Abstract

Since being discovered initially in mixed-cation systems, a method of forming end-member NiSO4·9H2O and NiSO4·8H2O has been found. We have obtained powder diffraction data from protonated analogues (with X-rays) and deuterated analogues (using neutrons) of these compounds over a range of temperatures, allowing us to determine their crystal structures—including all H-atoms—and to characterise the transitions on warming from 220 to 278 K; glass → 9-hydrate → 8-hydrate + ice → 7-hydrate + ice → partial melt (7-hydrate + liquid). NiSO4·8D2O is triclinic, space-group Pbar {1}, Z = 2, with unit cell parameters at 150 K, a = 6.12463(8) Å, b = 6.8401(1) Å, c = 12.5339(2) Å, α = 92.846(1)°, β = 97.822(1)°, γ = 96.627(1)° and V = 515.58(1) Å3. The structure consists of two symmetry-inequivalent Ni(D2O)6 octahedra on sites of bar {1} symmetry. These are directly joined by a water–water H-bond to form chains of octahedra parallel with the c-axis at x = 0. Two interstitial water molecules serve both to bridge the Ni(D2O)6 octahedral chains in the b–c plane and also to connect with the SO42− tetrahedral oxyanion. These tetrahedra are linked by the two interstitial water molecules in a reticular motif to form sheets perpendicular to c. NiSO4·9D2O is monoclinic, space-group P21/c, Z = 4, with unit-cell parameters at 150 K, a = 6.69739(6) Å, b = 11.8628(1) Å, c = 14.5667(1) Å, β = 94.9739(8)° and V = 1152.96(1) Å3. The structure is isotypic with the Mg analogue described elsewhere (Fortes et al., Acta Cryst B 73:47‒64, 2017b). It shares the motif of H-bonded octahedral chains with NiSO4·8D2O, although in the enneahydrate these run parallel with the b-axis at x = 0. Three interstitial water molecules bridge the Ni(D2O)6 octahedra to the SO42− tetrahedral oxyanion. The tetrahedra sit at x ≈ 0.5 and are linked by two of the three interstitial water molecules in a pentagonal motif to form ribbons parallel with b. A solid-solution series exists between Mg and Ni enneahydrate end-members where we observe preferential partitioning of Ni2+ into the octahedral sites on the 2c Wyckoff positions rather than the 2a sites. The solution is slightly non-ideal, as indicated by the small positive excess volume of mixing. Measurements of the DC magnetisation of quenched NiSO4 solutions reveal anomalies in the molar susceptibility on warming through the region from 221 to 225 K, probably due to devitrification of the (assumed) glassy specimen into a mixture of NiSO4·9H2O + ice Ih. Further temperature-dependent measurements on repeated warming and cooling provide no evidence of magnetic ordering and indicate a weak ferromagnetic coupling between neighbouring Ni2+ ions, likely via super-exchange through the H-bond between neighbouring Ni(H2O)6 octahedra.

Highlights

  • BackgroundCrystalline hydrates having the general formula N­ iSO4·nH2O with n = 1, 2, 3, 4, 5, 6, and 7 are well known (Chrétien and Rohmer 1934), some of which occur naturally as the minerals dwornikite (n = 1, with ~ 10 atom % ­Fe2+), retgersite and nickelhexahydrite, and morenosite (n = 7), respectively

  • Since we consider the formation of a single-phase and icefree specimen of N­ iSO4·8H2O to be practically impossible by flash-freezing of a stoichiometric aqueous solution, and since the metastability of this phase precludes growth, extraction or handling of even small crystals suitable for either X-ray single-crystal diffraction or thermogravimetric analysis, the only way to confirm the stoichiometry is to solve the structure from mixed-phase powder diffraction data

  • In achieving that goal we will show that this phase is an octahydrate; along with the structure refinement of nickel sulfate enneahydrate reported in this work, these are the first new N­ iSO4 hydrate structures to be established with certainty in over 80 years

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Summary

Introduction

Whilst we failed to form the ­NiSO4·11H2O end-member, we succeeded instead in producing a novel hydrate with n = 9 in systems containing mixtures of Ni, Zn or Fe with Mg, and a new hydrate with n = 8 in pure ­NiSO4 (Fortes et al 2012a, b). We have been able to form end-member 9-hydrates from each of M­ gSO4, ­NiSO4 and ­ZnSO4. We were quite cautious in our assertion that the newly identified hydrate of ­NiSO4 was an octahydrate based solely on molar volume considerations. In achieving that goal we will show that this phase is an octahydrate; along with the structure refinement of nickel sulfate enneahydrate reported in this work, these are the first new N­ iSO4 hydrate structures to be established with certainty in over 80 years

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