Peak scaling method to measure temperatures in the laser-heated diamond anvil cell and application to the thermal conductivity of MgO-Reference-Cited by-同舟云学术

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Peak scaling method to measure temperatures in the laser-heated diamond anvil cell and application to the thermal conductivity of MgO

Published:2014-11 Issue:11 Volume:119 Page:8154-8170
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Rainey E. S. G.¹,Kavner A.¹

Affiliation:

1. Department of Earth, Planetary, and Space Sciences; University of California; Los Angeles California USA

Funder

NSF

U.S. Department of Energy

NSF Cooperative Agreement

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014JB011267/fullpdf

Reference80 articles.

1. Variation of thermal conductivity and heat flux at the Earth's core mantle boundary;Ammann;Earth Planet. Sci. Lett.,2014

2. Evaluation of (Mg, Fe) partitioning between silicate perovskite and magnesiowustite up to 120 GPa and 2300 K;Andrault;J. Geophys. Res.,2001

3. Iron partitioning in Earth's mantle: Toward a deep lower mantle discontinuity;Badro;Science,2003

4. The effect of pressure and temperature on the absorption edges of three silver halides;Balchan;J. Phys. Chem. Solids,1961

5. Temperature gradients, wavelength-dependent emissivity, and accuracy of high and very-high temperatures measured in the laser-heated diamond anvil cell;Benedetti;High Pressure Res.,2004

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