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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

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Reference TypeJournal (article/letter/editorial)
TitleAn 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
JournalGeochimica et Cosmochimica Acta
AuthorsOelkers, Eric H.Author
Schott, JacquesAuthor
Year2001 (April)Volume65
Issue8
PublisherElsevier BV
DOIdoi:10.1016/s0016-7037(00)00564-0Search in ResearchGate
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Mindat Ref. ID348367Long-form Identifiermindat:1:5:348367:5
GUID0
Full ReferenceOelkers, 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
Plain TextOelkers, 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
In(2001, April) Geochimica et Cosmochimica Acta Vol. 65 (8) Elsevier BV

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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
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
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
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, 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 (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
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. (2001) An experimental study of forsterite dissolution rates as a function of temperature and aqueous Mg and Si concentrations. Chemical Geology, 175 (3) 485-494 doi:10.1016/s0009-2541(00)00352-1
Saldi, Giuseppe D., Schott, Jacques, Pokrovsky, Oleg S., Oelkers, Eric H. (2010) An experimental study of magnesite dissolution rates at neutral to alkaline conditions and 150 and 200°C as a function of pH, total dissolved carbonate concentration, and chemical affinity. Geochimica et Cosmochimica Acta, 74 (22) 6344-6356 doi:10.1016/j.gca.2010.07.012
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
 
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