@article{3632aa10590c4340b699c33a592d68d8,
title = "In situ measurement of interfacial tension of Fe-S and Fe-P liquids under high pressure using X-ray radiography and tomography techniques",
abstract = "Interfacial tension is one of the most important properties of the liquid iron alloy that controls the core formation process in the early history of the Earth and planets. In this study, we made high-pressure X-ray radiography and micro-tomography measurements to determine the interfacial tension between liquid iron alloys and silicate melt using the sessile drop method. The measured interfacial tension of liquid Fe-S decreased significantly (802-112 mN/m) with increasing sulphur content (0-40 at%) at 1.5 GPa. In contrast, the phosphorus content of Fe had an almost negligible effect on the interfacial tension of liquid iron. These tendencies in the effects of light elements are consistent with those measured at ambient pressure. Our results suggest that the effect of sulphur content on the interfacial tension of liquid Fe-S (690 mN/m reduction with the addition of 40 at% S) is large compared with the effect of temperature (∼273 mN/m reduction with an increase of 200 K). The three-dimensional structure of liquid Fe-S was obtained at ∼2 GPa and 1373-1873 K with a high-pressure tomography technique. The Fe-S droplet was quite homogeneous when evaluated in a slice of the three-dimensional image.",
keywords = "Core formation, High pressure, Interfacial tension, Tomography",
author = "H. Terasaki and S. Urakawa and K. Funakoshi and N. Nishiyama and Y. Wang and K. Nishida and T. Sakamaki and A. Suzuki and E. Ohtani",
note = "Funding Information: The authors acknowledge K. Tsuno, S. Ghosh, K. Litasov, S. Ozawa, C. Lesher, and S. Gaudio for fruitful discussions and their technical assistance. The authors also acknowledge to Y. Katayama for technical comments regarding the toroidal cell. This work was partly supported by the Bilateral Joint Projects/Seminars Program of the Ministry of Education, Culture, Science, Sport and Technology of the Japanese Government to S.U., by a Grant in Aid for Scientific Research (S) (no. 18104009) to E.O., and by the 21st Century Center of Excellence program {\textquoteleft}Advanced Science and Technology Center for the Dynamic Earth{\textquoteright}. The experiments at SPring-8 were performed under contract to SPring-8 (proposal numbers 2006A1400 and 2007A1096). The experiments at Advanced Photon Source (APS) were performed under contract to the APS (proposal numbers GUP-5651, GUP-6093, and GUP-6582). GeoSoilEnviroCARS is supported by the National Science Foundation-Earth Sciences (EAR-0622171) and the U.S. Department of Energy-Geosciences (DE-FG02-94ER14466). Use of the Advanced Photon Source was supported by the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences, under contract no. DE-AC02-06CH11357. Y.W. is grateful for NSF support (EAR-0001088) for the development of the high pressure tomography apparatus, and EAR-0711057 for work involved in this study.",
year = "2009",
month = may,
doi = "10.1016/j.pepi.2009.01.004",
language = "English",
volume = "174",
pages = "220--226",
journal = "Physics of the Earth and Planetary Interiors",
issn = "0031-9201",
publisher = "Elsevier",
number = "1-4",
}