LANL Environmental Programs

(PI of "Vadose Zone and Regional Aquifer Flow and Transport Modeling")

Los Alamos National Laboratory (LANL) is a complex site for environmental management. The site encompasses about 100 km2 (37 square miles) of terrain with 600 m (2,000 feet) of elevation change, and an average rainfall of less than 300-400 mm (12 to 16 inches) per year. The site is intersected by 14 major canyon systems. Ecosystems within the site range from riparian to high desert and boast over 2,000 archaeological sites, as well as endangered species habitats.  The surface and subsurface water flow discharges primarily along the Rio Grande to the east of LANL. The Rio Grande traverses the Española basin from north to south; several major municipalities use the river water downgradient from LANL for water supply (Santa Fe, Albuquerque, El Paso/ Ciudad Juarez).

Map of LANL and Espanola basin

Regional quifer beneath LANL

The regional aquifer beneath LANL is a complex hydrogeological system.  The regional aquifer extends throughout the Española basin, and is an important source for municipal water supply for Santa Fe, Los Alamos, Española, LANL, and several Native-American Pueblos. The wells providing groundwater from this aquifer for Los Alamos and LANL are located within the LANL site and in close proximity to existing contamination sites. The regional aquifer is comprised of sediments and lavas with heterogeneous flow and transport properties. The general shape of the regional water table is predominantly controlled by the areas of regional recharge to the west (the flanks of the Sierra de los Valles and the Pajarito fault zone) and discharge to the east (the Rio Grande and the White Rock Canyon Springs). At more local scales, the structure of groundwater flow is also influenced by (1) local infiltration zones (e.g., beneath wet canyons); (2) heterogeneity and anisotropy in the aquifer properties; and (3) discharge zones (municipal water-supply wells and springs). The aquifer is also characterized by well-defined, vertical stratification which, in general, provides sufficient protection of the deep groundwater resources.

The vadose zone, between the ground surface and the top of the regional aquifer, is about 180-300 m (600-1000 ft) thick. The vadose zone is comprised of sediments and lavas with heterogeneous flow and transport properties. The variably-saturated flow and transport through the thick vadose zone occurs through pores and fractures, and is predominantly vertical with lateral deviations along perching zones. The groundwater velocities in the vadose zone are high beneath wet canyons (up to 1 m/a) and low beneath the mesas (1 mm/a). Due to complexities in local hydrogeologic conditions, the hydraulic separation between the regional aquifer and the vadose zone is difficult to identify at some localities, especially where mountain-front recharge is pronounced.

The complexity and size of the LANL site make environmental management a continuing engineering and scientific challenge. Legacy contamination—both chemical and radioactive—exists at many locations. Some of the oldest worldwide radioactive Material Disposal Areas (MDA’s), where waste is buried in pits and shafts, are located on the site. LANL is mandated to follow timetables and requirements specified by the Compliance Order on Consent from the New Mexico Environment Department (NMED) for investigation, monitoring, and remediation of hazardous constituents and contaminated sites. Currently, all the remediation activities are scheduled for completion in 2015.  LANL is taking actions to prevent potential contaminant effects on human health and the environment.

Map of monitoring wells at the LANL site

The environmental work performed at the LANL site is managed by the Environmental Programs (EP) Directorate. A team of external and LANL (Computational Earth Sciences Group, Earth & Environmental Sciences) researchers is tasked by the EP Directorate to provide modeling and decision support to enable scientifically-defensible mitigation of the risks associated with various LANL sites. The principal investigator of this team is Velimir Vesselinov.

Since the 1950's, the LANL site has been the subject of intensive studies for characterization of the site conditions, including regional geology and hydrogeology. Various types of research have been performed at the site related to contaminant transport in the environment which include (1) laboratory experiments, (2) field tests, and (3) conceptual and numerical model analyses. The work is presented in a series of technical reports and peer-reviewed publications.

Currently, important aspects of the environmental management at the LANL site include:

Chromium plume in the regional aquifer

A chromium plume has been identified in the regional aquifer beneath the LANL site. Our team has been tasked with providing modeling decision support to the Environmental Programs (EP) Directorate to enable scientifically-defensible mitigation of the risks associated with chromium migration in the environment. Large amount of data and information are available related to the chromium site (vadose-zone moisture content, aquifer water levels, contaminant concentrations, geologic observations, drilling logs, etc.); they are used to develop and refine conceptual and numerical models of the contaminant transport in the environment. The development of numerical models and performance of model analyses (model calibration, sensitivity analyses, parameter estimations, uncertainty quantification, source identification, data-worth analyses, monitoring-network design, etc.) is a computationally intensive effort due to large model domains, large numbers of computational nodes, complex flow media (porous and fracture flow), and long model-execution times. Due to complexities in the model-parameter space, most of the model analyses require a substantial number of model executions. To improve computational effectiveness, our team utilizes state-of-the-art parallel computational resources and novel theoretical and computational methods for model calibration, uncertainty analysis, risk assessment and decision support.

Numerical modeling of flow and transport in the regional aquifer near Sandia Canyon

The numerical model is capturing current conceptual understanding and calibrated against existing data (taking into account uncertainties)

Regardless of existing uncertainties, the model provide information related to:

Conceptual model of flow at the TA-16 site

Relevant computer codes:

Relevant publications:

Relevant presentations:

Relevant technical reports: