第232回ジオダイナミクスセミナー
Geodynamics Seminar
"Relaxation of MgSiO3 glass"
山田明寛(COE研究員, GRC)
主催 : 愛媛大学地球深部ダイナミクス研究センター
日時 : 2009年5月28日(金)※16:30〜
場所 : 愛媛大学総合研究棟T 4F 共通会議室(理学部構内)
要 旨
MgSiO3 is one of the most common rock-forming components in the Earth.
However, due to its refractory nature and fragility in the molten state,
direct investigation of melt properties at extreme pressures and temperatures
are exceedingly challenging. Alternatively, properties of the (supercooled)
liquid at high pressure can be investigated by relaxing the glass on heating
near the glass transition temperature (region), Tg. Volumetric and structural
changes in MgSiO3 glass under sub-Tg to super-Tg conditions between 2.0
and 8.5 GPa provide insights into structural relaxation for fragile liquids
under compression.
MgSiO3 glass was prepared by melting crystalline MgSiO3 at ~1873 K
and quenching the liquid in air. Glass cylinders are heat-treated at high
pressure in the Walker 6/8 multi anvil apparatus. Samples were compressed
to the desire pressure and heated to the annealing temperature where they
were held for 5 minutes. Pressure was released at >10 GPa/min immediately
following the quench. Densities of recovered samples were measured by the
Archimedes methods. Additionally, Raman and NMR spectroscopy were performed
to examine the structural change with density.
The general trend of the densification with temperature are similar for
each pressure and can be categorized as follows: (1) a low temperature
interval where density changes on compression are recovered within 0.7%
of the initial density, (2) an intermediate temperature interval where
permanent densification with temperature is greatest and (3) a high temperature
interval where the change in density with annealing temperature is significantly
reduced. Since the relaxation begins abruptly just below the Tg at the
pressure, the temperature at which the slope of densification changes suggests
a limiting temperature for Tg. This limit is found to decrease with increasing
pressure expanding the temperature interval of the glass transition. The
result of Raman and NMR spectroscopy, which show the structural change
of MgSiO3 glass with pressure and temperature will be also presented.
問い合わせ先:土屋 卓久 TEL (089)927-8198
E-mail takut@sci.ehime-u.ac.jp
