“…One great strength of AFM is that it characterizes surface microtopography directly in solution. Thus it can track the progress of reactions such as mineral growth, dissolution, and heterogeneous precipitation as they occur (Drake et al, 1989;Hillner et al, 1992;Dove and Hochella, 1993;Bosbach and Rammensee, 1994;Dove and Chermak, 1994;Junta and Hochella, 1994;Bosbach et al, 1995;Putnis et al, 1995;Grantham and Dove, 1996;Liang et al, 1996;Junta-Rosso et al, 1997). However, none of the above real-time, in situ studies involved clay minerals because the standard sample preparation techniques used to fix clay particles for AFM characterization in air are inadequate for fluid-cell applications (Dove and Chermak, 1994).…”