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

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The feasibility of utiliz<strong>in</strong>g geopressured resources to produce<br />

potable water by desal<strong>in</strong>ation appears to have high near-term probability<br />

of successful application, especially <strong>in</strong> areas of limited water supplies<br />

such as <strong>the</strong> lower <strong>Rio</strong> <strong>Grande</strong> Valley region of south Texas, and <strong>the</strong><br />

central valley of Cali<strong>for</strong>nia.<br />

Studies made by Dorfman and o<strong>the</strong>rs dur<strong>in</strong>g <strong>the</strong> early program years of<br />

<strong>the</strong> geopressured program <strong>in</strong>dicate <strong>the</strong> Hidalgo county geopressured<br />

reservoir could susta<strong>in</strong> a br<strong>in</strong>e flow of 16,830,000 bpd without undue<br />

depletion over a 20 year life, and a br<strong>in</strong>e flow of 45,600,000 bpd is<br />

estimated <strong>for</strong> Cameron and Hidalgo Counties (Dorfman and Morton, 1985).<br />

After salt removal, -1.15 billion gal/d of desal<strong>in</strong>ated water could be<br />

recovered <strong>in</strong> a region that is characteristically low <strong>in</strong> water supplies<br />

(Spencer, 1990).<br />

Both of <strong>the</strong>se areas have geopressured bas<strong>in</strong>s that have <strong>the</strong> potential<br />

to be utilized <strong>for</strong> desal<strong>in</strong>ation. See Figure 6 <strong>for</strong> <strong>the</strong> approximate<br />

location of <strong>the</strong> Sacramento Valley, San Joaqu<strong>in</strong> Valley, and Los Angeles<br />

Bas<strong>in</strong>s <strong>in</strong> Cali<strong>for</strong>nia, and <strong>the</strong> Nor<strong>the</strong>rn Gulf of Mexico Bas<strong>in</strong> <strong>in</strong> Texas. As<br />

reported by <strong>the</strong> Department of <strong>Water</strong> Resources, State of Cali<strong>for</strong>nia, <strong>in</strong><br />

<strong>the</strong>ir drought Cont<strong>in</strong>gency Plann<strong>in</strong>g Guidel<strong>in</strong>es <strong>for</strong> 1989, Cali<strong>for</strong>nia<br />

realized a $2.4 billion loss <strong>in</strong> <strong>the</strong> drought of 1976 to 1977, and <strong>the</strong><br />

current drought is worse. The suggestions <strong>for</strong> deal<strong>in</strong>g with <strong>the</strong> drought<br />

are all conventional (more surface reservoirs, water purchases from<br />

surround<strong>in</strong>g states, etc.) Also, grandiose schemes such as digg<strong>in</strong>g a<br />

canal to <strong>the</strong> Columbia River and mov<strong>in</strong>g icebergs from Antarctica are be<strong>in</strong>g<br />

suggested by <strong>the</strong> City of Los Angeles. The Seattle Times, May 27, 1990,<br />

notes that under a scheme called <strong>the</strong> North American <strong>Water</strong> and Power<br />

Alliance, <strong>the</strong> Ralph Parsons Co., Pasadena, CA has developed a gigantic<br />

water-transfer plan that <strong>in</strong>cludes waterways snak<strong>in</strong>g down <strong>the</strong> cont<strong>in</strong>ent<br />

from Alaska, through Canada and <strong>the</strong> Northwest, to serve <strong>the</strong> freshwater<br />

needs of sou<strong>the</strong>rn Cali<strong>for</strong>nia. The estimated cost is $200 billion. By<br />

contrast, Nitschke and Harris'(1990) proposed system would provide -40%<br />

of Cali<strong>for</strong>nia's water demand at a cost of -$24 billion (Table 1). This<br />

approach would <strong>in</strong>clude us<strong>in</strong>g geopressured resources found <strong>in</strong> <strong>the</strong><br />

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