Quantitative assessment of reactive surface area of phlogopite during acid dissolution
The reactive surface area of a dissolving sheet silicate, phlogopite, was quantitatively assessed in experiments performed in the fluid cell of an atomic force microscope at room temperature and pH values of 2 and 5.7. Additional assessment was provided by surface chemical analysis and electron diffraction. Dissolution rates of phlogopite hk0 edges are in the range of 10(-10) moles per square meters per second, two orders of magnitude faster than bulk rates for this mineral. The basal 001 surfaces also show distinct reactivity, although it is short-lived before they become relatively inert. These basal surfaces are shown to leach, hydrate, and expand to an amorphous silica-enriched film.
Rufe
E
Department of Geological Sciences, Virginia Polytechnic Institute and State University, Blacksburg, VA 24061-0420, USA.
Hochella
MF