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- Adams–Williamson_equation abstract "The Adams–Williamson equation, named after L. H. Adams and E. D. Williamson, is a relation between the velocities of seismic waves and the density of the Earth's interior. Given the average density of rocks at the Earth's surface and profiles of the P-wave and S-wave speeds as function of depth, it can predict how density increases with depth. It assumes that the compression is adiabatic and that the Earth is spherically symmetric, homogeneous, and in hydrostatic equilibrium. It can also be applied to spherical shells with that property. It is an important part of models of the Earth's interior such as the Preliminary reference Earth model (PREM).".
- Adams–Williamson_equation wikiPageID "28974704".
- Adams–Williamson_equation wikiPageRevisionID "603917185".
- Adams–Williamson_equation subject Category:Geophysics.
- Adams–Williamson_equation subject Category:Ordinary_differential_equations.
- Adams–Williamson_equation subject Category:Structure_of_the_Earth.
- Adams–Williamson_equation comment "The Adams–Williamson equation, named after L. H. Adams and E. D. Williamson, is a relation between the velocities of seismic waves and the density of the Earth's interior. Given the average density of rocks at the Earth's surface and profiles of the P-wave and S-wave speeds as function of depth, it can predict how density increases with depth. It assumes that the compression is adiabatic and that the Earth is spherically symmetric, homogeneous, and in hydrostatic equilibrium.".
- Adams–Williamson_equation label "Adams–Williamson equation".
- Adams–Williamson_equation sameAs Adams%E2%80%93Williamson_equation.
- Adams–Williamson_equation sameAs Q4680537.
- Adams–Williamson_equation sameAs Q4680537.
- Adams–Williamson_equation wasDerivedFrom Adams–Williamson_equation?oldid=603917185.