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- W2095259315 abstract "IN a paper to be published elsewhere, I have derived the ormula: where η is a measure of departure from chemical homogeneity at depth z in the Earth (here treated as spherically symmetrical); k, p and g denote the adiabatic incompressibility, pressure and intensity of gravitational attraction, and Φ is a function of the P and S seismic velocities. The index η is equal to unity where the Earth is chemically homogeneous, in accordance with a simpler formula1 developed in 1949; η exceeds unity where the chemical composition is varying with the depth z. An important property of η is that it is equal to the ratio of the actual value of dρ/dz (where ρ denotes density) to the value dρ/dz would take if the composition were unvarying." @default.
- W2095259315 created "2016-06-24" @default.
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- W2095259315 date "1962-12-01" @default.
- W2095259315 modified "2023-09-27" @default.
- W2095259315 title "Earth's Central Density" @default.
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- W2095259315 doi "https://doi.org/10.1038/196973a0" @default.
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