Fe(II) reduction of pyrolusite (β-MnO2) and secondary mineral evolution
نویسندگان
چکیده
منابع مشابه
Fe(II) reduction of pyrolusite (β-MnO2) 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) with pyrolusite (β-MnO2) using electron microscopy, X-ray diffraction, aqueous Fe and Mn analyses...
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ژورنال
عنوان ژورنال: Geochemical Transactions
سال: 2017
ISSN: 1467-4866
DOI: 10.1186/s12932-017-0045-0