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Research Paper |
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
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