Highly toxic thallium (Tl) can be released into the environment through acid mine drainage (AMD). However, our knowledge on the biogeochemical processes of Tl in such acidic, iron (Fe)-rich environments is limited. Here, we show that schwertmannite, a naturally formed Fe(III) mineral in AMD, can effectively immobilize Tl(I) through coprecipitation and adsorption. Tl(I) coprecipitation into schwertmannite removed a large portion of Tl(I) under a wide range of initial Tl(I) concentrations (0.01~1.0mg/L) and within a short duration (48h). The saturated adsorption capacities of the biosynthetic and chemically synthesized schwertmannite for Tl(I) (1.0mg/L) were 1.96 and 1.59mg/g, respectively, under acidic conditions (pH=3.0). The kinetic dissolution results indicated that biogenic Tl-coprecipitated schwertmannite exhibited greater stability, which was attributed mainly to the elevated extent of Tl oxidation and enhanced crystallinity of Tl-bearing schwertmannite. The extended X-ray absorption fine structure (EXAFS) analyses revealed that the incorporation of Tl into schwertmannite involves the heterovalent substitution of Fe(III) by the formation of double-corner sharing linkages between the Tl-O tetrahedra and Fe-O octahedra. These results suggested that coprecipitation combined with adsorption can achieve retention of Tl in acidic environment throughout the entire mineralization process of schwertmannite, which provides a comprehensive understanding of biogeochemical fate of Tl in AMD-affected areas.
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