Why does Venus lack a magnetic field?

Computer Science

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

13

Scientific paper

Venus and Earth have similar radii and estimated bulk compositions, and both have an iron core that is at least partially liquid. However, despite these similarities, Venus lacks an appreciable dipolar magnetic field. Here I examine the hypothesis that this absence is due to Venus's also lacking plate tectonics for the past 0.5 b.y. The generation of a global magnetic field requires core convection, which in turn requires extraction of heat from the core into the overlying mantle. Plate tectonics cools Earth's mantle; on the basis of elastic thickness estimates and convection models, it is argued here that the mantle temperature on Venus is currently increasing. This heating will reduce the heat flux out of the core to zero over ˜1 b.y., halting core convection and magnetic field generation. If plate tectonics was operating on Venus prior to ca. 0.5 Ga, a magnetic field may also have existed. On Earth, the geodynamo may be a consequence of plate tectonics; this connection between near-surface processes and core magnetism may also be relevant to the generation of magnetic fields on Mars, Mercury, and Ganymede.

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

Why does Venus lack a magnetic field? 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 Why does Venus lack a magnetic field?, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Why does Venus lack a magnetic field? will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-740605

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