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(GP/GT) for Additional Water Supply in the Lower Rio Grande

(GP/GT) for Additional Water Supply in the Lower Rio Grande

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1-3<br />

C. SUMMARY AND CONCLUSIONS<br />

The pert<strong>in</strong>ent results of <strong>the</strong> Co-Location Studies <strong>for</strong> Cameron and Hidalgo Counties are presented on <strong>the</strong><br />

enclosed Figures 1 and 2, respectively; <strong>the</strong>se be<strong>in</strong>g compilations of <strong>the</strong> various overlays.<br />

1. The occurrences of brackish groundwaters at shallow depths are extensive enough so that<br />

choices of locations will not be unduly constra<strong>in</strong>ed<br />

2. Prelim<strong>in</strong>ary screen<strong>in</strong>g of <strong>the</strong> <strong>GP</strong>/<strong>GT</strong> Resource occurrences has revealed that area A <strong>in</strong><br />

<strong>the</strong> Rodgers Map, already extensively studied <strong>in</strong> <strong>the</strong> previous USDOE <strong>in</strong>vestigation<br />

referred to above, should not require fur<strong>the</strong>r study. Area D of <strong>the</strong> Rodgers Map is also<br />

shown to be less desirable from <strong>the</strong> standpo<strong>in</strong>t of both <strong>the</strong> extractable heat energy and <strong>the</strong><br />

water quality. Thus, it is concluded that Areas B and C of <strong>the</strong> Rodgers Map are those<br />

that clearly merit fur<strong>the</strong>r study <strong>in</strong> <strong>the</strong> Resource Assessment portion of this <strong>in</strong>vestigation<br />

and will be those on which we will concentrate hence<strong>for</strong>th<br />

3. A sufficiency of population densities appears to overlie - or be <strong>in</strong> close proximity to -<br />

both shallow groundwater and deep <strong>GP</strong>/<strong>GT</strong> sources to enable promis<strong>in</strong>g utilization of<br />

<strong>the</strong>se resources <strong>in</strong> <strong>the</strong> future.

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