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

Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina

Book ·
OSTI ID:6705995
The unsaturated zone consists of a few centimeters to > 1 m of surface sand underlain by up to 15 m of clayey sand. Tracer tests using sodium chloride were conducted at each monitoring site. Data collection at the monitoring sites began in January 1982 and continued until early May 1984. Tensiometer data show that the unsaturated materials had their highest percent saturations in the winter and spring. Saturations in the backfill sand varied from 20 to 100%. During 1984, the rise and fall of ponded water in an experimental trench was continuously monitored with a digital recorder. A cross-sectional finite element model of variably saturated flow was used to test the conceptual model of water movement in the unsaturated zone and to illustrate the effect of trench design on water movement into the experimental trenches. Monitoring and model results show that precipitation on trenches infiltrated the trench cap and moved vertically into the trench backfill material. 26 refs., 32 figs., 3 tabs.
OSTI ID:
6705995
Country of Publication:
United States
Language:
English