An empirical relationship between thermal conductivity and elastic wave velocities in sandstone

Details An empirical relationship between thermal conductivity and elastic wave velocities in sandstone An empirical relationship between thermal conductivity and elastic wave velocities in sandstone

Aug 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993georl..20.1679z&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 20, no. 16, p. 1679-1682.

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2

Elastic Waves, P Waves, S Waves, Sandstones, Thermal Conductivity, Correlation, Earth Crust, Earth Mantle, Geothermal Energy Extraction

Scientific paper

Measurements in three samples of very clean quartz sandstone in the porosity range 4-16 percent, under dry and 100 percent water-saturated conditions, show that P- and S-wave velocities are linearly correlated with thermal conductivity. The experimental results agree with the theoretical relation between seismic velocities (predicted by the Kuster and Toksoz model (1974)) and thermal conductivity (predicted by weighted geometric mean).

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