December 15, 2007
Journal Article

Uranium immobilization by sulfate-reducing biofilms grown on hematite, dolomite, and calcite.

Abstract

Biofilms of sulfate-reducing bacteria Desulfovibrio desulfuricans G20 wereused to reduce dissolved U(VI)and subsequently immobilize U(IV) in the presence of uranium-complexing carbonates. The biofilms were grown in three identically operated fixed bed reactors, filled with three types of minerals: one noncarbonate-bearing mineral(hematite) and two carbonate-bearing minerals (calcite and dolomite). The source of carbonates in the reactors filled with calcite and dolomite were the minerals, while in the reactor filled with hematite it was a 10 mM carbonate buffer, pH 7.2, which we added to the growth medium. Our five-month study demonstrated that the sulfate-reducing biofilms grown in all reactors were able to immobilize/reduce uranium efficiently, despite the presence of uranium-complexing carbonates.

Revised: April 7, 2011 | Published: December 15, 2007

Citation

Marsili E., H. Beyenal, L. Di Palma, C. Merli, A. Dohnalkova, J.E. Amonette, and Z. Lewandowski. 2007. Uranium immobilization by sulfate-reducing biofilms grown on hematite, dolomite, and calcite. Environmental Science & Technology 41, no. 24:8349-8354. PNNL-SA-57705. doi:10.1021/es071335k