Schwertmannite and Fe oxides formed by biological low-pH Fe(II) oxidation versus abiotic neutralization: Impact on trace metal sequestration

Author:

Burgos William D.,Borch Thomas,Troyer Lyndsay D.,Luan Fubo,Larson Lance N.,Brown Juliana F.,Lambson Janna,Shimizu Masayuki

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference47 articles.

1. The behavior of trace elements during schwertmannite precipitation and subsequent transformation into goethite and jarosite;Acero;Geochim. Cosmochim. Acta,2006

2. A poorly crystallized oxyhydroxysulfate of iron formed by bacterial oxidation of Fe(II) in acid mine waters;Bigham;Geochim. Cosmochim. Acta,1990

3. Schwertmannite and the chemical modeling of iron in acid sulfate waters;Bigham;Geochim. Cosmochim. Acta,1996

4. Phosphate imposed limitations on biological reduction and alteration of ferrihydrite;Borch;Environ. Sci. Technol.,2006

5. Application of a depositional facies model to an acid mine drainage site;Brown;Appl. Environ. Microbiol.,2010

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