MECHANISM OF THE TRANSITION FROM FRACTAL TO DENDRITIC GROWTH OF SURFACE AGGREGATES

Citation
H. Brune et al., MECHANISM OF THE TRANSITION FROM FRACTAL TO DENDRITIC GROWTH OF SURFACE AGGREGATES, Nature, 369(6480), 1994, pp. 469-471
Citations number
21
Categorie Soggetti
Multidisciplinary Sciences
Journal title
NatureACNP
ISSN journal
00280836
Volume
369
Issue
6480
Year of publication
1994
Pages
469 - 471
Database
ISI
SICI code
0028-0836(1994)369:6480<469:MOTTFF>2.0.ZU;2-K
Abstract
THE similarity of many patterns formed in non-equilibrium growth proce sses in physics, chemistry and biology is conspicuous, and many attemp ts have been made to discover common mechanisms underlying their forma tion(1). A central question is what causes some patterns to be dendrit ic (symmetrically branched, like snowflakes) and others fractal (rando mly ramified). In general, the transition from fractal to dendritic gr owth is regarded as a manifestation of the predominance of anisotropy over random noise in the growth process. In electrochemical deposition , this transition is observed as the growth speed is varied(2,3). Here we report a crossover from fractal to dendritic growth in two dimensi ons on the microscopic scale. We use the scanning tunnelling microscop e to study diffusion-limited aggregation of silver atoms on a Pt(111) surface. The transition occurs as the deposition flux is increased, an d our observations suggest that the increasing importance of anisotrop y of edge diffusion at higher flux is responsible for this crossover. We anticipate that a similar phenomenon may operate in three-dimension al crystal growth.