Heat conduction within an elastic earth

Details Heat conduction within an elastic earth Heat conduction within an elastic earth

Oct 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986em%26p...36..157l&link_type=abstract

Earth, Moon, and Planets (ISSN 0167-9295), vol. 36, Oct. 1986, p. 157-166.

Computer Science

Numerical Analysis

1

Conductive Heat Transfer, Earth Mantle, Elastic Bodies, Geotemperature, Nuclear Heat, Radioactive Decay, Actinide Series, Deformation, Numerical Analysis, Temperature Distribution

Scientific paper

The author uses theoretical results derived in a previous paper (Lanzano, 1986) to numerically evaluate the temperature profile and radial deformation within a spherical, elastic Earth due to heat generated by the decay of radiogenic elements. He considers only the uranium family and has assumed the diffusivity of the silicate mantle to be K = 8×10-3cm2s-1, the Poisson elastic ratio to be σ = 0.25 and the coefficient of thermal expansion to be α = 2×10-5(deg)-1. His series solutions when applied to the interiors of the Moon, Mercury, and Mars yield results in agreement with Kopal's (1963) evaluations.

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