Show simple item record

Non-adiabatic motion of charged particles traversing a weak magnetic field: Pitch angle scattering

dc.contributor.authorChapman, Sydneyen_US
dc.contributor.authorKendall, Peter C.en_US
dc.date.accessioned2006-09-08T21:13:33Z
dc.date.available2006-09-08T21:13:33Z
dc.date.issued1964-12en_US
dc.identifier.citationChapman, 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.issn0033-4553en_US
dc.identifier.issn1420-9136en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/43243
dc.description.abstractA 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.extent1283577 bytes
dc.format.extent3115 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypetext/plain
dc.language.isoen_US
dc.publisherBirkhäuser-Verlag; Birkhäuser Verlag ; Springer Science+Business Mediaen_US
dc.subject.otherGeosciencesen_US
dc.subject.otherGeophysics/Geodesyen_US
dc.titleNon-adiabatic motion of charged particles traversing a weak magnetic field: Pitch angle scatteringen_US
dc.typeArticleen_US
dc.subject.hlbsecondlevelAtmospheric, Oceanic and Space Sciencesen_US
dc.subject.hlbsecondlevelPhysicsen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumGeophysical Institute, College, Alaska; High Altitude Observatory, Boulder, Colorado; Institute of Science and Technology, University of Michigan, Ann Arbor, Michiganen_US
dc.contributor.affiliationotherHigh Altitude Observatory, Boulder, Colorado; Department of Applied Mathematics, University of Sheffield, Sheffield, UKen_US
dc.contributor.affiliationumcampusAnn Arboren_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/43243/1/24_2004_Article_BF00880512.pdfen_US
dc.identifier.doihttp://dx.doi.org/10.1007/BF00880512en_US
dc.identifier.sourcePure and Applied Geophysics PAGEOPHen_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


Files in this item

Show simple item record

Remediation of Harmful Language

The University of Michigan Library aims to describe library materials in a way that respects the people and communities who create, use, and are represented in our collections. Report harmful or offensive language in catalog records, finding aids, or elsewhere in our collections anonymously through our metadata feedback form. More information at Remediation of Harmful Language.

Accessibility

If you are unable to use this file in its current format, please select the Contact Us link and we can modify it to make it more accessible to you.