(Q57701457)

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Kinetics and mechanism of forsterite dissolution at 25°C and pH from 1 to 12

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Kinetics and mechanism of forsterite dissolution at 25°C and pH from 1 to 12 (English)

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Oleg S Pokrovsky

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Jacques Schott

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2

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Jacques Schott

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publication date

October 2000

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published in

Geochimica et Cosmochimica Acta

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volume

64

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issue

19

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page(s)

3313-3325

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cites work

The Relationship between Fluids in Some Fresh Alpine-Type Ultramafics and Possible Modern Serpentinization, Western United States

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7 January 2021

Carbon dioxide mediated dissolution of Ca-feldspar: implications for silicate weathering

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7 January 2021

Role of surface speciation in the low-temperature dissolution of minerals

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7 January 2021

Leaching and reconstruction at the surfaces of dissolving chain-silicate minerals

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7 January 2021

Dolomite surface speciation and reactivity in aquatic systems

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7 January 2021

Forsterite surface composition in aqueous solutions: a combined potentiometric, electrokinetic, and spectroscopic approach

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7 January 2021

Olivine dissolution at 25°C: Effects of pH, CO2, and organic acids

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7 January 2021

Olivine dissolution kinetics at near-surface conditions

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reference URL

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7 January 2021

Identifiers

DOI

10.1016/S0016-7037(00)00434-8

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ADS bibcode

2000GeCoA..64.3313P

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(Q57701457)

Kinetics and mechanism of forsterite dissolution at 25°C and pH from 1 to 12

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