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通过水热法制备粉体的实验观察到金红石、锐钛矿和α-Al2O3晶体的生长习性.采用配位多面体生长习性法则合理地解释了Ti O2和α-Al2O3的生长习性.其主要结果为α-Al2O3晶体的生长习性为平板{0001},其各晶面的生长速度为:V{0001 }<V{1123};锐钛矿的生长习性为四面体,其各晶面的生长速度为V<010>=V<001>>V<010>>V<111>.而PBC理论很难合理地解释α-Al2 O3晶体的生长习性.

The observed growth habit of TiO2, α-Al2 O3 crystals observed under hydrothermal conditions were successfully explained by the coordination polyhedron rule concerning growth habit. It is concluded that the habit of α-Al2 O3 crystal is the hexagonal platy {0001}, and the relationship of growth rate of various faces is: V{0001} < V{1123} < V{0112} < V{1120} < V{1010}; the growth habit of rutile (TiO2) crystal is elongated prismatic form, and the relationship of growth rate of various faces is: V<110> < V<100> < V<101> < V<001> < V<111>; the growth habit of anatase (TiO2) crystal is a tetrahedron, and the relationship of growth rate of various faces is:V<010> = V<001> > V<010> > V<111>. These results were compared with previous studies based on PBC theory.

参考文献

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