1956 Volume 20 Issue 7 Pages 396-400
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•υdγd-υcγc-υaγa)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(υdγd+υgγg)-4(υeγe+υfγf)-10•υcγc+3•υaγa}cos4θsin2θ+1/3{-4(υdγd+υgγg)+12(υeγe+υfγf)+3υcγc-10υaγa}cos2θsin4θ+(4/√3){-(υdγd-υgγg)+(υeγe-υfγf)}cosθsin3θcos3φ+(16/3√3){3(υdγd-υgγg)-(υeγe-υfγf)}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.