Abstract
Polythermic single-crystal X-ray studies of chalcocyanite CuSO4, dolerophanite Cu2OSO4, and kamchatkite KCu3O(SO4)2Cl have established their melting points as well as peculiarities of their thermal expansion. Association of oxocentered and sulfate tetrahedra in dolerophanite and kamchatkite leads to the formation of rigid tetrahedral “backbones” only slightly sensitive to thermal variations. Rigid complexes can also be distinguished in the structure of chalcocyanite, if we consider only the system of the shortest and strongest Cu–O and S–O bonds. The anisotropy of the thermal expansion can be explained by either rigid complexes drifting parallel to each other (as in dolerophanite and chalcocyanite), or radial and angular distortions in the polyhedra of alkali cations. The presence of a tetrahedrally coordinated additional oxygen atom in the structure of dolerophanite and kamchatkite leads to an increase in the principal eigenvalues. The demonstrated rigidity of the sulfate tetrahedra in studied anhydrous copper sulfate minerals explains the absence of phase transitions up to the melting temperatures. The variation of chemical composition leads to changes in their thermal decomposition points. Chlorine-containing kamchatkite decomposes at the lowest temperature of 590(5) K, next are chalcocyanite 675(10) K, and dolerophanite 925(10) K.
Similar content being viewed by others
Data availability
Not applicable.
References
Berlepsch P, Armbruster T, Brugger J, Bykova EY, Kartashov PM (1999) The crystal structure of vergasovaite Cu3O[(Mo, S)O4SO4], and its relation to synthetic Cu3O[MoO4]2. Eur J Mineral 11:101–110
Downs RT (2000) Analysis of harmonic displacement factors. In: Hazen RM, Downs RT (eds) High-temperature and high-pressure crystal chemistry, vol 41. Rev Mineral Geochem, pp 61–87
Effenberger H (1985) Cu2O(SO4), dolerophanite: refinement of the crystal structure with a comparison of [OCu(II)4] tetrahedra in inorganic compounds. Monatsh Chem 116:927–931
Jacobsen SD, Smyth JR, Swope RJ, Downs RT (1998) Rigid-body character of the SO4 groups in celestine, anglesite and barite. Can Mineral 36:1053–1060
Krivovichev SV, Mentré O, Siidra OI, Colmont M, Filatov SK (2013) Anion-centered tetrahedra in inorganic compounds. Chem Rev 113:6459–6535
Nazarchuk EV, Siidra OI, Charkin DO, Nikolaevich GV, Borisov AS, Ugolkov VL (2023) Vergasovaite to cupromolybdite topotactic transformation with crystal shape preservation. Am. Mineral. Accepted
Pekov IV, Zubkova NV, Pushcharovsky DYu (2018) Copper minerals from volcanic exhalations–a unique family of natural compounds: crystal-chemical review. Acta Crystallogr B 74(6):502–518
Siidra OI, Nazarchuk EV, Zaitsev AN, Lukina EA, Avdontseva EY, Vergasova LP, Vlasenko NS, Filatov SK, Turner R, Karpov GA (2017) Copper oxosulphates from fumaroles of Tolbachik Vulcano: puninite, Na2Cu3O(SO4)3—a new mineral species and structure refinements of kamchatkite and alumoklyuchevskite. Eur J Miner 29:499–510
Siidra OI, Borisov AS, Lukina AA, Depmeier W, Platonova NV, Colmont M, Nekrasova DO (2019) Reversible hydration/dehydration and thermal expansion of euchlorine, ideally KNaCu3O(SO4)3. Phys Chem Minerals 46:403–416
Siidra OI, Borisov AS, Charkin DO, Depmeier W, Platonova NV (2021) Evolution of fumarolic anhydrous copper sulfate minerals during successive hydration/dehydration. Mineral Mag 85:262–277
Vergasova LP, Filatov SK (2012) New mineral species in products of fumarole activity of the Great Tolbachik Fissure Eruption. J Volcanol Seismol 6:281–289
Vergasova LP, Filatov SK (2016) A study of volcanogenic exhalation mineralization. J Volcanol Seismol 10:71–85
Wildner M, Giester G (1988) Crystal structure refinements of synthetic chalcocyanite (CuSO4) and zincosite (ZnSO4). Miner Petrol 39:201–209
Acknowledgements
We are grateful to Pietro Vignola and one anonymous reviewer for their valuable comments that led to improvement of the initial version of the manuscript. Technical support by the St. Petersburg State University X-ray Diffraction Resource Centre is gratefully acknowledged.
Funding
The research was supported within the scientific task # 0081-2022-0002.
Author information
Authors and Affiliations
Contributions
All authors have equally contributed to the work described. EVN, OIS, DOC, SKF: MS preparation and analysis of the data. EVN, OIS, LRZ: HT single-crystal X-ray diffraction and interpretation. OIS, EVN: sampling of minerals from the Yadovitaya fumarole.
Corresponding author
Ethics declarations
Conflict of interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
Ethical approval
Not applicable.
Additional information
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Supplementary Information
Below is the link to the electronic supplementary material.
Rights and permissions
Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.
About this article
Cite this article
Nazarchuk, E.V., Siidra, O.I., Filatov, S.K. et al. Thermal expansion of anhydrous copper sulfate minerals determined by single crystal X-ray diffraction: chalcocyanite CuSO4, dolerophanite Cu2OSO4 and kamchatkite KCu3O(SO4)2Cl. Phys Chem Minerals 50, 11 (2023). https://doi.org/10.1007/s00269-023-01236-7
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s00269-023-01236-7