Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Preliminary analysis of some waters from the confined aquifers underlying the Hanford site

Technical Report ·
DOI:https://doi.org/10.2172/6502673· OSTI ID:6502673
This report presents results of analyses available at this time from waters from some wells sampled in or near the Hanford Site. The analyses of these wells were done for various purposes and are consolidated to help define the nature of the waters found within the Columbia Plateau basaltic sequence. Results of the analyses show the waters from the unconfined aquifers underlying the Hanford Site are characterized by a high calcium--magnesium content. These waters can be described as calcium--magnesium--bicarbonate-type. Waters from deeper basaltic confined aquifers are primarily of the sodium bicarbonate type. Two waters sampled from the Grande Ronde Formation from Rattlesnake Hills Exploratory Well Number 1 are slightly different and can be described as sodium--calcium--bicarbonate--sulfate--chloride-type. Age-dating results for these water samples lead to the conclusions that waters from the confined aquifers were entrapped 15,000 to 23,000 years ago.
Research Organization:
Atomics International Div., Richland, WA (USA). Rockwell Hanford Operations
DOE Contract Number:
EY-77-C-06-1030
OSTI ID:
6502673
Report Number(s):
RHO-BWI-LD-12
Country of Publication:
United States
Language:
English