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Published online 22 May 2009
Clay Minerals; March 2009; v. 44; no. 1; p. 113-123; DOI: 10.1180/claymin.2009.044.1.113
© 2009 Mineralogical Society of Great Britain and Ireland
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Research Paper

Site-specific P absorbency of ochre from acid mine-drainage near an abandoned Cu-S mine in the Avoca–Avonmore catchment, Ireland

O. Fenton1,*, M. G. Healy2, M. Rodgers2 and D. O Huallacháin1

1 Teagasc, Johnstown Castle, Environmental Research Centre, Co Wexford, Ireland,2 Department of Civil Engineering, National University of Ireland, Galway, Ireland

* E-mail: owen.fenton{at}teagasc.ie

(Received 13 June 2008; revised 25 September 2008)

Acid mine-drainage from an abandoned Cu-S mine adit, located in the Avoca–Avonmore catchment in the southeast of Ireland, results in low-value ochre deposition. Ochre found on-site had similar physical (particle size 97.7% <2 mm and dry bulk density 0.8 g cm3), but dissimilar maximum P-retention characteristics (16–21 g P kg –1) to coal-mining ochre found in the UK. Stereomicroscopy identified oolites and diatoms in the ochre that were indicative of acidic environments. X-ray diffraction showed Fe mineralogy consisting of goethite, jarosite and minor amounts of ferrihydrite. Investigations by inductively coupled plasma-mass spectrometry and bulk energy-dispersive spectroscopy showed potentially toxic concentrations of Fe, Zn, Pb, As and Cu. Rapid mobilization of metals occurred during P-adsorption tests, which makes Avoca ochre unsuitable for use in a surface-water environmental technology.

KEYWORDS: acid mine-drainage, ochre, phosphorus, Avoca–Avonmore catchment, Ireland







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Mineralogical Society of Great Britain and Ireland