Ultrafast X-ray Diffraction Study of a Shock-Compressed Iron Meteorite above 100 GPa

Natural kamacite samples (Fe<sub<92.5</sub<Ni<sub<7.5</sub<) from a fragment of the Gibeon meteorite were studied as a proxy material for terrestrial cores to examine phase transition kinetics under shock compression for a range of different pressures up to 140 GPa. In situ t...
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Autor*in:	Sabrina Tecklenburg [verfasserIn] Roberto Colina-Ruiz [verfasserIn] Sovanndara Hok [verfasserIn] Cynthia Bolme [verfasserIn] Eric Galtier [verfasserIn] Eduardo Granados [verfasserIn] Akel Hashim [verfasserIn] Hae Ja Lee [verfasserIn] Sébastien Merkel [verfasserIn] Benjamin Morrow [verfasserIn] Bob Nagler [verfasserIn] Kyle Ramos [verfasserIn] Dylan Rittman [verfasserIn] Richard Walroth [verfasserIn] Wendy L. Mao [verfasserIn] Arianna E. Gleason [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2021

Schlagwörter:	ultrafast X-ray diffraction laser shock compression iron meteorite

Übergeordnetes Werk:	In: Minerals - MDPI AG, 2012, 11(2021), 6, p 567
Übergeordnetes Werk:	volume:11 ; year:2021 ; number:6, p 567

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/min11060567

Katalog-ID:	DOAJ002862417

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callnumber-first	Q - Science
author	Sabrina Tecklenburg
spellingShingle	Sabrina Tecklenburg misc QE351-399.2 misc ultrafast X-ray diffraction misc laser shock compression misc iron meteorite misc Mineralogy Ultrafast X-ray Diffraction Study of a Shock-Compressed Iron Meteorite above 100 GPa
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topic_title	QE351-399.2 Ultrafast X-ray Diffraction Study of a Shock-Compressed Iron Meteorite above 100 GPa ultrafast X-ray diffraction laser shock compression iron meteorite
topic	misc QE351-399.2 misc ultrafast X-ray diffraction misc laser shock compression misc iron meteorite misc Mineralogy
topic_unstemmed	misc QE351-399.2 misc ultrafast X-ray diffraction misc laser shock compression misc iron meteorite misc Mineralogy
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title	Ultrafast X-ray Diffraction Study of a Shock-Compressed Iron Meteorite above 100 GPa
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title_sort	ultrafast x-ray diffraction study of a shock-compressed iron meteorite above 100 gpa
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title_auth	Ultrafast X-ray Diffraction Study of a Shock-Compressed Iron Meteorite above 100 GPa
abstract	Natural kamacite samples (Fe<sub<92.5</sub<Ni<sub<7.5</sub<) from a fragment of the Gibeon meteorite were studied as a proxy material for terrestrial cores to examine phase transition kinetics under shock compression for a range of different pressures up to 140 GPa. In situ time-resolved X-ray diffraction (XRD) data were collected of a body-centered cubic (bcc) kamacite section that transforms to the high-pressure hexagonal close-packed (hcp) phase with sub-nanosecond temporal resolution. The coarse-grained crystal of kamacite rapidly transformed to highly oriented crystallites of the hcp phase at maximum compression. The hcp phase persisted for as long as 9.5 ns following shock release. Comparing the <i<c/a</i< ratio with previous static and dynamic work on Fe and Fe-rich Fe-Ni alloys, it was found that some shots exhibit a larger than ideal <i<c/a</i< ratio, up to nearly 1.65. This work represents the first time-resolved laser shock compression structural study of a natural iron meteorite, relevant for understanding the dynamic material properties of metallic planetary bodies during impact events and Earth’s core elasticity.
abstractGer	Natural kamacite samples (Fe<sub<92.5</sub<Ni<sub<7.5</sub<) from a fragment of the Gibeon meteorite were studied as a proxy material for terrestrial cores to examine phase transition kinetics under shock compression for a range of different pressures up to 140 GPa. In situ time-resolved X-ray diffraction (XRD) data were collected of a body-centered cubic (bcc) kamacite section that transforms to the high-pressure hexagonal close-packed (hcp) phase with sub-nanosecond temporal resolution. The coarse-grained crystal of kamacite rapidly transformed to highly oriented crystallites of the hcp phase at maximum compression. The hcp phase persisted for as long as 9.5 ns following shock release. Comparing the <i<c/a</i< ratio with previous static and dynamic work on Fe and Fe-rich Fe-Ni alloys, it was found that some shots exhibit a larger than ideal <i<c/a</i< ratio, up to nearly 1.65. This work represents the first time-resolved laser shock compression structural study of a natural iron meteorite, relevant for understanding the dynamic material properties of metallic planetary bodies during impact events and Earth’s core elasticity.
abstract_unstemmed	Natural kamacite samples (Fe<sub<92.5</sub<Ni<sub<7.5</sub<) from a fragment of the Gibeon meteorite were studied as a proxy material for terrestrial cores to examine phase transition kinetics under shock compression for a range of different pressures up to 140 GPa. In situ time-resolved X-ray diffraction (XRD) data were collected of a body-centered cubic (bcc) kamacite section that transforms to the high-pressure hexagonal close-packed (hcp) phase with sub-nanosecond temporal resolution. The coarse-grained crystal of kamacite rapidly transformed to highly oriented crystallites of the hcp phase at maximum compression. The hcp phase persisted for as long as 9.5 ns following shock release. Comparing the <i<c/a</i< ratio with previous static and dynamic work on Fe and Fe-rich Fe-Ni alloys, it was found that some shots exhibit a larger than ideal <i<c/a</i< ratio, up to nearly 1.65. This work represents the first time-resolved laser shock compression structural study of a natural iron meteorite, relevant for understanding the dynamic material properties of metallic planetary bodies during impact events and Earth’s core elasticity.
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title_short	Ultrafast X-ray Diffraction Study of a Shock-Compressed Iron Meteorite above 100 GPa
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Ultrafast X-ray Diffraction Study of a Shock-Compressed Iron Meteorite above 100 GPa

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