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chondrodite

2Mg2SiO4·Mg(OH,F)2 (microprobe: Mg3.86Fe0.14(SiO4)·Mg0.00Ti0.05F1.38(OH)0.52O0.1, H assumed from stoichiometry)

third-order Birch-Murnaghan · Original · 1994

V₀
110.88
cm³/mol
Molar
K₀
136.200
GPa
Isothermal
K′
3.700
dimensionless

Volume (V₀)

Value Unit Basis Z
110.88 cm³/mol Molar

Reported value and unit are preserved as extracted. Z (formula units per cell) is not stored yet, so molar ↔ ų/f.u. conversion is not applied automatically.

Composition

OxideMolar
MgO3.86
FeO0.14
TiO20.05
SiO21
H2O0.26

Formula: (O2H2F2)

Conditions & method

Tref
Pref
Structure
other / unspecified
Method
experiment (XRD / DAC / multianvil compression)
static compression, x-ray diffraction in diamond anvil cell to 42.3 GPa, methanol:ethanol:water medium, ruby fluorescence pressure scale
Sample
natural chondrodite, U.C. Berkeley collection #13056 (same sample as Williams, 1992)

Source

Paper
Static compression of chondrodite: Implications for water in the upper mantle
Authors
J. W. Faust; Elise Knittle
DOI
10.1029/94gl01592
Year
1994
Journal
Geophysical Research Letters
Origin
Original (measured or fitted in the source paper)

Evidence from the paper

The lattice parameters of this sample at ambient pressure are ... giving a V0 of 110.88 (+0.01) cm3/mol ... we fit our compression data to a third-order Eulerian finite-strain equation of state (i.e. Birch-Murnaghan equation: Birch, 1978) ... we did not constrain the value of K0T'. Our results yield a K0T for chondrodite of 136.2 (±8.8) GPa, with K0T' equal to 3.7 (±0.4).

Additional notes

rho0
3.13 (+0.01) g/cm3 (also quoted as 3.127 g/cm3)
lattice parameters
a = 4.795 (±0.112) Å, b = 10.314 (±0.056) Å, c = 7.881 (±0.075) Å, α = 109.059°
max pressure
42.3 GPa
lower mantle relevance
Chondrodite breaks down to MgSiO3 perovskite, MgO and a hydrated melt at lower mantle pressures and temperatures; no EOS parameters reported for the perovskite or MgO breakdown products
note
Hydrous phase framed as upper-mantle water carrier; included because paper explicitly discusses lower-mantle P/T behavior with EOS numbers