Investigation of acidic dissolution of mixed clays between pH 1.0 and −3.0 using Si and Al X-ray absorption near edge structure
Although widely investigated in relation to acid mine drainage systems at pH > 1.0, we know little about the impact of sulfuric acid (H 2SO 4) on the geochemistry and mineralogy of clays at pH < 1.0 (including negative pH values). Thus, laboratory batch experiments were conducted on three mixe...
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Veröffentlicht in: | Geochimica et cosmochimica acta 2009-07, Vol.73 (14), p.4151-4165 |
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Format: | Artikel |
Sprache: | eng |
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