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

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1II-32<br />

2. Generally speak<strong>in</strong>g, <strong>the</strong> same areas from (1) are also underla<strong>in</strong> by very significant<br />

quantities of <strong>GP</strong>/<strong>GT</strong> fluids which are primarily useful as an energy source to power <strong>the</strong><br />

desal<strong>in</strong>ation systems, but could, if proven feasible, be converted to potable water via<br />

auto-desal<strong>in</strong>ation, most probably utiliz<strong>in</strong>g <strong>the</strong> MSF process.<br />

3. Because of <strong>the</strong> a<strong>for</strong>ementioned horizontal co<strong>in</strong>cidence of <strong>the</strong> two resources <strong>in</strong> most areas,<br />

coupled with <strong>the</strong> fact that <strong>the</strong> cost of desal<strong>in</strong>ation practically always <strong>in</strong>creases with<br />

<strong>in</strong>creas<strong>in</strong>g sal<strong>in</strong>ity levels, <strong>in</strong> <strong>the</strong> majority of applications <strong>the</strong> shallow brackish<br />

groundwaters aquifers should be utilized as <strong>the</strong> feed water sources, while utiliz<strong>in</strong>g <strong>the</strong><br />

<strong>GP</strong>/<strong>GT</strong> fluids to provide <strong>the</strong> necessary energy. A possible exception to this majority case<br />

could be <strong>the</strong> above mentioned area to <strong>the</strong> north and east of McAllen, which appears to<br />

be underla<strong>in</strong> by significant quantities of <strong>the</strong> <strong>GP</strong>/<strong>GT</strong> resource, but not significant quantities<br />

of mildly to moderately brackish groundwater <strong>in</strong> shallow aquifers. This m<strong>in</strong>ority area<br />

could prove to be a possible location <strong>for</strong> an auto-desal<strong>in</strong>ation application if certa<strong>in</strong><br />

conditions of feasibility are met.<br />

B. Availabiljtv and Characteristics of Si,"ificam Quantities of <strong>GP</strong>/<strong>GT</strong> Enera.<br />

!!a11J! of Section I of <strong>the</strong> write up <strong>for</strong> Task 2 is entitled Simulation of <strong>GP</strong>/<strong>GT</strong> Resource Potentia!, and<br />

it provides a substantial amount of <strong>in</strong><strong>for</strong>mation regard<strong>in</strong>g <strong>the</strong> projected availability and characteristics of<br />

<strong>the</strong> <strong>GP</strong>/<strong>GT</strong> energy available from <strong>the</strong> deep zones. Specifically, it presents such <strong>in</strong><strong>for</strong>mation <strong>for</strong> three<br />

different sand zones, one found <strong>in</strong> <strong>the</strong> Reservoir B Area and referred to here<strong>in</strong> as <strong>the</strong> East Sand, and two<br />

found <strong>in</strong> <strong>the</strong> Reservoir C Area, namely <strong>the</strong> Marks Sand and <strong>the</strong> Bond Sand. A summary of <strong>the</strong> pert<strong>in</strong>ent<br />

energy parameters <strong>for</strong> each sand, taken primarily from Figures 4-9 of Part B of Section I, and averaged<br />

over a projected productive life of 15 years, is presented as follows:<br />

East Sand Bond Sand Marks Sand<br />

Max M<strong>in</strong> Max M<strong>in</strong> Max M<strong>in</strong><br />

Br<strong>in</strong>e Production 25,000 25,000 24,900 23,500 14,750 14,125<br />

(Barre1s1Day)<br />

Gas Production 600 600 600 550 300 275<br />

(MSCF/Day)<br />

Wellhead Pressure 950 950 850 850 850 850<br />

(PSIA)<br />

Bottom Hole Temp. 264 264 296 296 279 279<br />

("F)<br />

Br<strong>in</strong>e Sal<strong>in</strong>ity 15,000 9,000 50,000 40,000 50,000 40,000<br />

(mg/l)

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