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- W2014586136 abstract "Abstract We have investigated the possibilities for thermochemical convective instability of a low viscous, dense D″-layer heated from below, in either the extended Boussinesq approximation (i.e. with dissipation) or the Boussinesq approximation only. We find, that the compositional excess density in the D″-layer, required for its stratification at the core–mantle boundary is greatly overestimated in the Boussinesq approximation ( Di =0, R ρ ≈0.8). In the extended Boussinesq approximation the stabilizing excess density is far less ( Di =0.3, R ρ =0.3). Therefore, in a dissipative mantle, a strongly stratified D″-density profile is unlikely, because it would stabilize the D″-layer and inhibit the development of large mantle plumes. A too low viscosity drop, greater than 10 2 , of the D″-layer would lead to stratification of the layer and small-scale convection taking place inside it." @default.
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- W2014586136 date "2004-08-01" @default.
- W2014586136 modified "2023-10-17" @default.
- W2014586136 title "Influences of dissipation and rheology on mantle plumes coming from the D″-layer" @default.
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- W2014586136 doi "https://doi.org/10.1016/j.pepi.2003.07.026" @default.
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