Fe(II) reduction of pyrolusite (β-MnO(2)) and secondary mineral evolution

Iron (Fe) and manganese (Mn) are the two most common redox-active elements in the Earth’s crust and are well known to influence mineral formation and dissolution, trace metal sequestration, and contaminant transformations in soils and sediments. Here, we characterized the reaction of aqueous Fe(II)...

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Detalles Bibliográficos
Autores principales: Schaefer, Michael V., Handler, Robert M., Scherer, Michelle M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer International Publishing 2017
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5716966/
https://www.ncbi.nlm.nih.gov/pubmed/29209871
http://dx.doi.org/10.1186/s12932-017-0045-0

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5716966/
https://www.ncbi.nlm.nih.gov/pubmed/29209871
http://dx.doi.org/10.1186/s12932-017-0045-0

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