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Stability of beta-iron: A new synchrotron X-ray study of heated iron at high pressure
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences. Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences, Solid Earth Geology.
1998 (English)In: EUROPEAN JOURNAL OF MINERALOGY, ISSN 0935-1221, Vol. 10, no 1, p. 43-47Article in journal (Refereed) Published
Abstract [en]

We have conducted a new study on the stability of the beta-iron phase at high pressure and temperature. With the X-ray study of the electrically heated iron wire at pressures between 35 and 68 GPa, we are able to demonstrate the reversibility of transform
Place, publisher, year, edition, pages
1998. Vol. 10, no 1, p. 43-47
Keywords [en]
iron; diamond-anvil cell; phase transition; inner core; HIGH-TEMPERATURE; EARTHS CORE; PHASE
Identifiers
URN: urn:nbn:se:uu:diva-27833OAI: oai:DiVA.org:uu-27833DiVA, id: diva2:55729
Note
Addresses: Dubrovinsky LS, Univ Uppsala, Inst Earth Sci, S-75236 Uppsala, Sweden. Univ Uppsala, Inst Earth Sci, S-75236 Uppsala, Sweden.Available from: 2006-12-01 Created: 2006-12-01 Last updated: 2011-01-14

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Lazor, P

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