2010
DOI: 10.1080/08957959.2010.494844
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In situviscometry of high-pressure melts in the Paris–Edinburgh cell: application to liquid FeS

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Cited by 23 publications
(17 citation statements)
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“…In contrast, later studies used an in situ X-ray radiography technique to monitor the fall of the probing spheres and reported that liquid Fe-S alloys have very low viscosities around 10 mPa s, about 3 orders of magnitude lower than those reported by LeBlanc and Secco (1996). However, the reported results from these previous in-situ studies are also scattered, covering a range of almost one order of magnitude: 2.4-23.7 mPa s for liquid Fe (Terasaki et al, 2002;Rutter et al, 2002), 3.6-17.9 mPa s for liquid FeS (Dobson et al, 2000;Perrillat et al, 2010), and 7.4-35.6 mPa s for the eutectic Fe-S liquid (Dobson et al, 2000;Terasaki et al, 2001;Urakawa et al, 2001). For example for liquid Fe, Terasaki et al (2002) reported an increase of viscosity with increasing pressure from 17.4 mPa s at 2.8 GPa and 1692°C to 23.7 mPa s at 5.4 GPa and 1820°C, and then a rapid decrease to about 6-9 mPa s at 6-7 GPa around 1900°C, respectively.…”
Section: Introductionmentioning
confidence: 58%
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“…In contrast, later studies used an in situ X-ray radiography technique to monitor the fall of the probing spheres and reported that liquid Fe-S alloys have very low viscosities around 10 mPa s, about 3 orders of magnitude lower than those reported by LeBlanc and Secco (1996). However, the reported results from these previous in-situ studies are also scattered, covering a range of almost one order of magnitude: 2.4-23.7 mPa s for liquid Fe (Terasaki et al, 2002;Rutter et al, 2002), 3.6-17.9 mPa s for liquid FeS (Dobson et al, 2000;Perrillat et al, 2010), and 7.4-35.6 mPa s for the eutectic Fe-S liquid (Dobson et al, 2000;Terasaki et al, 2001;Urakawa et al, 2001). For example for liquid Fe, Terasaki et al (2002) reported an increase of viscosity with increasing pressure from 17.4 mPa s at 2.8 GPa and 1692°C to 23.7 mPa s at 5.4 GPa and 1820°C, and then a rapid decrease to about 6-9 mPa s at 6-7 GPa around 1900°C, respectively.…”
Section: Introductionmentioning
confidence: 58%
“…Such low-speed imaging may be sufficient for studying viscous melts such as silicates or oxides, but it is insufficient to study less viscous liquids such as liquid Fe alloys. For example, some viscosity results were based on only 2-4 images of the falling balls (Dobson et al, 2000;Terasaki et al, 2001;Urakawa et al, 2001;Perrillat et al, 2010). Such limited imaging rates make it difficult to ensure that the falling sphere has reached terminal velocity and therefore result in large uncertainties in the calculated viscosity.…”
Section: Introductionmentioning
confidence: 99%
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“…Structure and physical properties of liquids have been much less studied than those of crystalline materials due to experimental difficulties. Some efforts have been made to investigate structure of liquids [e.g., Tsuji et al, 1989;Mezouar et al, 2002;Shen et al, 2004;Yamada et al, 2011], physical properties such as density [e.g., Katayama et al, 1998;Shen et al, 2002;Ohtani et al, 2005], viscosity [e.g., Kushiro et al, 1976;Kanzaki et al, 1987;Dobson et al, 2000;Terasaki et al, 2001;Perrillat et al, 2010], and elastic wave velocity [e.g., Krisch et al, 2002;Decremps et al, 2009;Nishida et al, 2013]. However, these results were often based on individual techniques, and the discussions were made by comparisons with results obtained by other researchers using in different apparatus using different techniques.…”
Section: Introductionmentioning
confidence: 99%
“…The low viscosity of the core (eg Poirier, 1988;de Wijs et al, 1998;Perrillat et al, 2010) makes convection currents very efficient at mixing all the extensive variables, and in particular entropy and composition. A good evidence of that efficiency comes from the observation of the secular variation of the magnetic field which implies a flow velocity of the order of 10 −4 m s −1 (eg.…”
Section: Radial Structure Of the Corementioning
confidence: 99%