Thermal Conduction of Materials in the Upper Mantle and the Transition Zone

• OSAKO Masahiro

  Department of Science and Engineering, National Museum of Nature and Science

• YONEDA Akira

  Institute for Study of the Earth's Interior, Okayama University

• ITO Eiji

  Institute for Study of the Earth's Interior, Okayama University

Bibliographic Information

Other Title

• 上部マントルおよび遷移層物質の熱伝導
• ジョウブ マントル オヨビ センイソウ ブッシツ ノ ネツ デンドウ

Abstract

Measurements of thermal conduction for materials in the Earth's upper mantle and the transition zone under high pressure have been developed by using a Kawai-type apparatus, with a one-dimensional plane pulse-heating method. This method is a predominant one for study in mantle materials under pressure because it requires comparatively small amount of sample and is applicable to materials with anisotropy in thermal conduction. Thermal conductivities and thermal diffusivities of olivine, garnet, pyroxenes, serpentine and talc were measured under high-pressure using this method.<br>

Journal

• The Review of High Pressure Science and Technology

  The Review of High Pressure Science and Technology 24 (2), 108-117, 2014

  The Japan Society of High Pressure Science and Technology

Keywords

• thermal diffusivity
• thermal conductivity
• upper mantle
• transition zone
• Kawai-type apparatus
• plane pulse-heating method

Details

• CRID: 1390001204382230784
• NII Article ID: 130004447677
• NII Book ID: AN10452913
• DOI: 10.4131/jshpreview.24.108
• ISSN: 13481940
• ISSN: 0917639X
• NDL BIB ID: 025601938
• Web Site: http://id.ndl.go.jp/bib/025601938
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I025601938
• Text Lang: ja
• Data Source:
  • JaLC
  • NDL
  • Crossref
  • CiNii Articles
  • KAKEN
• Abstract License Flag: Disallowed