Journal of the Japan Institute of Metals and Materials
Online ISSN : 1880-6880
Print ISSN : 0021-4876
ISSN-L : 0021-4876
Further Studies on the Solution Anisotropy and the Shape of Solution Bodies in Tetragonal, Hexagonal, and Rhombohedral Crystals
Mikio Yamamoto
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1956 Volume 20 Issue 7 Pages 396-400

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Abstract

It is shown that the anisotropy of the solution rate along any direction, υ, and that of the radius vestor along the same direction, γ, from the origin to the circumference of a solution body produced from an originally sphere crystal, are generally expressed by υγ=υcγc•cos4θ+(υaγa•cos22φ+υbγb•sin22φ)sin4θ+(4•υdγdcγcaγa)cos2θsin2θ for tetragonal crystals, by υγ=υcγc•cos6θ+(υaγa•cos23φ+υbγb•sin23φ)sin6θ+1/3(24•υdγd-8•υeγe-10•υcγc+3•υaγa)cos4θsin2θ+1/3(-8•υdγd+24•υeγe+3•υcγc-10•υaγa)cos2θsin4θ for hexagonal crystals, and by υγ=υcγc•cos6θ+(υaγa•cos23φ+υbγb•sin23φ)×sin6θ+1/3{12(υdγdgγg)-4(υeγefγf)-10•υcγc+3•υaγa}cos4θsin2θ+1/3{-4(υdγdgγg)+12(υeγefγf)+3υcγc-10υaγa}cos2θsin4θ+(4/√3){-(υdγdgγg)+(υeγefγf)}cosθsin3θcos3φ+(16/3√3){3(υdγdgγg)-(υeγefγf)}cos3θsin3θcos3φ for rhombohedral crystals, where θ and φ are, respectively, the polar and azimuthal angles of the direction referred to a polar coordinate system of which the polar axis and zero line for φ are, respectively, the [001]and [100]axes for tetragonal crystals, the [0001]and [1010]axes for hexagonal crystals, and the [111]and [211]axes for rhombohedral crystals.

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