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Title: Soil moisture transport in arid site vadose zones. [Evaluation of Hanford as national site for radioactive waste storage]

Technical Report ·
DOI:https://doi.org/10.2172/7282680· OSTI ID:7282680

Data are presented from measurements of soil moisture at the Hanford Reservation. Possible mechanisms for moisture transport in arid and semi-arid climates were studied. Measurements for the lysimeter experiment and the thermocouple psychrometer experiment were continued with a new series of measurements using closely spaced sensors installed to a depth of 1.52 meters. During the 1973-1974 water year the percolation envelope of higher moisture content penetrated to a depth of four meters in the closed-bottom lysimeter and then was eliminated by upward transport of water in late summer. Precipitation during the 1973-1974 water year percolated to a depth of about six meters in the open-bottom lysimeter and remains as a residual perched envelope. The increase over normal percolation was due in part to a residual envelope of higher moisture content from the previous water year. Results obtained indicate the advantages of Hanford as a site for a national repository for radioactive waste. (CH)

Research Organization:
Atlantic Richfield Hanford Co., Richland, WA (United States)
DOE Contract Number:
E(45-1)-2130
OSTI ID:
7282680
Report Number(s):
ARH-ST-123; TRN: 76-014984
Country of Publication:
United States
Language:
English