Theory of magnetic properties of solid oxygen
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Annotatsiya
It is shown that the entire set of data on the behavior of solid oxygen can be explained consistently by assuming that its magnetic subsystem is a quasi-two-dimensional Heisenberg system, whose structure changes with increasing temperature as follows: The α-phase has a quasi-two-dimensional collinear antiferromagnetic structure; in a narrow temperature range near the α–β transition there is a quasi-two-dimensional structure with helicoidal packing which, as the degree of lattice monoclinicity decreases, transforms continuously into a three-sublattice structure, as short-range order persists in the whole range of existence of the β-phase.
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