Deformation of Earth's inner core by electromagnetic forces

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

8

Geomagnetism And Paleomagnetism: Dynamo Theories, Seismology: Core And Mantle, Tectonophysics: Core Processes, Tectonophysics: Earth'S Interior-Composition And State

Scientific paper

A recent study of Karato (1999) suggests that deformation induced in the inner core by electromagnetic (Lorentz) forces may account for the development of seismic anisotropy. The viability of this proposal depends on whether Lorentz forces can sustain persistent flow within the inner core. We explore this question by establishing the conditions for static equilibrium when Lorentz forces are present. We find that the requirements for thermodynamic and hydrostatic equilibrium are incompatible at the surface of the inner core. However, the resulting deformation redistributes mass in the interior so as to minimize steady flow. Numerical calculations show that the flow becomes vanishingly weak and is confined to the top of the inner core. Strains in the interior are small and the alignment of crystals is insufficient to explain the anisotropy inferred from seismological observations.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Deformation of Earth's inner core by electromagnetic forces does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Deformation of Earth's inner core by electromagnetic forces, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Deformation of Earth's inner core by electromagnetic forces will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1043553

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.