Direct demonstration of microwave demagnetization of a whole rock sample with minimal heating

Computer Science

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

4

Scientific paper

Microwave demagnetization has been employed in a number of palaeointensity determinations and has been shown to produce equivalent results to thermal methods, yet the degree of demagnetization caused by the magnetic component of the microwave field, rather than dielectric heating, has never been fully established. Here we present results that show unequivocally that a sample of basalt may be demagnetized by the microwave magnetic field with minimal heating. The fields within a resonant cavity are described quantitatively and the possibility of perturbation due to the sample is accounted for. This allows direct comparison of the demagnetizing effect of the electric and magnetic field components. While the magnetic field can demagnetize the sample it is shown that without careful control of the sample's shape and placement, the effects of the electric field become dominant.

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

Direct demonstration of microwave demagnetization of a whole rock sample with minimal heating 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 Direct demonstration of microwave demagnetization of a whole rock sample with minimal heating, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Direct demonstration of microwave demagnetization of a whole rock sample with minimal heating will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1314625

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