Are quartz dissolution rates proportional to B.E.T. surface areas

By J. Gautier, E. Oelkers, J. Schott. 2001

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The effects of organic acids on the dissolution of silicate minerals: A case study of oxalate catalysis of kaolinite dissolution (2006, unknown): “Several studies (e.g., Walther, 1996; Gautier et al., 2001) indicated that the amount of time prior to steady state may influence the resulting steady-state dissolution rate.”
EUROPIUM RETENTION ONTO CLAY MINERALS FROM 25 TO 150°C: EXPERIMENTAL MEASUREMENTS, SPECTROSCOPIC FEATURES AND SORPTION MODELLING. (2006, methodology): “The quartz sample is the 50-125 µm size fraction of the sample previously used by Gautier et al. (2001), with a BET surface of 0.061 m2.g-1.”
Impact of coating development on the hydraulic and transport properties in argillaceous limestone fracture (2007, background): “Gautier et al. [2001] suggested that the observed increase in surface should be related to an increase in pit surface which is little or nonreactive.”
Olivine dissolution rates: A critical review (2018, background): “A similar behavior was found for quartz dissolution by Gautier et al. (2001), which was attributed by these authors to the fact that the surface area increase observed during etch pit formation consisted of relatively unreactive etch pit walls.”