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Last modified
1/26/2010 3:19:34 PM
Creation date
10/12/2006 5:20:57 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8509
Description
San Luis Valley
State
CO
Basin
Rio Grande
Water Division
3
Date
8/10/1987
Title
San Luis Valley Confined Aquifer Study (Phase I) Final Report
Water Supply Pro - Doc Type
Report/Study
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<br />I <br /> CJ <br />I f'- <br />f'o. <br /> N <br />I (~, <br />(...,~ <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 />evaluation shows a layered sequence of unconsolidated sedimentary deposits <br />with extensive faulting within and surrounding the Valley'arising from several <br />sets of forces acting over different periods of geologic time. <br /> <br />The complexity of the geologic structure has led the study team to the <br />conclusion that any ground water flow modeling of the Valley would depend on <br />estimates of physical parameters that are highly subjective, and that appear <br />to be highly variable in different parts of the Valley. Thus, any Valley-wide <br />modeling results with existing data would almost certainly be subject to <br />significant changes as more data becomes available in the future. <br /> <br />In summary, the study team concludes from the Phase I studies that it is <br />not economically feasible to develop water for irrigation from the deep (below <br />3000 feet) confined aquifer due to relatively low transmissivity and <br />unacceptably poor water quality for the intended uses. For the shallow <br />confined aquifer between approximately 1000 and 2500 feet, it is concluded <br />that development of supplemental water for irrigation would not be <br />economically feasible at this time. <br /> <br />For the confined aquifer, no definite conclusions can be reached from the <br />Phase I studies regarding the institutional issues of tributariness of the <br />confined aquifer system in the Valley and the potential for injury to existing <br />water rights which may result from development of those aquifers. <br /> <br />The recommendations presented below follow from the study team's Phase I <br />studies of the deep confined aquifer of the Valley, and are based on the <br />conclusions presented in the preceding part of this summary. These <br />recommendations also recognize that the primary function of the Authority is <br />to finance economically-feasible water-development projects. <br /> <br />RECOMMENDATIONS <br />The first r.e~tlr:tga,ti~D~!lL!1!!LfMs.e-U.j;Y91!:.s...~i.s that the Phase II <br />_ ' _'_'.,_.J~'_~___",,__, 'm _ . <br />,i.~.~~.i-tLgs'l.iQn_.as---'trigi na.l.1 yem:isio.ned,.~in-"'QIVitl.Q.JJ1:ill.iJlg,}I.Q5!...!~~n~i.,o!~.e,~p:: <br />ml~....s.b.aJJJJL.nQ.Lb.e.j,nJt:i4j;~JL!Ltl1is, tjm~. This recommendation is based on <br />the conclusion that it is not presently economically feasible to implement a <br /> <br />$-6 <br />
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