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

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Matrix of<br />

Locations!') and Descriptions!') of Productive Zones of Brackish Groundwaters In Cameron and Hidalgo Counties, Texas<br />

Character of Hydrolo gic Unns Generalized <strong>Water</strong>- Projections of Recoverable Volumes<br />

System Series Formation Material Report: 316(» Bullet<strong>in</strong> 6014!') Bear<strong>in</strong>a Characteristics") Individual WeH Yields (gal/m<strong>in</strong>i Potential Supp~ Volumes<br />

Quality<br />

Considerations!')<br />

Not.,:<br />

Q Yields moderate to large For <strong>Lower</strong> <strong>Rio</strong> <strong>Grande</strong> No perennial yield data Is<br />

U Alluvial quantnies of fresh to slightly Groundwater Reservoir: presently avallabie <strong>for</strong> <strong>the</strong><br />

A Recent Deposits Sand Mercedes slightly sal<strong>in</strong>e water near overall study areas,<br />

T of <strong>the</strong> & Silt Sebastian <strong>the</strong> <strong>Rio</strong> <strong>Grande</strong> In Cameron Maximum Yield = although n has been<br />

E <strong>Rio</strong> <strong>Grande</strong> Shallow and Hidalgo Counties. 2900gpm estimated that <strong>the</strong> entire<br />

R Groundwater reseNOir would yield<br />

N Chlcot ReservOir Average Yletd = 75,000 acre-feet of water<br />

A Beaumont Mostly Clay AquWer 1200gpm per foot of drawdown of <strong>the</strong><br />

R Formation WlIhSome <strong>Lower</strong> water lable.!·)<br />

Y Pleistocene Sand & Silt <strong>Rio</strong> <strong>Grande</strong><br />

Groundwater Yields moderate to<br />

Rasarvolr large quantities of In that portion of <strong>the</strong> study<br />

fresh to moderataly<br />

area just wast of Brownsville,<br />

Ussle Clay, Sift, sal<strong>in</strong>e water. at least 350,000 acre-feet<br />

Formation Sand, Gravel, Unn-Faysvlne No available data <strong>for</strong> of fresh ~ slightly lal<strong>in</strong>e<br />

& Caliche Groundwater Mercedes Sebastian groundwater Is estimated<br />

Reservoir and Unn - Faysvlne to be In storage, and<br />

T & Groundwater Reservoirs computer Ilmulatloni have<br />

E Clay, Sand, Indicated that, by maln-<br />

R Sandstone, Evangel<strong>in</strong>e Yields moderate to la<strong>in</strong>lng a spac<strong>in</strong>g of 2000<br />

T Pliocene Goliad Mart, Caliche, AquWer large quantities of feet, a supply of 9-10 mgd<br />

I Formation Umestone, & tresh 10 slightly can be produced on a long<br />

A Conglomerate sallnewater term basis.!')<br />

R<br />

Y<br />

Mudstone, Yields moderate quantnles Maximum Yield =<br />

Miocene Oakville Claystone, Oakville Oakville of slightly 10 moderately 600gpm No available data.<br />

Sandstone Sandstone, Sandstone Sandstone sal<strong>in</strong>e water In north-<br />

Tull & Clay westem Hlldalgo County Average Yield =<br />

125 gpm<br />

(1) ReMr to Exha,it t •• '.prlnt of ~ from TWOS', Report 3'8 entitled Productive A, ... of <strong>the</strong> Malor SourcH of Groundwat., In <strong>the</strong> low.r Rto Granda v.ney<br />

(2) A lub.tantl,. part of th.ln<strong>for</strong>m •• on pr.anted In til_ matrix"" been taken from Tab .. , of TWOB', Report 318 .ntlled Stratigraphic and Hydrologic Section of !halo.., <strong>Rio</strong> Grand. Vall.yAr ••<br />

(3) Tok.n loom Tabl., 01 TWOa R.port No. 31 e<br />

Concentrations of<br />

silica (SIO,) In <strong>the</strong><br />

range of 30 to 50<br />

ppm have been<br />

ldentf18d In certa<strong>in</strong><br />

wells, and <strong>the</strong>se<br />

concentrations of<br />

silica could severely<br />

affect water recovery<br />

from <strong>the</strong> RO process.<br />

High suWate (SO.J<br />

concenlrations are<br />

also prevalent In<br />

some areas and could ,<br />

affect water recovery<br />

from both <strong>the</strong> EDR and<br />

RO processes.<br />

(4) Bued on lnbrmellon takan from Tax_ Bo.d 0' <strong>Water</strong> Enqlneel1l' Bullet<strong>in</strong> 8014 Voluma1<br />

(5) YJ.1dI of welts: .mall.

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