A remarkable autofragmentation/rearrangement sequence results in the unprecedented formation of inorganic concave cyclic anion [(NiPS4)3]3− (structure shown on the right) upon dissolving the potassium salt of the charged mineral polymer 1∞[NiPS4]− in DMF; the initial complex fluid has a transient anisotropic texture that can be identified by optical microscopy under polarized light. In contrast, the complex fluid that results upon dissolving 1∞[PdPS4]− is stable up to 323 K as persistent, flexible, charged chains.
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Sayettat et al. (1998) studied this question.
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