Two main natural processes which control the migration of radioactive contaminants to the biosphere were studied in the Yamin Plain in order to evaluate the thickness of a cover layer needed for near-surface radioactive waste disposal facility. The first is the natural erosion of the cover layer, and the second is the infiltration during rain and runoff events. The erosion rate of the soil surface was studied by optical stimulation luminescence technique. It was found that during the last 14,000 years, the erosion rate was 0.3 mm/y which are 3 m for 10,000 years. The infiltration depth assessment was based on water content measurements and numerical modeling. It shows that under the most extreme rain event having an equivalent rain of 84 mm, infiltration depth was limited to 4.5 m. Taking into account the two processes, the effective cover layer thickness over 10,000 years should be at least 7.5 m thick.
Issue Section:
Special Section Papers
References
1.
IAEA
, 1999
, “Safety Assessments for Near Surface Disposal of Radioactive Waste
,” International Atomic Energy Agency, Vienna, Austria, Standard No. WS-G-1.1.2.
IAEA
, 2011
, “Disposal of Radioactive Waste
,” Specific Safety Requirements, International Atomic Energy Agency, Vienna, Austria, Standard No. SSR-5.3.
IAEA
, 2014
, “Near Surface Disposal Facilities for Radioactive Waste
,” International Atomic Energy Agency, Vienna, Austria, Standard No. SSG-29.4.
IAEA
2001
, “Performance of Engineered Barriers Material in Near Surface Disposal Facilities for Radioactive Waste
,” International Atomic Energy Agency, Vienna, Austria, Standard No. IAEA-TECDOC–1255.5.
Hawkins
, R. H.
, and Horton
, J. H.
, 1967
, “Bentonite as a Protective Dover for Buried Radioactive Waste
,” Health Physics
, 13
(3
), pp. 241
–292
.6.
Petit-Berghem
, Y.
, and Lemperiere
, G.
, 2012
, “Vegetation Cover and Long-Term Conservation of Radioactive Waste Packages: The Case Study of the CSM Waste Disposal Facility (Manche District, France)
,” Environ. Manage.
, 49
(3
), pp.. 605
–622
.7.
Albright
, W.
, Benson
, C.
, Gee
, G.
, Abichou
, T.
, McDonald
, E.
, Tyler
, S.
, and Rock
, S.
, 2006
, “Field Performance of a Compacted Clay Landfill Final Cover at a Humid Site
,” J. Geotech. Geoenviron. Eng.
, 132
(11
), pp. 1393
–1403
.8.
Hauser
, V.
, Weand
, B.
, and Gill
, M.
, 2001
, “Natural Covers for Landfills and Buried Waste
,” J. Environ. Eng.
, 127
(9
), pp. 768
–775
.9.
Levitt
, D. G.
, Sully
, M. J.
, Dozier
, B. L.
, Charles
, F.
, and Lohrstorfer
, C. F.
, 1999
, “Determining the Performance of an Radioactive Waste Site Through Site Characterization, Modeling and Monitoring
,” WM
Conference
, Feb. 28–Mar. 1.10.
Kernel
, E.
,’ 1924
, “Syriche Bogen
,” Mineral
, 9
, pp. 274
–281
.11.
Salomon
, A.
, 1987
, “The Monoclines in the Northern Negev: A Model of Tilted Blocks and Shortening
,” M.Sc. thesis, The Hebrew University, Jerusalem, Israel (in Hebrew, English abstract).12.
Calvo
, R.
, and Bartov
, Y.
, 2001
, “Hazeva Group, Southern Israel: New Observations and Their Implications for Its Stratigraphy, Paleogeography, and Tectono-Sedimentary Regime
,” Isr. J. Earth Sci.
, 50
, pp. 71
–99
.13.
Bruner
, I.
, Weiner
, D.
, Goldman
, M.
, Calvo
, R.
, and Bartov
, Y.
, 1999
, “Geophysical Investigation Through Subsurface Imaging in the Mishor Yamin Area
,” Geophysical Institute of Israel Report, Report No. 641/170/96 (in Hebrew).14.
Dody
, A.
, and Wiener
, D.
, 2005
, “Recharge Processes of the Neogene Aquifer in Mishor Yamin NE Negev, Israel
,” Isr. J. Earth Sci.
, 54
(1
), pp. 29
–34
.15.
Kahana
, R.
, Ziv
, B.
, Enzel
, Y.
, and Dayan
, U.
, 2002
, “Synoptic Climatology of Major Floods in the Negev Desert, Israel
,” Int. J Climatol.
, 22
(7
), pp. 867
–882
.16.
Columbus
, U.
, Dody
, A.
, Renan
, I.
, Bogin-Zilka
, Y.
, Siegal
, Z.
, Walchak
, M.
, and Zvik
, Y.
, 2016
, “Ecological Survey in Yamin and Rotem Plains
,” Israel Nature and Parks Authority, Beer Sheva, Israel (in Hebrew).17.
Hetz
, G.
, 2009
, “Monitoring Surface Alternations in the Yamin Plateau by Spaceborne Images and Aerial Photography Between 1945–2009
,” M.A. thesis, Ben Gurion University, Beer Sheva, Israel (in Hebrew, English abstract).18.
Edri
, A.
, 2014
, “Spatial Differences in Aeolian Erosion of Arid Silty—Sand Soils due to Surface Features
,” M.A. thesis, Ben Gurion University, Beer Sheva, Israel (in Hebrew, English abstract).19.
Belnap
, J.
, 2006
, “The Potential Roles of Biological Soil Crusts in Dryland Hydrologic Cycles
,” Hydrol. Processes
, 20
(15
), pp. 3159
–3178
.20.
Porat
, N.
, 2007
, “Analytical Procedures in the Luminescence Dating Laboratory
,” Geophysical Institute of Israel Report, Report No. TR-S\GSI/2/2007 (in Hebrew).21.
Aitken
, M. J.
, 1985
, Thermoluminescence Dating
, Academic Press
, London
, p. 359
.22.
Rimon
, Y.
, Dahan
, O.
, Nativ
, R.
, and Geyer
, S.
, 2007
, “Water Percolation Through the Deep Vadose Zone and Groundwater Recharge: Preliminary Results Based on a New Vadose Zone Monitoring System
,” Water Resour. Res.
, 43
(5
).23.
Robinson
, D. A.
, Jones
, S. B.
, Wraith
, J. M.
, Or
, D.
, and Friedman
, S. P.
, 2003
, “A Review of Advances in Dielectric and Electrical Conductivity Measurement in Soils Using Time Domain Reflectometry
,” Vadose Zone J.
, 2
(4
), pp. 444
–475
.24.
Šimůnek
, J.
, Van Genuchten
, M. T.
, and Šejna
, M.
, 2008
, “Development and Applications of the Hydrus and Stanmod Software Packages and Related Codes
,” Vadose Zone J.
, 7
(2
), pp. 587
–600
.25.
Carsel
, R. F.
, and Parrish
, R. S.
, 1988
, “Developing Joint Probability—Distributions of Soil—Water Retention Characteristics
,” Water Resour. Res.
, 24
(5
), pp. 755
–769
.26.
Dody
, A.
, Nahlieli
, A.
, Avni
, Y.
, Cohen
, H.
, Weiner
, D.
, and Porat
, N.
, 2008
, “Late Quaternary Deposition and Erosion Process Along the Margins of the Yamin Plain, Northeast Negev, Israel
,” Isr. J. Earth Sci.
, 57
(3
), pp. 199
–211
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