Assessing aluminium toxicity in streams affected by acid mine drainage

2013 ◽  
Vol 67 (8) ◽  
pp. 1764-1772 ◽  
Author(s):  
A. S. Waters ◽  
J. G. Webster-Brown

Acid mine drainage (AMD) has degraded water quality and ecology in streams on the Stockton Plateau, the site of New Zealand's largest open-cast coal mining operation. This has previously been attributed largely to the effects of acidity and elevated aluminium (Al) concentrations. However, the toxicity of dissolved Al is dependent on speciation, which is influenced by pH which affects Al hydrolysis, as well as the concentrations of organic carbon and sulphate which complex Al. Methods for the assessment of the toxic fraction of Al, by chemical analysis and geochemical modelling, have been investigated in selected streams on the Stockton Plateau, where dissolved Al concentrations ranged from 0.034 to 27 mg L−1. Modelling using PHREEQC indicated that between 0.2 and 85% of the dissolved Al was present as the free ion Al3+, the most toxic Al species, which dominated in waters of pH = 3.8–4.8. Al-sulphate complexation reduced the Al3+ concentration at lower pH, while Al-organic and –hydroxide complexes dominated at higher pH. Macroinvertebrate richness in the streams identified an Al3+ ‘threshold’ of approximately 0.42 mg/L, above which taxa declined rapidly. Colorimetric ‘Aluminon’ analysis on unpreserved, unfiltered waters provided a better estimation of Al3+ concentrations than inductively couple plasma–mass spectrometry (ICP-MS) on filtered, acidified waters. The Aluminon method does not react with particulate Al or strong Al complexes, often registering as little as 53% of the dissolved Al concentration determined by ICP-MS.

2016 ◽  
Vol 8 (40) ◽  
pp. 7420-7426 ◽  
Author(s):  
Resongles E. ◽  
Le Pape P. ◽  
Fernandez-Rojo L. ◽  
Morin G. ◽  
Delpoux S. ◽  
...  

As(iii)/As(v) ratio determined from orthophosphoric acid extraction/HPLC-ICP-MS matched XANES results, allowing routine measurement of As oxidation state in acid mine drainage precipitates.


Clay Minerals ◽  
2009 ◽  
Vol 44 (1) ◽  
pp. 113-123 ◽  
Author(s):  
O. Fenton ◽  
M. G. Healy ◽  
M. Rodgers ◽  
D. O Huallacháin

AbstractAcid 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.


2016 ◽  
Vol 07 (02) ◽  
pp. 160-169 ◽  
Author(s):  
Shinji Matsumoto ◽  
Hideki Shimada ◽  
Takashi Sasaoka ◽  
Ginting J. Kusuma ◽  
Rudy S. Gautama

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