VZJ Journal of Natural Resources and Life Sciences Education
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Published in Vadose Zone Journal 3:190-202 (2004)
© 2004 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA

SPECIAL SECTION: UNDERSTANDING SUBSURFACE FLOW AND TRANSPORT PROCESSES AT THE IDAHO NATIONAL ENGINEERING & ENVIRONMENTAL LABORATORY (INEEL) SITE

Fate of Brine Applied to Unpaved Roads at a Radioactive Waste Subsurface Disposal Area

Larry C. Hull* and Carolyn W. Bishop

Idaho National Engineering and Environmental Laboratory, P.O. Box 1625, Idaho Falls, ID 83415-2107
* Corresponding author (hulllc{at}inel.gov).

Received 28 March 2003.

Between 1984 and 1993, MgCl2 brine was used to suppress dust on unpaved roads at a radioactive waste subsurface disposal area. Because Cl might enhance corrosion of buried metals in the waste, we investigated the distribution and fate of Cl in the vadose zone using pore water samples collected from suction lysimeters and soluble salt concentrations extracted from sediment samples. The Cl/Br mass ratio and the total dissolved Cl concentration of pore water show that brine contamination occurs primarily within 13 m of treated roads, but can extend as much as 30 m laterally in near-surface sedimentary deposits. Within the deep vadose zone, which consists of interlayered basalt lava flows and sedimentary interbeds, brine has moved up to 110 m laterally. This lateral migration suggests formation of perched water and horizontal transport during periods of high recharge. In a few locations, brine migrated to depths of 67 m within 3 to 5 yr. Elevated Cl concentrations were found to depths of 2 m in roadbed material. In drainage ditches along roads, where runoff accumulates and recharge of surface water is high, Cl was flushed from the sediments in 3 to 4 yr. In areas of lower recharge, Cl remained in the sediments after 5 yr. Vertical brine movement is directly related to surface recharge through sediments. The distribution of Cl in pore water and sediments is consistent with estimates of vadose zone residence times and spatial distribution of surface water recharge from other investigations at the subsurface disposal area.

Abbreviations: INEEL, Idaho National Engineering and Environmental Laboratory • SDA, Subsurface Disposal Area




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E. D. Mattson, S. O. Magnuson, and S. L. Ansley
Interpreting INEEL Vadose Zone Water Movement on the Basis of Large-Scale Field Tests and Long-Term Vadose Zone Monitoring Results
Vadose Zone J., February 1, 2004; 3(1): 35 - 46.
[Abstract] [Full Text] [PDF]




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