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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

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Reference TypeJournal (article/letter/editorial)
TitleGeneral kinetic description of multioxide silicate mineral and glass dissolution
JournalGeochimica et Cosmochimica Acta
AuthorsOelkers, Eric H.Author
Year2001 (November)Volume65
Issue21
PublisherElsevier BV
DOIdoi:10.1016/s0016-7037(01)00710-4Search in ResearchGate
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Mindat Ref. ID348240Long-form Identifiermindat:1:5:348240:1
GUID0
Full ReferenceOelkers, 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
Plain TextOelkers, 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
In(2001, November) Geochimica et Cosmochimica Acta Vol. 65 (21) Elsevier BV

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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
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
Oelkers, Eric H., Gislason, Sigurdur R. (2001) 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°C and pH = 3 and 11. Geochimica et Cosmochimica Acta, 65 (21) 3671-3681 doi:10.1016/s0016-7037(01)00664-0
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
Ragnarsdottir, K.Vala, Fournier, Patricia, Oelkers, Eric H., Harrichoury, Jean-Claude (2001) Experimental determination of the complexation of strontium and cesium with acetate in high-temperature aqueous solutions. Geochimica et Cosmochimica Acta, 65 (21) 3955-3964 doi:10.1016/s0016-7037(01)00725-6
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
Fletcher, Raymond C., Merino, Enrique (2001) Mineral growth in rocks: kinetic-rheological models of replacement, vein formation, and syntectonic crystallization. Geochimica et Cosmochimica Acta, 65 (21) 3733-3748 doi:10.1016/s0016-7037(01)00726-8
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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
Gislason, Sigurdur R., Oelkers, Eric H. (2003) Mechanism, rates, and consequences of basaltic glass dissolution: II. An experimental study of the dissolution rates of basaltic glass as a function of pH and temperature. Geochimica et Cosmochimica Acta, 67 (20) 3817-3832 doi:10.1016/s0016-7037(03)00176-5
 
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