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Data from controlled laboratory rock-dissolution experiments are presented. Material used in these experiments consisted of two size fractions of ground welded tuff from Snowshoe Mountain near Creede, Colorado, and two size fractions of a reactive-mineral component of the welded tuff, an augite. Dissolution experiments were performed under acidic conditions with pH ranging from 1 to about 6.7. Several experimental configurations were used to obtain data for evaluating the effect of rock dispersion in the reacting solution on the dissolution-reaction kinetics.

Data from laboratory dissolution experiments using a welded tuff from Snowshoe Mountain near Creede, Colorado