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a Escuela Politécnica Superior, Departamento de Edafología y Química Agrícola, Universidad de Santiago de Compostela, Campus Universitario, 27002 Lugo, Spain
b Facultad de Farmacia, Departamento de Edafología y Química Agrícola, Universidad de Santiago de Compostela, Campus Sur, 15706 Santiago de Compostela, Spain
* Corresponding author (seoane{at}lugo.usc.es)
Received for publication May 22, 2000. A laboratory experiment was conducted to investigate the long-term effects of amending sulfide-rich lignite mine spoil with fly ash (originating from a coal-fired power station and largely comprised of aluminosilicates) and/or agricultural limestone. The experiment was carried out with soil moisture maintained at field capacity or alternate cycles of wetting and drying. Results obtained suggest that the principal acidification processes were oxidation of sulfide and formation of hydroxysulfate (FeOHSO4), whereas the main neutralization processes were weathering of aluminosilicates in fly ashtreated samples and dissolution of calcium carbonate in limestone-treated samples. The highest dose of limestone rapidly raised the pH of the spoil, but this increase was not maintained throughout the one-year experiment. In contrast, fly ashtreated samples showed a more sustained increase in pH, attributable to the gradual weathering of aluminosilicates. The best results (i.e., good short- and long-term neutralization) were obtained in samples treated with both fly ash and limestone. The low liming capacity of the fly ash (47.85 cmol kg-1) means that it must be used in large quantities, an advantage in achieving the further aim of disposing of the fly ash.
Abbreviations: FC, field capacity SI, saturation index WD, wettingdrying cycles
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