No.274 Geodynamics Seminar
"Numerical investigations of the effects of the spatial variations
in transport properties on the convective patterns in the mantle"
Arata Miyauchi (Ph.D. Student, Ehime University)
4:30 pm 〜, 15 October 2010
Meeting room "Glova", 4 floor, Integrated Research
Building
Abstract
We performed a linear stability analysis on the onset of thermal convection
of fluid in the presence of spatial variation of physical properties. The
viscosity of the fluid is exponentially dependent on temperature, while
thermal expansivity and thermal conductivity are linearly dependent on
pressure (or depth). The geometry, planar layer model, is employed. The top
and bottom boundary conditions are taken to be either free-slip or rigid
surface. We seek for critical values of Rayleigh number which characterizes
the onset of convection. Velocity field and temperature distribution are
also obtained as infinitesimal perturbations for given horizontal
wavelength. We examine the influence on convection patterns of the magnitude
in spatial variation in physical properties.
Our analysis successfully reproduced the transition in flow patterns into
the ‘stagnant lid’ regime where a thick and stagnant lid of cold fluid
develops at the top surface due to the very strong temperature dependence of
viscosity. These flow patterns are quite similar to the one obtained in
finite-amplitude convection. Moreover, we found that the presence of spatial
variation in thermal expansivity and thermal conductivity changes the
convective planform and moderately affects the onset of stagnant lid regime.
Increasing the degree of spatial variation of properties other than the
viscosity inhibits the development of cold layer on top surface.
In the presentation, the details of numerical results and future directions
will be discussed.
For inquiry:Taku Tsuchiya TEL:(089)927-8198
E-mail takut@sci.ehime-u.ac.jp
