RADIOGRAPHIC STUDY ON THE VISCOSITY OF THE FE-FES MELTS AT THE PRESSURE OF 5 TO 7 GPA

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dc.contributor.author Urakawa S.
dc.contributor.author Terasaki H.
dc.contributor.author Kato T.
dc.contributor.author Funakoshi K.
dc.contributor.author Suzuki A.
dc.date.accessioned 2021-04-05T02:40:13Z
dc.date.available 2021-04-05T02:40:13Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=13987696
dc.identifier.citation American Mineralogist, 2001, 86, 4, 578-582
dc.identifier.issn 0003-004X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/27292
dc.description.abstract Stokes' viscometry combined with in situ X-ray radiographic observation, using the 6-8 type multi-anvil press and synchrotron radiation, has been applied to the viscosity measurement of the Fe-FeS melt up to pressures of 7 GPa. The viscosity is found to be about 2 × 10-2 Pa-s at 5 to 7 GPa and temperatures about 1350 K, in marked contrast to previous viscosity measurements, which showed high viscosity, 0.5 to 14 Pa-s, at 2 to 5 GPa (LeBlanc and Secco 1996). Our viscosity data, however, is consistent with all other evidence, which include I atm viscosity data, X-ray structure analysis, and ab initio simulations. Recent viscosity measurements (Dobson et al. 2000) also showed the viscosity of Fe-FeS melt to be about 10-2 Pa-s at 2.5 GPa. Thus, we are confident that the viscosity of the Fe- FeS melt is close to a typical value (10-2 Pa-s) of viscosity for liquid metal even at high pressures.
dc.title RADIOGRAPHIC STUDY ON THE VISCOSITY OF THE FE-FES MELTS AT THE PRESSURE OF 5 TO 7 GPA
dc.type Статья


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