z-logo
Premium
High pressure phase transformations in MgF 2 (rutile)
Author(s) -
Ming Lichung,
Manghnana Murli H.
Publication year - 1979
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl006i001p00013
Subject(s) - rutile , diamond anvil cell , phase diagram , materials science , phase (matter) , crystallite , diffraction , analytical chemistry (journal) , volume (thermodynamics) , x ray crystallography , high pressure , mineralogy , crystallography , thermodynamics , chemistry , optics , metallurgy , physics , organic chemistry , chromatography
Employing a diamond‐anvil pressure cell and a YAG laser as a heating source, phase relationships in polycrystalline MgF 2 (rutile) were investigated to ∼330 kbar at both room temperature (∼23°C), and high temperature (∼1300°C). In situ high pressure X‐ray diffraction data show that MgF 2 (I) of rutile structure transforms into MgF 2 (II) of a cubic structure at ∼300 kbar at room temperature, and at ∼190 kbar at high temperature (∼1300°C), resulting in a negative d P /d T slope for the univariant line between MgF 2 (I) and MgF 2 (II) in the P‐T phase diagram. The molar volume differences at room temperature between MgF 2 (I) and MgF 2 (II) at 190 kbar and 300 kbar are ∼8% and ∼5%, respectively.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom