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10.1021/acs.est.5c12024

http://scihub22266oqcxt.onion/10.1021/acs.est.5c12024
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41391016!?!41391016

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suck abstract from ncbi

pmid41391016      Environ+Sci+Technol 2025 ; ? (?): ?
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  • Technetium Retention and Remobilization Potential after Prolonged Reaction in Fe(III)- and Sulfate-Reducing Model Aquifer Systems #MMPMID41391016
  • Ho MS; Vettese GF; Morris K; Lloyd JR; Boothman C; Shaw S; Dardenne K; Pearce C; Law GTW
  • Environ Sci Technol 2025[Dec]; ? (?): ? PMID41391016show ga
  • (99)Tc is a long-lived radioactive fission product whose subsurface mobility is governed by redox conditions. Under oxic conditions, soluble Tc(VII)O(4)(-) is mobile, whereas under reducing conditions, poorly soluble Tc(IV) phases limit transport. Microcosm studies have frequently reported TcO(2)-like solids and, less consistently, Tc(IV)-sulfides. The stability of Tc(IV)-sulfides under environmentally relevant conditions remains unclear. Here, we used flowing sediment columns representative of the Sellafield subsurface to examine Tc speciation and stability over approximately 1 year. Under reducing conditions, >90% of added TcO(4)(-) (400 mug) was retained under both Fe(III)- and sulfate-reducing conditions. X-ray absorption spectroscopy showed TcO(2)-like phases dominated in Fe(III)-reducing columns, while Tc(IV)-sulfides dominated after sustained sulfate reduction. Sequential extractions indicated that Tc in sulfidic sediments was more recalcitrant (
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