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- W2156548036 abstract "A pressure-density model of the outer core is assumed, and the corresponding observed seismic velocity distribution is compared to that calculated from shock-wave theory, for assumed values of Hugoniot parameters and Grueneisen's ratio. A wide range of Hugoniot parameter values is compatible with the seismic properties of the outer core, if reasonable uncertainty is admitted in observed velocities and in estimates of Grueneisen's ratio. Estimated temperature in the outer core varies widely with assumed outer-core Hugoniot parameters and with model density; thus, temperature variation in the outer core is not restricted by seismic data. The wide range of possible Hugoniot parameter values for the outer core implies a wide range of possible compositions. Assuming in particular the composition Fe-Si and reasonable values of Grueneisen's ratio and model density, silicon concentration between 8% and 20% implies acceptable velocity and temperature distributions in the outer core. Alloys other than Fe-Si are possible in the outer core, but results similar to those for Fe-Si may be expected for them." @default.
- W2156548036 created "2016-06-24" @default.
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- W2156548036 date "1973-05-10" @default.
- W2156548036 modified "2023-09-26" @default.
- W2156548036 title "Composition and temperature of the outer core" @default.
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- W2156548036 doi "https://doi.org/10.1029/jb078i014p02586" @default.
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