hydrous ringwoodite
hydrous ringwoodite (footnote b: water content of hydrous wadsleyite was 2.5 ± 0.3 wt %)
unknown · Cited · 2002
V₀
—
Unknown basis
K₀
155
GPa
Isothermal
K′
4.300
dimensionless
Volume (V₀)
| Value | Unit | Basis | Z |
|---|---|---|---|
| — | — | Unknown basis | — |
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
hydrous ringwoodite (footnote b: water content of hydrous wadsleyite was 2.5 ± 0.3 wt %)
Conditions & method
- Tref
- —
- Pref
- —
- Structure
- —
- Method
- literature compilation / cited valueunknown (literature value, Table 2)
- Sample
- —
Source
- Paper
- Equation of state of the hydrous phase δ‐AlOOH at room temperature up to 22.5 G…
- Authors
- C. B. Vanpeteghem; Eiji Ohtani; Tadashi Kondo
- DOI
- 10.1029/2001gl014224
- Year
- 2002
- Journal
- Geophysical Research Letters
- Origin
- Cited (quoted from earlier work)
Evidence from the paper
Table 2: Hydrous ringwoodite(b) 155 ± 2 GPa, K'0T = 4.3, Yusa and Inoue [1997]. Footnote b: the water content of hydrous wadsleyite was 2.5 ± 0.3 wt %.
Additional notes
reference
Yusa and Inoue [1997]
note
footnote b refers to 'hydrous wadsleyite' although the table row is labeled hydrous ringwoodite; copied verbatim