T12 Hydrogeology of Mountainous Terrains

Sunday, 28 October 2007
8:00 AM - 12:00 PM

RADIOGENIC AND STABLE ISOTOPE AND HYDROGEOCHEMICAL INVESTIGATION OF GROUNDWATER, PAJARITO PLATEAU AND SURROUNDING AREAS, NEW MEXICO

Paper number: T12-10
Program: Technical Sessions
Time: 10:10 AM – 10:25 AM

Authors

Abstract

Understanding groundwater flow is critical for resource protection and aquifer sustainability, especially in the arid southwest. Knowing this, several agencies undertook an investigation to evaluate flow paths and date the modern and submodern components of the groundwater-flow system at Los Alamos, New Mexico and the surrounding areas. At Los Alamos, groundwater is modern (post-1943), submodern (pre-1943), or mixed (containing both pre- and post-1943 components). The regional aquifer primarily consists of submodern groundwater. Mixed-age groundwater results from initial infiltration of surface water, followed by mixing with perched alluvial and intermediate-depth groundwater and the regional aquifer. No groundwater investigation is complete without using tritium/helium-3 and carbon-14 dating methods to quantify amounts of modern, mixed, and/or submodern components present in samples. Computer models of groundwater flow and transport at Los Alamos should be calibrated to groundwater ages for perched intermediate zones and the regional aquifer determined from this investigation.

Results of this study clearly demonstrate the occurrence of multiple flow paths and groundwater ages occurring within the Sierra de los Valles, beneath the Pajarito Plateau, and at the White Rock Canyon springs. Localized groundwater recharge occurs within several canyons dissecting the Pajarito Plateau. Perched intermediate-depth groundwater and the regional aquifer beneath Pueblo Canyon, Los Alamos Canyon, Sandia Canyon, Mortandad Canyon, Pajarito Canyon, and Cañon de Valle contain a modern component. This modern component consists of tritium, nitrate, perchlorate, chromate, boron, uranium, and/or high explosive compounds. It is very unlikely that there is only one transport or travel time, ranging from 25 to 62 years, for these conservative chemicals migrating from surface water to the regional water table. Lengths of groundwater flow paths vary within deep saturated zones containing variable concentrations of tritium. The 4-series springs discharging within White Rock Canyon contain a modern component of groundwater, primarily tritium. Average groundwater ages for the regional aquifer beneath the Pajarito Plateau vary from 565 to 10,817 years, based on unadjusted carbon-14 measurements.