Shock wave equation of state of muscovite

T. Sekine; A. M. Rubin; T. J. Ahrens

doi:10.1029/91jb02253

Shock wave equation of state of muscovite

T. Sekine, A. M. Rubin, T. J. Ahrens

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

24 Scopus citations

Abstract

Shock wave data to provide an equation of state of muscovite (initial density: 2.835 g/cm³) were determined up to a pressure of 141 GPa. The shock velocity (Us) versus particle velocity (Up) data are fit with a single linear relationship: Us=4.62(±0.12) +1.27(±0.04)Up (km/s). Third-order Birch-Murnaghan equation of state parameters (isentropic bulk modulus and isentropic pressure derivative of bulk modulus) are K_os=52±4GPa and K′_os=3.2±0.3. The pressure-temperature relation along the Hugoniot suggests that muscovite may dehydrate to KA1Si₃O₈(hollandite), corundum, and water, with a small volume change, above 80 GPa. Thermodynamic calculations of the equilibrium pressure for the dehydration yields a significantly lower value. -from Authors

Original language	English (US)
Pages (from-to)	19,675-19,680
Journal	Journal of Geophysical Research
Volume	96
Issue number	B12
DOIs	https://doi.org/10.1029/91jb02253
State	Published - 1991
Externally published	Yes

All Science Journal Classification (ASJC) codes

Geophysics
Forestry
Oceanography
Aquatic Science
Ecology
Water Science and Technology
Soil Science
Geochemistry and Petrology
Earth-Surface Processes
Atmospheric Science
Earth and Planetary Sciences (miscellaneous)
Space and Planetary Science
Palaeontology

Access to Document

10.1029/91jb02253

Cite this

@article{34c72d0a73bf4ec78ce9e2e42af35baa,

title = "Shock wave equation of state of muscovite",

abstract = "Shock wave data to provide an equation of state of muscovite (initial density: 2.835 g/cm3) were determined up to a pressure of 141 GPa. The shock velocity (Us) versus particle velocity (Up) data are fit with a single linear relationship: Us=4.62(±0.12) +1.27(±0.04)Up (km/s). Third-order Birch-Murnaghan equation of state parameters (isentropic bulk modulus and isentropic pressure derivative of bulk modulus) are Kos=52±4GPa and K′os=3.2±0.3. The pressure-temperature relation along the Hugoniot suggests that muscovite may dehydrate to KA1Si3O8(hollandite), corundum, and water, with a small volume change, above 80 GPa. Thermodynamic calculations of the equilibrium pressure for the dehydration yields a significantly lower value. -from Authors",

author = "T. Sekine and Rubin, {A. M.} and Ahrens, {T. J.}",

year = "1991",

doi = "10.1029/91jb02253",

language = "English (US)",

volume = "96",

pages = "19,675--19,680",

journal = "Journal of Geophysical Research",

issn = "0148-0227",

number = "B12",

}

TY - JOUR

T1 - Shock wave equation of state of muscovite

AU - Sekine, T.

AU - Rubin, A. M.

AU - Ahrens, T. J.

PY - 1991

Y1 - 1991

N2 - Shock wave data to provide an equation of state of muscovite (initial density: 2.835 g/cm3) were determined up to a pressure of 141 GPa. The shock velocity (Us) versus particle velocity (Up) data are fit with a single linear relationship: Us=4.62(±0.12) +1.27(±0.04)Up (km/s). Third-order Birch-Murnaghan equation of state parameters (isentropic bulk modulus and isentropic pressure derivative of bulk modulus) are Kos=52±4GPa and K′os=3.2±0.3. The pressure-temperature relation along the Hugoniot suggests that muscovite may dehydrate to KA1Si3O8(hollandite), corundum, and water, with a small volume change, above 80 GPa. Thermodynamic calculations of the equilibrium pressure for the dehydration yields a significantly lower value. -from Authors

AB - Shock wave data to provide an equation of state of muscovite (initial density: 2.835 g/cm3) were determined up to a pressure of 141 GPa. The shock velocity (Us) versus particle velocity (Up) data are fit with a single linear relationship: Us=4.62(±0.12) +1.27(±0.04)Up (km/s). Third-order Birch-Murnaghan equation of state parameters (isentropic bulk modulus and isentropic pressure derivative of bulk modulus) are Kos=52±4GPa and K′os=3.2±0.3. The pressure-temperature relation along the Hugoniot suggests that muscovite may dehydrate to KA1Si3O8(hollandite), corundum, and water, with a small volume change, above 80 GPa. Thermodynamic calculations of the equilibrium pressure for the dehydration yields a significantly lower value. -from Authors

UR - http://www.scopus.com/inward/record.url?scp=0026293341&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0026293341&partnerID=8YFLogxK

U2 - 10.1029/91jb02253

DO - 10.1029/91jb02253

M3 - Article

AN - SCOPUS:0026293341

SN - 0148-0227

VL - 96

SP - 19,675-19,680

JO - Journal of Geophysical Research

JF - Journal of Geophysical Research

IS - B12

ER -

Shock wave equation of state of muscovite

Abstract

All Science Journal Classification (ASJC) codes

Access to Document

Other files and links

Fingerprint

Cite this