A scaling law for K'0 for silicates with constant mean atomic mass

Details A scaling law for K'0 for silicates with constant mean atomic mass A scaling law for K'0 for silicates with constant mean atomic mass

Sep 1973

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1973e%26psl..20...73a&link_type=abstract

Earth and Planetary Science Letters, Volume 20, Issue 1, p. 73-76.

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It is shown that Birch's formula for the isothermal pressure derivative of the isothermal bulk modulus, K', can be used to generate reasonable values of K'0 for a sequence of silicates with various ambient densities and constant mean atomic mass, m. The theory predicts values in fairly good agreement with experimental results, although there is a regrettable spread of experimental values of K'0 for each solid. This first-order approximation theory for scaling between K'0 and ϱ0 is analogous to the law of corresponding states which scales K0 and ϱ0.

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