Abstract
Two problems in the analysis of diffusion-limited aggregation are studied here: the isotropy of the growing aggregate and the meaning of the large-N limit as a practical matter. The isotropy of the aggregate is quantified by the ratio of the radii of gyration of the aggregate about its principal axes. The ratio varies from ∼0.70 for N=200 to 0.90 for N=50000. The next particle capture radius is directionally dependent with respect to the principal axes and scales with the respective radii of gyration. A lower bound is obtained for the size N necessary for the emergence of a single dominant length scale by taking this as the size for which the radii of gyration are equal. In d=2 the lower bound is N1.5×106; in d=3 it is N8×105.