Local Structure and Crystallization Transformation of Hydrous Ferric Arsenate in Acidic H2O–Fe(III)–As(V)–SO42– Systems: Implications for Acid Mine Drainage and Arsenic Geochemical Cycling
Hydrous ferric arsenate (HFA) is a common thermodynamically metastable phase in acid mine drainage (AMD). However, little is known regarding the structural forms and transformation mechanism of HFA. We investigated the local atomic structures and the crystallization transformation of HFA at various...
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Veröffentlicht in: | Environmental science & technology 2024-04, Vol.58 (16), p.7176-7185 |
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Sprache: | eng |
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