Non-adiabatic motion of charged particles traversing a weak magnetic field: Pitch angle scattering
dc.contributor.author | Chapman, Sydney | en_US |
dc.contributor.author | Kendall, Peter C. | en_US |
dc.date.accessioned | 2006-09-08T21:13:33Z | |
dc.date.available | 2006-09-08T21:13:33Z | |
dc.date.issued | 1964-12 | en_US |
dc.identifier.citation | Chapman, Sydney; Kendall, Peter C.; (1964). "Non-adiabatic motion of charged particles traversing a weak magnetic field: Pitch angle scattering." Pure and Applied Geophysics PAGEOPH 59(1): 100-122. <http://hdl.handle.net/2027.42/43243> | en_US |
dc.identifier.issn | 0033-4553 | en_US |
dc.identifier.issn | 1420-9136 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/43243 | |
dc.description.abstract | A charged particle moves with velocity v in a constant non-uniform magnetic field H , spiralling with Larmor radius R . If R is small compared with the scale length L of the field, the magnetic moment associated with the Larmor motion of the particle is nearly constant. Consequently θ, the (‘pitch’) angle between v and H , varies as arcsin H 1/2 . Hence θ in such adiabatic motion is approximately the same at points on the path where H has the same value. But the magnetic moment and the pitch angle may differ materially at two such points, each in the region where R/L is small, if between them the particle traverses a region where R/L is not small. This region of non-adiabatic motion ‘scatters’ the pitch angles. | en_US |
dc.format.extent | 1283577 bytes | |
dc.format.extent | 3115 bytes | |
dc.format.mimetype | application/pdf | |
dc.format.mimetype | text/plain | |
dc.language.iso | en_US | |
dc.publisher | Birkhäuser-Verlag; Birkhäuser Verlag ; Springer Science+Business Media | en_US |
dc.subject.other | Geosciences | en_US |
dc.subject.other | Geophysics/Geodesy | en_US |
dc.title | Non-adiabatic motion of charged particles traversing a weak magnetic field: Pitch angle scattering | en_US |
dc.type | Article | en_US |
dc.subject.hlbsecondlevel | Atmospheric, Oceanic and Space Sciences | en_US |
dc.subject.hlbsecondlevel | Physics | en_US |
dc.subject.hlbtoplevel | Science | en_US |
dc.description.peerreviewed | Peer Reviewed | en_US |
dc.contributor.affiliationum | Geophysical Institute, College, Alaska; High Altitude Observatory, Boulder, Colorado; Institute of Science and Technology, University of Michigan, Ann Arbor, Michigan | en_US |
dc.contributor.affiliationother | High Altitude Observatory, Boulder, Colorado; Department of Applied Mathematics, University of Sheffield, Sheffield, UK | en_US |
dc.contributor.affiliationumcampus | Ann Arbor | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/43243/1/24_2004_Article_BF00880512.pdf | en_US |
dc.identifier.doi | http://dx.doi.org/10.1007/BF00880512 | en_US |
dc.identifier.source | Pure and Applied Geophysics PAGEOPH | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
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