Crystal structure of iron at the center of the Earth

Shigehiko Tateno

Research output: Contribution to journalArticle

Abstract

The inner core, most remote part of our planet, is composed of solid iron. Because the relevant ultrahigh pressure and temperature conditions were only accessible by dynamical shock-wave compression experiments, the crystal structure of iron at the inner core has long been under debate. Our first static experiments show that the hexagonal close-packed (hcp) structure is a stable form of iron up to 377 GPa and 5700 K, corresponding to inner core conditions. The observed weak temperature-dependence of the c/a axial ratio suggests that hcp-Fe is elastically anisotropic at core temperatures. Preferred orientation of the hcp phase may cause inner core seismic anisotropy.

Original languageEnglish
Pages (from-to)91-97
Number of pages7
JournalReview of High Pressure Science and Technology/Koatsuryoku No Kagaku To Gijutsu
Volume21
Issue number2
DOIs
Publication statusPublished - 2011
Externally publishedYes

Fingerprint

Iron
Crystal structure
Earth (planet)
iron
crystal structure
Planets
Shock waves
Temperature
Compaction
Anisotropy
Experiments
shock waves
planets
temperature dependence
anisotropy
temperature
causes

Keywords

  • Core
  • Diamond-anvil cell
  • Iron

ASJC Scopus subject areas

  • Condensed Matter Physics
  • Materials Science(all)
  • Chemistry(all)

Cite this

Crystal structure of iron at the center of the Earth. / Tateno, Shigehiko.

In: Review of High Pressure Science and Technology/Koatsuryoku No Kagaku To Gijutsu, Vol. 21, No. 2, 2011, p. 91-97.

Research output: Contribution to journalArticle

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