globalchange  > 气候减缓与适应
DOI: 10.1002/2013GL058328
论文题名:
Equation of state for silicate melts: A comparison between static and shock compression
作者: Wakabayashi D.; Funamori N.; Sato T.; Sekine T.
刊名: Geophysical Research Letters
ISSN: 0094-10510
EISSN: 1944-10241
出版年: 2014
卷: 41, 期:1
起始页码: 50
结束页码: 54
语种: 英语
英文关键词: deep upper mantle condition ; equation of state ; phase-transition-like structural change ; shock compression ; silicate melt ; static compression
Scopus关键词: Deep upper mantle ; Equation of state ; phase-transition-like structural change ; Shock compressions ; Silicate melts ; Static compression ; Equations of state ; Semiconductor insulator boundaries ; Silicates ; Data compression ; compression ; data acquisition ; estimation method ; high pressure ; mantle ; phase transition ; pressure effect ; silicate
英文摘要: The density data of silicate melts reported by static and shock compression have been compared quantitatively at the pressure condition of the Earth's deep upper mantle. The equation of state based on the static compression data cannot explain the shock compression data, and the systematic differences between them have been revealed. The shock temperatures were estimated with different methods among papers, and the reported values differed considerably from one another. The shock temperatures estimated by assuming phase-transition-like structural changes in melts lie between the previous estimates. Many of them are well below the liquidus temperatures of each sample, suggesting that the sample state may have been altered during the shock compression. In addition, some of the shock compression data reanalyzed in the recent paper differ considerably from the original. These results suggest that silicate melts show phase-transition-like structural changes at high pressures, which are consistent with the static compression data. Key Points Discrepancies are found in silicate melt density by static and shock compression Reestimated temperatures of shock data are well below liquidus temperatures Silicate melts show phase-transition-like structural changes at high pressures ©2013. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84896735771&doi=10.1002%2f2013GL058328&partnerID=40&md5=84821a219fa793e5df8da31d5d9d6f64
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/7774
Appears in Collections:气候减缓与适应

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作者单位: Department of Earth and Planetary Science, University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-0033, Japan

Recommended Citation:
Wakabayashi D.,Funamori N.,Sato T.,et al. Equation of state for silicate melts: A comparison between static and shock compression[J]. Geophysical Research Letters,2014-01-01,41(1).
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