Abstract
The erosion of agglomerates in viscous flows—a process proportional to surface area of the agglomerate—is analyzed by means of fragmentation theory. An analytical solution is obtained; this solution cannot be described by the usual scaling ansatz, nor does it have an asymptotic form. Fitting to available data is discussed. © 1996 The American Physical Society.
- Received 25 October 1995
DOI:https://doi.org/10.1103/PhysRevE.53.4209
©1996 American Physical Society
