The characterization of diffusion tensor for mid-latitude ionospheric plasma

dc.contributor.authorSagir, Selcuk
dc.contributor.authorYesil, Ali
dc.contributor.authorSanac, Gulay
dc.contributor.authorUnal, Ibrahim
dc.date.accessioned2026-08-12T17:15:24Z
dc.date.issued2014
dc.departmentFırat Üniversitesi
dc.description.abstractIn this study, the relationship between diffusion and the electrical conductivity tensor is investigated by using the real geometry of the Earth's magnetic field in the Northern Hemisphere for mid-latitudes. This relationship is derived from equation. Only in the elements of the diagonal of the tensor is an equal relationship found between the electrical conductivity called the longitudinal conductivity and the diffusion coefficient. The diagonal elements are equal to each other and do not depend on the Earth's magnetic field; however, the other elements of the tensor strongly depend on the Earth's magnetic field and they have characteristic of Bohm diffusion became a semi-empirical model (D-B= (1/16)kT/eB) but they do not depend on the electrical conductivity or the classical diffusion coefficient.
dc.identifier.doi10.4401/ag-6469
dc.identifier.issn1593-5213
dc.identifier.issn2037-416X
dc.identifier.issue2
dc.identifier.orcid0000-0002-5698-0154
dc.identifier.scopus2-s2.0-84900421357
dc.identifier.scopusqualityQ2
dc.identifier.urihttps://doi.org/10.4401/ag-6469
dc.identifier.urihttps://hdl.handle.net/11508/52206
dc.identifier.volume57
dc.identifier.wosWOS:000335835200007
dc.identifier.wosqualityQ3
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherIst Nazionale Di Geofisica E Vulcanologia
dc.relation.ispartofAnnals of Geophysics
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_WoS_20260511
dc.titleThe characterization of diffusion tensor for mid-latitude ionospheric plasma
dc.typeArticle

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