High-pressure thermo-elastic properties of beryl (Al4Be6Si12O36) from ab initio calculations,and observations about the source of thermal expansion |
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Authors: | Mauro?Prencipe author-information" > author-information__contact u-icon-before" > mailto:mauro.prencipe@unito.it" title=" mauro.prencipe@unito.it" itemprop=" email" data-track=" click" data-track-action=" Email author" data-track-label=" " >Email author,Isacco?Scanavino,Fabrizio?Nestola,Marco?Merlini,Bartolomeo?Civalleri,Marco?Bruno,Roberto?Dovesi |
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Affiliation: | 1.Dipartimento di Scienze Mineralogiche e Petrologiche,Università di Torino,Torino,Italy;2.Dipartimento di Mineralogia e Petrologia,Università di Padova,Padova,Italy;3.Dipartimento di Scienze della Terra, Sezione di Mineralogia, Petrografia, Geochimica e Giacimenti Minerari,Università di Milano,Milano,Italy;4.Dipartimento di Chimica IFM e NIS-Centre of excellence,Università di Torino,Torino,Italy |
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Abstract: | Ab initio calculations of thermo-elastic properties of beryl (Al4Be6Si12O36) have been carried out at the hybrid HF/DFT level by using the B3LYP and WC1LYP Hamiltonians. Static geometries and vibrational frequencies were calculated at different values of the unit cell volume to get static pressure and mode-γ Grüneisen’s parameters. Zero point and thermal pressures were calculated by following a standard statistical-thermodynamics approach, within the limit of the quasi-harmonic approximation, and added to the static pressure at each volume, to get the total pressure (P) as a function of both temperature (T) and cell volume (V). The resulting P(V, T) curves were fitted by appropriate EoS’, to get bulk modulus (K 0) and its derivative (K′), at different temperatures. The calculation successfully reproduced the available experimental data concerning compressibility at room temperature (the WC1LYP Hamiltonian provided K 0 and K′ values of 180.2 Gpa and 4.0, respectively) and the low values observed for the thermal expansion coefficient. A zone-centre soft mode ( P6/mcc to Pbar{1} ) phase transition was predicted to occur at a pressure of about 14 GPa; the reduction of the frequency of the soft vibrational mode, as the pressure is increased, and the similar behaviour of the majority of the low-frequency modes, provided an explanation of the thermal behaviour of the crystal, which is consistent with the RUM model (Rigid Unit Model; Dove et al. in Miner Mag 59:629–639, 1995), where the negative contribution to thermal expansion is ascribed to a geometric effect connected to the tilting of rigid polyhedra in framework silicates. |
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