Reaction rates of natural orpiment oxidation at 25 to 40 o C and pH 6.8 to 8.2 and comparison with amorphous As 2 S 3 oxidation

By Lengke M.F.   Tempel R.N.  

Geochimica et Cosmochimica Acta, Vol. 66, Iss. 18, 2002-09 ,pp. : 3281-3291

Elsevier

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Surface oxidation of chalcopyrite (CuFeS 2 ) under ambient atmospheric and aqueous (pH 2-10) conditions: Cu, Fe L- and O K-edge X-ray spectroscopy

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Geochimica et Cosmochimica Acta, Vol. 67, Iss. 12, 2003-06 ,pp. : 2137-2146

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Kinetics of chalcopyrite dissolution at pH 3

By Acero Patricia   Cama Jordi   Ayora Carlos  

European Journal of Mineralogy, Vol. 19, Iss. 2, 2007-03 ,pp. : 173-182

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Low-temperature heat capacity of synthetic Fe- and Mg-cordierite: thermodynamic properties and phase relations in the system FeO-Al₂O₃-SiO₂-(H₂O)

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European Journal of Mineralogy, Vol. 20, Iss. 1, 2008-02 ,pp. : 47-62

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The mechanism, rates and consequences of basaltic glass dissolution: I. An experimental study of the dissolution rates of basaltic glass as a function of aqueous Al, Si and oxalic acid concentration at 25 o C and pH = 3 and 11

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Geochimica et Cosmochimica Acta, Vol. 65, Iss. 21, 2001-11 ,pp. : 3671-3681

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