 <br />
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