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- W2742883601 abstract "Intercommunication has been identified between the unconfined and uppermost confined aquifer systems underlying a portion of the U.S. Department of Energy's Hanford Site. Erosional thinning and fracturing of the basalt confining layer within the study area allows physical contact between the two aquifers, but the vertical hydraulic gradient (a required driving force) is small. To better conceptualize the distribution and volume of the leakage occurring between the aquifer systems, this study investigates the confined Rattlesnake Ridge Aquifer flow system, which appears to be more sensitive to the vertical leakage than the overlying unconfined aquifer." @default.
- W2742883601 created "2017-08-17" @default.
- W2742883601 creator A5059423276 @default.
- W2742883601 date "2017-11-22" @default.
- W2742883601 modified "2023-09-27" @default.
- W2742883601 title "A groundwater flow model of the aquifer intercommunication area, Hanford site, Washington" @default.
- W2742883601 doi "https://doi.org/10.15760/etd.5223" @default.
- W2742883601 hasPublicationYear "2017" @default.
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