Abstract
The intimate connection between the incompressibility k and the density ρ, as expressed in the relation (7.15), shows that evidence involving k is very pertinent to the determination of the Earth’s density variation. An illustration has already been provided in the use of information on φ, i.e. k/ρ, derived from seismic data in applying (10.7) to estimate density gradients in some regions of the Earth. In the present chapter, a quantity of additional evidence, theoretical and experimental, involving k is brought to bear.
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Bullen, K.E. (2002). Evidence on compressibility in the Earth. In: The Earth’s Density. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-5700-8_11
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DOI: https://doi.org/10.1007/978-94-009-5700-8_11
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