Pressure-induced dehydration transitions of CoSO4·6H2O and CoSO4·7H2O were observed by in-situ powder X-ray diffraction at high pressure. Both transformed to an unreported high-pressure phase, CoSO4·5H2O at 1–2 GPa, whose crystal structure was determined by single crystal X-ray diffraction. The results show that CoSO4·5H2O has a triclinic structure with cell parameters of a = 6.4436 (6) Å, b = 10.2300 (12) Å, c = 5.1914 (6) Å, α = 91.953 (10)°, β = 87.084 (10)°, γ = 101.085 (10)°, V = 335.28 (6) Å3, at 1.3 GPa, and it has a layered crystal structure consisting of [Co(H2O)6] and [Co(H2O)4(SO4)2]. This structure is distinct from previously reported crystal structures of MSO4·5H2O (M = Mg, Mn, Fe, Cu) in a metal coordination environment. The compressibility of CoSO4·5H2O was fitted by the 3rd-order Birch-Murnaghan equation of state, yielding K0 = 25 (±2) GPa, K0′ = 7.4 (±0.5), V0 = 352 (±2) Å3.
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