Thermal Conductivity of Rocks and Minerals

By C. Clauser, E. Huenges. 2013

939 citations recorded by the source corpus.

Subfields: Artificial Intelligence, Geophysics, Mechanics of Materials

View Paper: https://www.semanticscholar.org/paper/3b3fb9a1a796da99ef0434b1abf4adad5ca81d3d

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Artificial Intelligence

1. Taras V. Gerya

In Geophysics

1. D. May
2. T. Duretz
3. Taras V. Gerya
4. A. Maggi
5. M. An
6. S. Swenson
7. L. Perchuk
8. John M. Wahr

In Mechanics of Materials

1. Zong‐Liang Yang
2. Taras V. Gerya
3. D. May
4. X. Zeng

Citations in the corpus

• Numerical modelling of spontaneous slab breakoff and subsequent topographic response (2011, background): “Temperature dependent thermal conductivity k is documented in (Clauser and Huenges, 1995).”
• Temperature dependence of thermal diffusivity, specific heat capacity, and thermal conductivity for several types of rocks (2014, neutral): “83 for biotite [30], 2.”
• Thermal Properties of Rocks and Density of Fluids (2014, background): “…differently, at low and moderate temperatures (up to 573–773 K) the value of heat conductivity varies proportionally with the reciprocal of the temperature (Lubimova 1968b; Clauser and Huenges 1995, amongst others), but the actual relationships between these two parameters are more complicated.”
• Temperature, lithosphere‐asthenosphere boundary, and heat flux beneath the Antarctic Plate inferred from seismic velocities (2015, background): “[Clauser and Huenges, 1995;Whittington et al., 2009] and upper mantle (olivine, wadsleyite, and ringwoodite)”
• Three-dimensional thermomechanical modeling of oceanic spreading initiation and evolution (2013, neutral): “…is the temperature ( C) k is the thermal conductivity of dry rocks (W/m/K) [k = 0.73 + 1293/(T + 77) for the mantle and k = 1.18 + 474/(T + 77) for the crust (Clauser and Huenges, 1995)], k0 = 3 W/m/K is the reference thermal conductivity, Nu = 2–4 is the assumed Nusselt number for the…”
• Effective Thermal Conductivity Modeling of Sandstones: SVM Framework Analysis (2016, methodology): “For curve fitting of experimental ETC data of porous rocks, several types of functions have been employed by some researchers [37,38].”
• Parameterization improvements and functional and structural advances in Version 4 of the Community Land Model (2011, methodology): “For CLM4, the lake and wetland distributions revert back to those used in CLM3 (Cogley 1991), except that the threshold area fraction that is used to determine whether or not a lake, wetland, or glacier surface type is represented in a particular grid cell is reduced from 5% to 1%.”