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Mineralogical Magazine; December 2006; v. 70; no. 6; p. 731-741; DOI: 10.1180/0026461067060360
© 2006 Mineralogical Society of Great Britain and Ireland
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Letter

Fe(II)/Fe(III) ‘green rust’ developed within ochreous coal mine drainage sediment in South Wales, UK

J. M. Bearcock1,*, W. T. Perkins1, E. Dinelli2 and S. C. Wade3

1 Institute of Geography and Earth Sciences, University of Wales, Aberystwyth SY23 3DB, UK
2 Bologna University, Piazza di Porta San Donato, 1, Bologna, I-40126, Italy
3 Institute of Biological Sciences, University of Wales, Aberystwyth SY23 3DA, UK

* E-mail: jjb{at}aber.ac.uk

ABSTRACT

‘Green rusts’ are a group of reduced Fe hydroxides with a pyroaurite-like structure. In a new occurrence, green rust is present as a 45–60 mm thick band which lies just below the surface (~4 mm) of an ochreous deposit at an abandoned coal mine site. The sample is characterized by the presence of µ m-sized hexagonal crystals which have been identified from SEM imaging. Chemical analyses reveal an Fe(II):Fe(III) ratio which is close to the characteristic 2:1 ratio, and XRD analysis identifies the material by characteristic lattice spacings. The green rust layer also contains aragonite which is not present in the surrounding ochre. Green rusts are important as they have the potential to be used in water treatment.

KEYWORDS: Green rust, coal mine, ochre, drainage, South Wales







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