Bioreduction of Fe-bearing clay minerals and their reactivity toward pertechnetate (Tc-99)

By Michael E. Bishop, Hailiang Dong, R. Kukkadapu, Chongxuan Liu, R. Edelmann. 2011

143 citations recorded by the source corpus.

Subfields: Geochemistry and Petrology, Inorganic Chemistry, Materials Chemistry

View Paper: https://www.semanticscholar.org/paper/628130df5b7e11a06319455e5137ab84deacea67

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In Geochemistry and Petrology

1. I. Skorochod
2. M. Fomina

In Inorganic Chemistry

1. I. Skorochod
2. M. Fomina

In Materials Chemistry

1. M. Fomina

Citations in the corpus

• Microbial Interaction with Clay Minerals and Its Environmental and Biotechnological Implications (2020, background): “For Tc(VII) reduction to Tc(IV), it was reported that structural Fe(II) is most reactive in smectite and least in illite [328], and that for nontronite reduced Tc(IV) is firmly immobilized within the mineral matrix, minimizing the potential for remobilization and suggesting long-term bioremediation ”