The Biogeochemical Fate of Se(VI) in Bentonite Systems Relevant to the Disposal of High-Level Radioactive Waste

ORCID

Document Type

Article

Abstract

Selenium-79, a radionuclide present in higher-activity radioactive wastes destined for deep geological disposal, is mobile under oxic conditions, where Se(IV) and Se(VI) dominate. Anoxic batch microcosm incubations were constructed containing Wyoming MX80 bentonite (a candidate buffer material in geological disposal) and artificial groundwater with or without steel coupons to represent canister materials. Se(VI)(aq) bioreduced and was removed by 7 days when lactate was added as an electron donor, after which sulfate reduction occurred. With H2 gas as the electron donor, Se(VI) bioreduction slowed, with complete removal at 14 days and minimal sulfate reduction thereafter. 16S rRNA gene sequencing highlighted the dominance of Anaerobacillus spp. (44% at 28 days) during Se(VI)-reduction, and in the lactate-amended systems, there was a subsequent enrichment in sulfate-reducing bacteria affiliated with Desulfosporosinus spp. (60% relative abundance at 84 days). Extended X-ray absorption fine structure (EXAFS) analyses identified monoclinic Se(0) as the bioreduction product after 28 days, but by 84 days this evolved to trigonal Se(0) in the absence of steel coupons or was further reduced to FeSe2 with steel present. The reduction of Se(VI)(aq) to poorly soluble Se(0)/FeSe2 mediated by indigenous bentonite microbial communities highlights their potential importance in promoting Se-79 retention during deep geological disposal.

Publication Date

2026-02-10

Publication Title

Environmental Science and Technology

Volume

60

Issue

5

ISSN

0013-936X

Acceptance Date

2026-01-14

Deposit Date

2026-09-28

Embargo Period

2027-01-26

Keywords

Bentonite, Bioreduction, Geological Disposal Facility, Selenium-79, Steel corrosion

First Page

4124

Last Page

4133

This document is currently not available here.

This item is under embargo until 26 January 2027

Share

COinS