1. Thermal convection of compressible fluid in the mantle of super-Earths
- Author
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Masanori Kameyama, Chihiro Tachinami, and Masaki Ogawa
- Subjects
Convection ,Materials science ,Convective heat transfer ,Thermal resistance ,Prandtl number ,Thermodynamics ,Astronomy and Astrophysics ,Physics::Geophysics ,Physics::Fluid Dynamics ,symbols.namesake ,Mantle convection ,Space and Planetary Science ,Thermal ,symbols ,Astrophysics::Earth and Planetary Astrophysics ,Adiabatic process ,Convection cell - Abstract
To understand how adiabatic compression influences mantle convection in super-Earths, we carried out linear stability analysis and non-linear numerical simulation of thermal convection for constant viscosity infinite Prandtl number fluid with both constant and pressure-dependent thermal expansivity. The mantle is basally heated and internal heating is not considered. In the case of constant thermal expansivity, thermal convection is totally inhibited in super-Earths of more than about 5 times the Earth’s mass owing to the strong effect of adiabatic compression, when the surface temperature is sufficiently high. Pressure-dependence of thermal expansivity is crucial for the onset of convection in massive super-Earths. Even when the thermal expansivity depends on pressure, our numerical simulation shows that the effect of adiabatic compression reduces the efficiency of convective heat transport by up to about 60%, depending on the planetary mass and the surface temperature. The reduction in the efficiency of convective heat transport makes cooling of the mantle more difficult in massive super-Earths, especially when the surface temperature is high. The surface temperature of a planet may affect its thermal history not only through its effects on the mechanical properties of convecting mantle materials, but also through its influence on adiabatic compression of convecting materials.
- Published
- 2014
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