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Gautier, Jean-Marie, Oelkers, Eric H., Schott, Jacques (2001) Are quartz dissolution rates proportional to B.E.T. surface areas?. Geochimica et Cosmochimica Acta, 65 (7) 1059-1070 doi:10.1016/s0016-7037(00)00570-6

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Reference TypeJournal (article/letter/editorial)
TitleAre quartz dissolution rates proportional to B.E.T. surface areas?
JournalGeochimica et Cosmochimica Acta
AuthorsGautier, Jean-MarieAuthor
Oelkers, Eric H.Author
Schott, JacquesAuthor
Year2001 (April)Volume65
Issue7
PublisherElsevier BV
DOIdoi:10.1016/s0016-7037(00)00570-6Search in ResearchGate
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Mindat Ref. ID348358Long-form Identifiermindat:1:5:348358:3
GUID0
Full ReferenceGautier, Jean-Marie, Oelkers, Eric H., Schott, Jacques (2001) Are quartz dissolution rates proportional to B.E.T. surface areas?. Geochimica et Cosmochimica Acta, 65 (7) 1059-1070 doi:10.1016/s0016-7037(00)00570-6
Plain TextGautier, Jean-Marie, Oelkers, Eric H., Schott, Jacques (2001) Are quartz dissolution rates proportional to B.E.T. surface areas?. Geochimica et Cosmochimica Acta, 65 (7) 1059-1070 doi:10.1016/s0016-7037(00)00570-6
In(2001, April) Geochimica et Cosmochimica Acta Vol. 65 (7) Elsevier BV

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Oelkers, Eric H., Schott, Jacques (2001) An experimental study of enstatite dissolution rates as a function of pH, temperature, and aqueous Mg and Si concentration, and the mechanism of pyroxene/pyroxenoid dissolution. Geochimica et Cosmochimica Acta, 65 (8) 1219-1231 doi:10.1016/s0016-7037(00)00564-0
Gautier, Jean-Marie, Oelkers, Eric H, Schott, Jacques (1994) Experimental study of K-feldspar dissolution rates as a function of chemical affinity at 150°C and pH 9. Geochimica et Cosmochimica Acta, 58 (21) 4549-4560 doi:10.1016/0016-7037(94)90190-2
Oelkers, Eric H, Schott, Jacques (1999) Experimental study of kyanite dissolution rates as a function of chemical affinity and solution composition. Geochimica et Cosmochimica Acta, 63 (6) 785-797 doi:10.1016/s0016-7037(98)00294-4
Huertas, F.Javier, Chou, Lei, Wollast, Roland (2001) Kaolinite dissolution rates in batch experiments at room temperature and pressure: reply to “on the interpretation of closed system mineral dissolution experiments,” comment by Eric H. Oelkers, Jacques Schott, and Jean-Luc Devidal. Geochimica et Cosmochimica Acta, 65 (23) 4433-4434 doi:10.1016/s0016-7037(01)00732-3
Oelkers, Eric H., Schott, Jacques, Gauthier, Jean-Marie, Herrero-Roncal, Teresa (2008) An experimental study of the dissolution mechanism and rates of muscovite. Geochimica et Cosmochimica Acta, 72 (20) 4948-4961 doi:10.1016/j.gca.2008.01.040
Oelkers, Eric H., Schott, Jacques, Devidal, Jean-Luc (2001) On the interpretation of closed system mineral dissolution experiments: comment on “Mechanism of kaolinite dissolution at room temperature and pressure part II: kinetic study” by Huertas et al. (1999) Geochimica et Cosmochimica Acta, 65 (23) 4429-4432 doi:10.1016/s0016-7037(01)00735-9
Oelkers, Eric H, Schott, Jacques, Devidal, Jean-Luc (1994) The effect of aluminum, pH, and chemical affinity on the rates of aluminosilicate dissolution reactions. Geochimica et Cosmochimica Acta, 58 (9) 2011-2024 doi:10.1016/0016-7037(94)90281-x
Oelkers, Eric H. (2001) General kinetic description of multioxide silicate mineral and glass dissolution. Geochimica et Cosmochimica Acta, 65 (21) 3703-3719 doi:10.1016/s0016-7037(01)00710-4
Oelkers, Eric H., Schott, Jacques (1995) Experimental study of anorthite dissolution and the relative mechanism of feldspar hydrolysis. Geochimica et Cosmochimica Acta, 59 (24) 5039-5053 doi:10.1016/0016-7037(95)00326-6
GĂ­slason, Sigurdur R., Heaney, Peter J., Oelkers, Eric H., Schott, Jacques (1997) Kinetic and thermodynamic properties of moganite, a novel silica polymorph. Geochimica et Cosmochimica Acta, 61 (6) 1193-1204 doi:10.1016/s0016-7037(96)00409-7
Gout, Robert, Oelkers, Eric H., Schott, Jacques, Wick, Antoine (1997) The surface chemistry and structure of acid-leached albite: New insights on the dissolution mechanism of the alkali feldspars. Geochimica et Cosmochimica Acta, 61 (14) 3013-3018 doi:10.1016/s0016-7037(97)00122-1
 
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