Molecular-level mechanisms of quartz dissolution under neutral and alkaline conditions in the presence of electrolytes
Author:
Publisher
Geochemical Society of Japan
Subject
Geochemistry and Petrology,Geophysics
Reference70 articles.
1. Bandstra, J. Z. and Brantley, S. L. (2008) Surface evolution of dissolving minerals investigated with a kinetic ising model. Geochim. Cosmochim. Acta 72, 2587-2600.
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3. Berger, G., Cadore, E., Schott, J. and Dove, P. M. (1994) Dissolution rate of quartz in lead and sodium electrolyte solutions between 25 and 300-degrees-C: Effect of the nature of surface complexes and reaction affinity. Geochim. Cosmochim. Acta 58, 541-551.
4. Bickmore, B. R., Wheeler, J. C., Bates, B., Nagy, K. L. and Eggett, D. L. (2008) Reaction pathways for quartz dissolution determined by statistical and graphical analysis of macroscopic experimental data. Geochim. Cosmochim. Acta 72, 4521-4536.
5. Blum, A. E. and Lasaga, A. C. (1988) Role of surface speciation in the low-temperature dissolution of mineral. Nature 331, 431-433.
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