Geologic and Hydrogeologic Framework of Regional Aquifers in the Twin Mountains, Paluxy, and Woodbine Formations Near the SSC Site, North-Central Texas
Water-utility districts and many municipalities in North-Central Texas
recently obtained as much as 100 percent of their water supply from deep
regional aquifers in Cretaceous formations. Use of groundwater from the
aquifers during the past century has resulted in water-level declines of as
much as 850 ft (259 m), especially in Dallas and Tarrant Counties. Future
water-level changes will depend on the amount of groundwater produced to
help meet growing water-supply needs for municipalities, industries, and
agriculture throughout North-Central Texas. It is probable that a significant
part of the increased water demand will be met by groundwater although at
less than historic rates.
The objective of this study was to develop a predictive tool for studying
the effect of future groundwater production from regional aquifers in North-Central
Texas. To do this, we reviewed the history of groundwater
development, hydrogeology of the regional aquifers, and constructed
numerical models of groundwater flow. A cross-sectional model of both
aquifers and confining layers was used to evaluate model boundary
conditions and the vertical hydrologic properties of the confining layers.
Results and insights from the cross-sectional model were used in a three-dimensional
simulation of groundwater flow in the deep aquifers. The layers
of the regional confining system were not explicitly included in the three-dimensional
model. Hydrogeologic properties were assigned on the basis of
aquifer test results and stratigraphic mapping of sandstone distribution in the
aquifer units.Bureau of Economic Geolog