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1 CEA-DEN, Service de Chimie et Physique Analytique, CE Saclay, 91191 Gif-sur-Yvette, France. Tel. : +33-1-69-08-73-60; fax : +33-1-69-08-32-42 ; e-mail : michael.descostes{at}cea.fr.
2 Université Paris 7, Laboratoire de Géochimie des Eaux, 75251 Paris cedex 05, France.
3 IPSN, Service dEtudes et de Recherches sur la Géosphère et lélimination des Déchets, 92265 Fontenay-aux-Roses, France.
4 CNRS-UMR 8587, CE Saclay, 91191 Gif-sur-Yvette, France.
Abstract
Neutralization by carbonate of acidification generated by pyrite (FeS2) oxidation was investigated by both solution (iron and sulfur speciation, pH and Eh) and solid (FT-IR) characterizations. Batch dissolution experiments were carried out in contact with atmospheric oxygen (20 %) in four different bicarbonated solutions ([NaHCO3]=103, 1,12.102, 101 and 1 mol/L). Five different contact duration were selected : 6 hours, 1, 3, 8 and 30 days. Ferrous carbonate complexes (FeOHCO3 and Fe(CO3 )22 ) tend to maintain iron in solution (up to 152.2 µmol/L in [NaHCO3]=1 mol/L solution) and to increase pyrite oxidation rate by preventing surface coating. Acidification is thus more intense in diluted and concentrated carbonate medium ([NaHCO3 ] =103 and 1 mol/L) with respectively
pH=5.06 and
pH=1.99 at 30 days whereas pH remains buffered in [NaHCO3 ] =1.12.102 and 0.1 mol/L solutions. Siderite appears to be the first solid precipitating, transforming into g
thite, oxyhydroxy ferric sulfate incorporating sulfite and thiosulfate, and then lepidocrocite. Sulfur chemistry controls the acidification observed. Thiosulfate is the first sulfoxyanion released in solution and its oxidation into sulfite then sulfate seems to be the key of acidification production. Thus, carbonate pH buffer properties seem to be limited and effective for moderated carbonate concentrations.
Key Words: Pyrite Oxidation Carbonate pH buffer FTIR Redox
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