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Laura M. Bexfield

Publications and source records attributed to Laura M. Bexfield.

40 records · Page 3Linked to original sources

Estimated water-level declines in the Santa Fe Group aquifer system in the Albuquerque area, central New Mexico, predevelopment to 2002

In the Albuquerque metropolitan area of central New Mexico, residential water-supply requirements have historically been met almost exclusively by ground-water withdrawal from the Santa Fe Group aquifer system. The rapid population growth of the metropolitan area from about 262,200 residents in 1960 (Karen D. Thompson, U.S. Census Bureau, written commun., 2002) to about 712,700 residents in 2000 (U.S. Census Bureau, 2001) has resulted in a large increase in the number of municipal-supply wells operated in the region and the total quantity of water they withdraw per year. The largest municipal supplier is the City of Albuquerque, which delivered about 35.8 billion gallons of water to approximately 450,000 people during 1997 (files of the City of Albuquerque) and operates more than 90 municipal-supply wells. Other nearby important suppliers include the City of Rio Rancho and the Town of Bernalillo. The large quantity of ground-water withdrawal in the Albuquerque metropolitan area relative to ground-water recharge has resulted in water-level declines in the Santa Fe Group aquifer system across much of the region. Analysis of the magnitude of and patterns in water-level declines can improve understanding of how the ground-water system responds to withdrawals and how the system might be managed in the future to minimize water-level declines and operating costs of water suppliers.

Water-Resources Investigations Report↗

Predevelopment water-level map of the Santa Fe Group aquifer system in the middle Rio Grande basin between Cochiti Lake and San Acacia, New Mexico

Because of its increasing population and limited water resources, the Middle Rio Grande Basin between Cochiti Lake and San Acacia, New Mexico, has recently become the subject of intense study. In particular, the U.S. Geological Survey (USGS) in cooperation with the City of Albuquerque has constructed a series of ground-water-flow models of the Tertiary and Quaternary basin-fill deposits of the Santa Fe Group aquifer system (Kernodle and Scott, 1986; Kernodle and others, 1987; Kernodle and others, 1995; Kernodle, 1998; Tiedeman and others, 1998). The ground-water-flow system also has been the focus of hydrochemical studies and other efforts intended largely to help develop an improved flow model. Among the information critical to a thorough understanding of the ground-water-flow system are water-level data that indicate the directions of ground-water flow and the magnitudes of hydraulic gradients in the aquifer prior to perturbation by substantial ground-water withdrawals (under predevelopment conditions).

Water-Resources Investigations Report↗

Summary of water-quality data for City of Albuquerque drinking-water supply wells, 1988-97

The City of Albuquerque has collected and analyzed more than 5,000 water-quality samples from 113 water-supply wells in the Albuquerque area, including many drinking-water supply wells, since May of 1988. As a result, a large water-quality data base has been compiled that includes data for major ions, nutrients, trace elements, carbon, volatile organic compounds, radiological constituents, and bacteria. These data are intended to improve the understanding and management of the ground-water resources of the region, rather than demonstrate compliance with Federal and State drinking-water standards. This report gives summary statistics for selected physical properties and chemical constituents for ground water from wells used by the City of Albuquerque for drinking-water supply between 1988 and 1997. Maps are provided to show the general spatial distribution of selected parameters and water types around the region. Although the values of some parameters vary substantially across the city, median values for all parameters included in this report are less than their respective maximum contaminant levels in each drinking-water supply well. The dominant water types are sodium plus potassium / carbonate plus bicarbonate in the western part of the city and calcium / carbonate plus bicarbonate in the eastern part of the city.

Open-File Report↗