Experimental study of thermal conductivity at high pressures: Implications for the deep Earth’s interior

Lattice thermal conductivity of ferropericlase and radiative thermal conductivity of iron bearing magnesium silicate perovskite (bridgmanite) – the major mineral of Earth’s lower mantle– have been measured at room temperature up to 30 and 46GPa, respectively, using time-domain thermoreflectance and...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Physics of the earth and planetary interiors 2015-10, Vol.247 (C), p.11-16
Hauptverfasser:	Goncharov, Alexander F., Lobanov, Sergey S., Tan, Xiaojing, Hohensee, Gregory T., Cahill, David G., Lin, Jung-Fu, Thomas, Sylvia-Monique, Okuchi, Takuo, Tomioka, Naotaka
Format:	Artikel
Sprache:	eng
Schlagworte:	Bridgmanite CONDENSED MATTER PHYSICS, SUPERCONDUCTIVITY AND SUPERFLUIDITY Deep Earth’s minerals Ferropericlase GEOSCIENCES High pressure Lattice thermal conductivity Lower mantle Optical properties Radiative conductivity Thermal conductivity
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!