Modeling of Shock-Wave Loading of Magnesium Silicates on the Example of Forsterite

Standard

Modeling of Shock-Wave Loading of Magnesium Silicates on the Example of Forsterite. / Maevskii, K. K.

In: Technical Physics, Vol. 69, No. 2, 02.2024, p. 320-326.

Research output: Contribution to journal › Article › peer-review

BibTeX

@article{ffbb2f62d8b04e00b01c6f27e950bf8b,

title = "Modeling of Shock-Wave Loading of Magnesium Silicates on the Example of Forsterite",

abstract = "The results of modeling the shock-wave loading of Mg2SiO4 forsterite, which in this case is considered as a mixture of SiO2 quartz and MgO periclase, are presented. The model is based on the assumption that the components of the mixture under shock-wave loading are in thermodynamic equilibrium. The model allows us to reliably describe the phase transition region. The components of the investigated material are considered as a mixture of low and high pressure phases. Polymorphic phase transitions of quartz and periclase are taken into account in the calculation of forsterite in pressure range from 1 to 1000 GPa. The results are verified by experimental data obtained in dynamic experiments.",

keywords = "equation of state, forsterite, magnesium silicates, sho ck adiabat, thermo dynamic equality",

author = "Maevskii, {K. K.}",

note = "This study was supported by the Budget Project III.22.3.1.",

year = "2024",

month = feb,

doi = "10.1134/S1063784224010262",

language = "English",

volume = "69",

pages = "320--326",

journal = "Technical Physics",

issn = "1063-7842",

publisher = "PLEIADES PUBLISHING INC",

number = "2",

}

RIS

TY - JOUR

T1 - Modeling of Shock-Wave Loading of Magnesium Silicates on the Example of Forsterite

AU - Maevskii, K. K.

N1 - This study was supported by the Budget Project III.22.3.1.

PY - 2024/2

Y1 - 2024/2

N2 - The results of modeling the shock-wave loading of Mg2SiO4 forsterite, which in this case is considered as a mixture of SiO2 quartz and MgO periclase, are presented. The model is based on the assumption that the components of the mixture under shock-wave loading are in thermodynamic equilibrium. The model allows us to reliably describe the phase transition region. The components of the investigated material are considered as a mixture of low and high pressure phases. Polymorphic phase transitions of quartz and periclase are taken into account in the calculation of forsterite in pressure range from 1 to 1000 GPa. The results are verified by experimental data obtained in dynamic experiments.

AB - The results of modeling the shock-wave loading of Mg2SiO4 forsterite, which in this case is considered as a mixture of SiO2 quartz and MgO periclase, are presented. The model is based on the assumption that the components of the mixture under shock-wave loading are in thermodynamic equilibrium. The model allows us to reliably describe the phase transition region. The components of the investigated material are considered as a mixture of low and high pressure phases. Polymorphic phase transitions of quartz and periclase are taken into account in the calculation of forsterite in pressure range from 1 to 1000 GPa. The results are verified by experimental data obtained in dynamic experiments.

KW - equation of state

KW - forsterite

KW - magnesium silicates

KW - sho ck adiabat

KW - thermo dynamic equality

UR - https://www.scopus.com/record/display.uri?eid=2-s2.0-85202930964&origin=inward&txGid=73c8b4747995235e6f79b58b62c71f1d

UR - https://elibrary.ru/item.asp?id=69095179

UR - https://www.mendeley.com/catalogue/690395e4-01fa-3adb-9e51-5784397d9bab/

U2 - 10.1134/S1063784224010262

DO - 10.1134/S1063784224010262

M3 - Article

VL - 69

SP - 320

EP - 326

JO - Technical Physics

JF - Technical Physics

SN - 1063-7842

IS - 2

ER -

ID: 61157572