Abstract
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.
| Original language | English |
|---|---|
| Pages (from-to) | 113-123 |
| Number of pages | 11 |
| Journal | Clay Minerals |
| Volume | 44 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 1 Mar 2009 |
Keywords
- Acid mine-drainage
- Avoca-Avonmore catchment
- Ireland
- Ochre
- Phosphorus
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