Phase Separation in glass melts with liquid-liquid immiscibility after rapid cooling under terrestrial conditions and at microgravity

dc.bibliographicCitation.firstPage	224
dc.bibliographicCitation.journalTitle	Glass Science and Technology	eng
dc.bibliographicCitation.lastPage	226
dc.bibliographicCitation.volume	70
dc.contributor.author	Reiß, Helmut
dc.date.accessioned	2024-01-08T07:53:02Z
dc.date.available	2024-01-08T07:53:02Z
dc.date.issued	1997
dc.description.abstract	Glass melts with a stable (liquid-liquid) miscibility gap tend to form two layers by a Sedimentation process. The heavier phase forms the lower layer, the other the upper layer, in which droplets of the heavier phase become deposited. Cooling of glass melts with stable miscibility gaps under microgravity conditions prevents the Sedimentation. The structure (texture) of glasses cooled under microgravity conditions is compared with that of glasses cooled on earth.	eng
dc.description.version	publishedVersion
dc.identifier.uri	https://oa.tib.eu/renate/handle/123456789/14223
dc.identifier.uri	https://doi.org/10.34657/13253
dc.language.iso	eng
dc.publisher	Offenbach : Verlag der Deutschen Glastechnischen Gesellschaft
dc.relation.issn	0946-7475
dc.rights.license	CC BY 3.0 DE
dc.rights.uri	https://creativecommons.org/licenses/by/3.0/de/
dc.subject.ddc	660
dc.title	Phase Separation in glass melts with liquid-liquid immiscibility after rapid cooling under terrestrial conditions and at microgravity	eng
dc.type	Article	eng
dc.type	Text	eng
tib.accessRights	openAccess

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