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Published online 9 August 2006
Published in J Environ Qual 35:1731-1741 (2006)
DOI: 10.2134/jeq2005.0123
© 2006 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
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TECHNICAL REPORTS

Heavy Metals in the Environment

Physicochemical and Mineralogical Characterization of Soil–Saprolite Cores from a Field Research Site, Tennessee

Ji-Won Moona, Yul Rohb,*, Tommy J. Phelpsa, Debra H. Phillipsc, David B. Watsona, Young-Jin Kima and Scott C. Brooksa

a Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831
b Faculty of Earth System and Environmental Sciences, Chonnam National University, 300 Yongbong-Dong, Buk-Gu, Gwangju, 500-757, Korea
c Environmental Engineering Research Centre, School of Architecture, Civil and Environmental Engineering, and Planning, Queen's University of Belfast, Belfast BT9 5AG, Northern Ireland, UK

* Corresponding author (rohy{at}chonnam.ac.kr)

Received for publication April 11, 2005. Site characterization is an essential initial step in determining the feasibility of remedial alternatives at hazardous waste sites. Physicochemical and mineralogical characterization of U-contaminated soils in deeply weathered saprolite at Area 2 of the DOE Field Research Center (FRC) site, Oak Ridge, TN, was accomplished to examine the feasibility of bioremediation. Concentrations of U in soil–saprolite (up to 291 mg kg–1 in oxalate-extractable Uo) were closely related to low pH (ca. 4–5), high effective cation exchange capacity without Ca (64.7–83.2 cmolc kg–1), amorphous Mn content (up to 9910 mg kg–1), and the decreased presence of relative clay mineral contents in the bulk samples (i.e., illite 2.5–12 wt. %, average 32 wt. %). The pH of the fill material ranged from 7.0 to 10.5, whereas the pH of the saprolite ranged from 4.5 to 8. Uranium concentration was highest (about 300 mg kg–1) at around 6 m below land surface near the saprolite–fill interface. The pH of ground water at Area 2 tended to be between 6 and 7 with U concentrations of about 0.9 to 1.7 mg L–1. These site specific characteristics of Area 2, which has lower U and nitrate contamination levels and more neutral ground water pH compared with FRC Areas 1 and 3 (ca. 5.5 and <4, respectively), indicate that with appropriate addition of electron donors and nutrients bioremediation of U by metal reducing microorganisms may be possible.

Abbreviations: BCV, Bear Creek Valley • CBD, citrate–bicarbonate–dithionate • DOE, Department of Energy • DXRD, differential X-ray diffraction • ECEC, effective cation exchange capacity • EDX, energy dispersive X-ray • FRC, field research center • HIV, hydroxy-interstratified vermiculite • IC, ion chromatograph • MRB, metal-reducing bacteria • NABIR, Natural and Accelerated Bioremediation Research • ORR, Oak Ridge Reservation • PCB, polychlorinated biphenyl • PCE, tetrachloroethylene • RIR, reference intensity ratio • SEM, scanning electron microscope • TIC, total inorganic carbon • TOC, total organic carbon • XRD, X-ray diffraction • XRF, X-ray fluorescence




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