摘要
(Figure Presented) Fractal hematite dendrites with structures resembling pine trees (see picture) were obtained by hydrothermal treatment of K 3[Fe(CN)6]. They are formed by a novel process in which fast growth along six crystallographically equivalent directions forms dendritic or snowflakelike single-crystal structures, which differs from the mechanisms reported for other fractal structures.
源语言 | 英语 |
---|---|
页(从-至) | 4197-4201 |
页数 | 5 |
期刊 | Angewandte Chemie - International Edition |
卷 | 44 |
期 | 27 |
DOI | |
出版状态 | 已出版 - 4 7月 2005 |
指纹
探究 'Single-crystal dendritic micro-pines of magnetic α-Fe 2O3: Large-scale synthesis, formation mechanism, and properties' 的科研主题。它们共同构成独一无二的指纹。引用此
Cao, M., Liu, T., Gao, S., Sun, G., Wu, X., Hu, C., & Zhong, L. W. (2005). Single-crystal dendritic micro-pines of magnetic α-Fe 2O3: Large-scale synthesis, formation mechanism, and properties. Angewandte Chemie - International Edition, 44(27), 4197-4201. https://doi.org/10.1002/anie.200500448