Fractal structure of fullerite

被引：8

作者：

Zolotukhin, IV ^{[1
]}

Yanchenko, LI ^{[1
]}

Belonogov, EK ^{[1
]}

机构：

[1] Voronezh State Tech Univ, Voronezh 394026, Russia

来源：

JETP LETTERS | 1998年 / 67卷 / 09期

关键词：

81.05.Tp; 61.43.Hv; 61.48.1c;

D O I：

10.1134/1.567707

中图分类号：

O4 [物理学];

学科分类号：

0702 ;

摘要：

We have obtained macroscopic fractal aggregates of fullerite ranging in size from 100 to 400 mu m. The fractal structure of fullerite is formed by microscopic (30-100 nm) fullerite crystals in the presence of a temperature gradient under conditions of diffusion-limited aggregation. (C) 1998 American Institute of Physics. [S0021-3640(98)01404-1].

引用

页码：720 / 722

页数：3