2009
DOI: 10.1029/2009gl039318
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Correction to “P‐V‐T relations of the MgSiO3 perovskite determined by in situ X‐ray diffraction using a large‐volume high‐pressure apparatus”

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Cited by 8 publications
(13 citation statements)
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“…Previous data recalculated by the new scale were successfully reduced to the present room temperature isotherm of MgSiO 3 within the typical uncertainty in the pressure determinations. Differences between reduced and original room temperature pressures are 0.5 GPa in Funamori et al [1996] and 0.3 GPa in Katsura et al [2009b]. This suggests that present P-V-T data sets of MgSiO 3 perovskite and MgO simultaneously measured up to 110 GPa and 2500 K is mutually consistent with the previous data sets.…”
Section: Comparison With Previous Eos Modelssupporting
confidence: 85%
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“…Previous data recalculated by the new scale were successfully reduced to the present room temperature isotherm of MgSiO 3 within the typical uncertainty in the pressure determinations. Differences between reduced and original room temperature pressures are 0.5 GPa in Funamori et al [1996] and 0.3 GPa in Katsura et al [2009b]. This suggests that present P-V-T data sets of MgSiO 3 perovskite and MgO simultaneously measured up to 110 GPa and 2500 K is mutually consistent with the previous data sets.…”
Section: Comparison With Previous Eos Modelssupporting
confidence: 85%
“…Due to the mistake, the reported parameters do not reproduce their original data. However, the original data of Katsura et al [2009b] does give EOS parameters consistent with those of this study, if the correct analysis is carried out.…”
Section: Comparison With Previous Eos Modelssupporting
confidence: 70%
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“…For mantle silicates, such as Mg 2 SiO 4 polymorphs and MgSiO 3 -perovskite these values vary in the range of (∂K T /∂T) P = -0.02-0.03 GPa/K and aK T = 3-7 × 10 −3 GPa/K (e.g., Ref. 46). For naphthalene it was calculated that (∂K T /∂T) P = -0.003 GPa/K and aK T = 6 × 10 −4 GPa/K.…”
Section: Resultsmentioning
confidence: 99%