The phase transitions in β-eucryptite have been investigated by the slow neutron scattering technique. In the temperature range $430<~T<~490$^∘{}C an incommensurate structure is found which coexists with the well-known low-temperature superstructure in the range $430<~T<~482.5$^∘{}C. A pronounced temperature dependence of the satellite positions is observed. Interpretations of the observed scattering are based on a simple model which accounts only for the Li chains within the quartz channels. The width of the diffuse scattering at 525^∘{}C indicates that the Li correlations within a chain are effective over 19 ±{} 3 Li-Li distances while chain-chain correlations are relatively weak. A rather profound analogy to the triangular Ising lattice in the presence of an external field is discussed. At present this model does not explain the incommensurate structure.
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Press et al. (1980) studied this question.
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