Abstract
This paper discusses the statistical mechanics of ferromagnetic and antiferromagnetic systems in the presence of uniaxial anisotropy, which is included both as anisotropic exchange DijSizSjz and in the form of single-ion crystal-field terms D0(Siz)2. Emphasis is given to the calculation of magnetic transition temperatures TN and particularly to a discussion of the sensitivity of TN to crystal-field anisotropy. Earlier efforts in this direction have produced widely varying results, some Green's-function calculations predicting a sensitivity fully ten times the equivalent molecular-field result. A Green's-function theory is developed for which the decoupling of anisotropy terms is carried out in a manner which is essentially consistent with the random-phase decoupling of exchange terms, at least in the limit of small anisotropy. As such, the theory is an improvement on earlier decoupling schemes and allows, in particular, for a value of (Sz)2 at TN, which differs from the isotropic result 13S(S+1). It indicates a sensitivity of TN to D0 which is smaller than suggested by earlier Green's-function theories but still considerably larger than given by molecular-field theory. Quantitative calculations are carried out for simple cubic and body-centered cubic lattices and the detailed results for the different theories are compared. In Paper II the theory is applied to the salt FeF2 for which the spin Hamiltonian contains a sizeable crystal-field anisotropy of the form D0(Siz)2.