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Shock-wave compression of silica gel as a model material for comets
by
Okuno, Masayuki
, Arai, Shoji
, Arasuna, Akane
, Okudera, Hiroki
, Mizukami, Tomoyuki
, Chen, Liliang
, Mashimo, Tsutomu
in
Comets
/ Crystallography and Scattering Methods
/ Dehydration
/ Earth and Environmental Science
/ Earth Sciences
/ Earth surface
/ Geochemistry
/ Hydrogen bonding
/ Longitudinal waves
/ Mineral Resources
/ Mineralogy
/ Original Paper
/ Shock waves
/ Silica
/ Silica gel
/ Silica glass
/ Silicon dioxide
/ Tetrahedra
/ Water chemistry
2016
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Shock-wave compression of silica gel as a model material for comets
by
Okuno, Masayuki
, Arai, Shoji
, Arasuna, Akane
, Okudera, Hiroki
, Mizukami, Tomoyuki
, Chen, Liliang
, Mashimo, Tsutomu
in
Comets
/ Crystallography and Scattering Methods
/ Dehydration
/ Earth and Environmental Science
/ Earth Sciences
/ Earth surface
/ Geochemistry
/ Hydrogen bonding
/ Longitudinal waves
/ Mineral Resources
/ Mineralogy
/ Original Paper
/ Shock waves
/ Silica
/ Silica gel
/ Silica glass
/ Silicon dioxide
/ Tetrahedra
/ Water chemistry
2016
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Shock-wave compression of silica gel as a model material for comets
by
Okuno, Masayuki
, Arai, Shoji
, Arasuna, Akane
, Okudera, Hiroki
, Mizukami, Tomoyuki
, Chen, Liliang
, Mashimo, Tsutomu
in
Comets
/ Crystallography and Scattering Methods
/ Dehydration
/ Earth and Environmental Science
/ Earth Sciences
/ Earth surface
/ Geochemistry
/ Hydrogen bonding
/ Longitudinal waves
/ Mineral Resources
/ Mineralogy
/ Original Paper
/ Shock waves
/ Silica
/ Silica gel
/ Silica glass
/ Silicon dioxide
/ Tetrahedra
/ Water chemistry
2016
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Shock-wave compression of silica gel as a model material for comets
Journal Article
Shock-wave compression of silica gel as a model material for comets
2016
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Overview
A shock-wave compression experiment using synthesized silica gel was investigated as a model for a comet impact event on the Earth’s surface. The sample shocked at 20.7 GPa showed considerable structural changes, a release of water molecules, and the dehydration of silanol (Si–OH) that led to the formation of a new Si–O–Si network structure containing larger rings (e.g., six-membered ring of SiO
4
tetrahedra). The high aftershock temperature at 20.7 GPa, which could be close to 800 °C, influenced the sample structure. However, some silanols, which were presumed to be the mutually hydrogen-bonded silanol group, remained at pressures >20.7 GPa. This type of silanol along with a small number of water molecules may remain even after shock compression at 30.9 GPa, although the intermediate structure of the sample recovered was similar to that of silica glass.
Publisher
Springer Berlin Heidelberg,Springer Nature B.V
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