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Hydrogen bonding, thermal expansion, and phase transition of cranswickite (MgSO4 · 4H2O)
Cranswickite and starkeyite are two polymorphs of MgSO₄·4H₂O and are candidate minerals in the hydrated sulfate deposits on Mars. Using neutron powder diffraction, we studied cranswickite’s structure, hydrogen bonding and thermal expansion, and its irreversible transf
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