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Isotopic Tracers for Waste Fluid Tracking and Fluid-Soil Interactions: Hanford, Washington
Author(s) -
Donald J. DePaolo
Publication year - 2005
Publication title -
osti oai (u.s. department of energy office of scientific and technical information)
Language(s) - English
Resource type - Reports
DOI - 10.2172/884924
Subject(s) - vadose zone , groundwater , infiltration (hvac) , geology , hydrology (agriculture) , tracer , radioactive waste , capillary fringe , environmental science , environmental chemistry , geochemistry , chemistry , geotechnical engineering , physics , nuclear chemistry , nuclear physics , thermodynamics
The objective of this research is to develop and advance isotopic methods for characterizing fluid flow and chemical transport through the vadose zone to groundwater. Previous research has been concentrated on developing and comparing different isotopic systems (e.g., hydrogen, oxygen and strontium isotopes) for determining fluid infiltration rates and pathways in the vadose zone (e.g., Maher et al., 2003; DePaolo et al., 2004; Singleton et al., in press). The focus of our current efforts is on using the isotopic compositions of different chemical phases (e.g., uranium, nitrate) to track their movement through the vadose zone. Preliminary results indicate that this will be a powerful tool for assessing environmental risks associated with vadose zone contamination

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