LaNiO3 is locally distorted to orthorhombic at room temperature, and further to monoclinic at 200 K from globally rhombohedral structure. Such local rhombohedral phase hosts uncorrelated singlets, resulting in a pseudogap. Consequently, a crossover emerges at the rare earth nickelates phase diagram from fully gapped monoclinic long-range order to pseudogap monoclinic short-range order, as the radius of rare earth ions increases.
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Li et al. (2015) studied this question.
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