A revised estimate of the conductivity of iron alloy at high pressure and implications for the core energy balance
By F. Stacey, D. Loper. 2007
140 citations recorded by the source corpus.
Subfields: Geophysics, Molecular Biology
View Paper: https://www.semanticscholar.org/paper/655d2389d239e370346255320b6fff6a886d550f
How researchers see this paper
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In Geophysics
- Stéphane Labrosse
- Julien Aubert
- Charles Poitou
- B. Buffett
- F. Nimmo
- Jun Korenaga
- U. Christensen
- Paul J. Tackley
In Molecular Biology
- Stéphane Labrosse
- Julien Aubert
- Charles Poitou
- F. Nimmo
- B. Buffett
- U. Christensen
- Alexandre Fournier
- T. Gastine
Citations in the corpus
- Modelling the palaeo-evolution of the geodynamo (2009, methodology): “Following Stacey & Loper (2007), Labrosse et al. (2007) and Lay et al. (2008), we adopt Qa = 6 TW for a central value and allow for an uncertainty range of 1 TW above and below this value.”
- Stratification of the top of the core due to chemical interactions with the mantle (2010, background): “A heat flow of 8 TW at the CMB corresponds to a temperature gradient of 1.9 K km − 1 for a thermal conductivity of 28 W m − 1 K − 1 [ Stacey and Loper , 2007].”