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Last modified
1/26/2010 3:19:26 PM
Creation date
10/12/2006 5:19:14 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
1/1/1996
Author
U.S. Geologic Survey
Title
Plan Of Study To Quantify The Hydrologic Relations Between The Rio Grande And Santa Fe Group Aquifer System Near Albuquerque/ Central New Mexico
Water Supply Pro - Doc Type
Report/Study
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<br /> Table 3.-SUIIlII\ary of properties that influence ground~water production potenticU of Santa Fe Group lithofacies <br /> (modifil!cl from Iiawley apd Haase, 1992) <br /> [>, greater than; <<., less than] 0 <br /> r-..... <br /> . nRatio of I-" <br /> sand plus gravel Bedding Bedd" Bedding Beddin Hydraulic Ground-water C") <br /> .. mg g ,-.J <br /> Lithofacies to sili plus clayl thickness (feet) configuration2 continuity (feet)3 connectivity" conductivity production potential tv <br /> I High to moderate >5 Elongate >500 High !:Iigh to moderate High to moderate <br /> Iv High to m!Xlerate >5 Elongate >500 High Higlt to moderate High <br /> Ib H" h >5 Elongate >500 High . High High <br /> tg <br /> II High to moderate >5 Elongate >500 Moderate to I1igh High to moderate High to moderate <br /> III Low lto5 Pl(U1~:r >?OO Low u,w Low <br /> IV Low to mQderat~ 1to5 Planar to elol)gate. 100 to SOO u,w to moder;lte Moderate to low Moderate to low <br />..... V Moderate 1105 Elongate to lobate 100 to ?OO Moderate to high MOderate Moderate <br />0\ <br /> Vf Moderate 1105 Elol)gate to lobate 100 to 500 Moderate Moder~te to low Moderate to low <br /> Vd Moderate to high >5 IJlongate to lobate 100 to 500 High Moderat~ to high Moderate to high <br /> VI High >5 Lobate <100 Moderate Moperate to high Moderate <br /> VII Moderate lto5 Elol)gate to lobate 100 to 500 Moder~te to higil MO<ierate to low Moderate to low <br /> VIII High >5 Lobate <;100 Moderate Moderate to low Moderate to low <br /> IX Low <1 Planar >500 u,W Low Low <br /> X Low <;1 Planar >500 Low Low Low <br /> <br />llligh >2; moderate 0,$-2; low <0.5. <br />2Elongate (length to width ratios >5); planar (length to width ratios I "5); lobate (asymmetricl!l or incomplete planar beds), <br />3Measure of tIie lateral extent of an individual bed of given thigkness and config1lIlition, . <br />"Estimation of the ease with which ground water can flQw betw(:en individual beds within a Pwticular lithofacies. Generally. high sand + gravel/silt + <br />- - --. - - . <br />clay ratios, thick beds, and high bedding continuity favor high bedding <:pnnectivity. All other parameten; being equal, the greater the bedding <br />connectivity, the greater the grpund-water production potential of a sedimentary unit (Hawley and Haase, 1992, p. VI). <br />
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