Preprints
https://doi.org/10.5194/egusphere-2024-3429
https://doi.org/10.5194/egusphere-2024-3429
15 Jan 2025
 | 15 Jan 2025
Status: this preprint is open for discussion and under review for Solid Earth (SE).

High-pressure behaviour and elastic constants of 1M and 2M1 polytypes of phlogopite KMg3Si3AlO10(OH)2

Gianfranco Ulian, Francesca Ranellucci, and Giovanni Valdrè

Abstract. In the present work, the elastic properties of both 1M and 2M1 phlogopite polytypes, KMg3Si3AlO10(OH)2 (monoclinic crystal system) were investigated from PV equation of state fitting and by analysis of the fourth-rank elastic tensor. The analysis was performed within the Density Functional Theory framework, using all-electron Gaussian-type orbitals basis sets and the B3LYP functional corrected a posteriori to include long-range interactions (B3LYP-D*). In general, the elastic properties of the two polytypes were strongly anisotropic, with the axial moduli ratio M(a) : M(b) : M(c) being close to 4 : 4 : 1. The volume-integrated third-order Birch-Murnaghan equation of state fitting parameters at 0 K were K0 = 57.9(2) GPa, K’ = 8.29(7) and V0 = 489.82(3) Å3 for phlogopite-1M, which were very close to those of the 2M1 polytype, i.e., K0 = 58.3(1) GPa, K’ = 8.71(8) and V0 = 978.96(9) Å3. The monoclinic elastic tensors obtained for the two polytypes of phlogopite, which have never been experimentally reported for both minerals so far, were in line with the PV behaviour of the mineral, providing further data related to the directional dependence of the elastic properties and seismic wave propagation. The elastic properties from both PV hydrostatic compression and from the elastic moduli tensor were discussed against the available experimental and theoretical data in the scientific literature, extending the knowledge on this important trioctahedral phyllosilicate.

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Gianfranco Ulian, Francesca Ranellucci, and Giovanni Valdrè

Status: open (until 26 Feb 2025)

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Gianfranco Ulian, Francesca Ranellucci, and Giovanni Valdrè
Gianfranco Ulian, Francesca Ranellucci, and Giovanni Valdrè

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Short summary
Layer silicates (phyllosilicates) are important minerals because of their ubiquity on the Earth’s crust and due to their ability to release water in the mantle. The present study focuses on the elastic properties of a specific phyllosilicate known as phlogopite [KMg3Si3AlO10(OH)2], which were characterised using first-principles methods. The results show the mineral's anisotropic mechanical behaviour, which also depends on how the mineral layers are stacked in the crystal structure.