dc.creator | CLEMENTE, RA | |
dc.creator | STEINHAUER, LC | |
dc.date | 1994 | |
dc.date | AUG | |
dc.date | 2014-12-16T11:36:17Z | |
dc.date | 2015-11-26T17:24:06Z | |
dc.date | 2014-12-16T11:36:17Z | |
dc.date | 2015-11-26T17:24:06Z | |
dc.date.accessioned | 2018-03-29T00:11:23Z | |
dc.date.available | 2018-03-29T00:11:23Z | |
dc.identifier | Journal Of The Physical Society Of Japan. Physical Soc Japan, v. 63, n. 8, n. 3003, n. 3007, 1994. | |
dc.identifier | 0031-9015 | |
dc.identifier | WOS:A1994PD49300026 | |
dc.identifier | 10.1143/JPSJ.63.3003 | |
dc.identifier | http://www.repositorio.unicamp.br/jspui/handle/REPOSIP/70997 | |
dc.identifier | http://www.repositorio.unicamp.br/handle/REPOSIP/70997 | |
dc.identifier | http://repositorio.unicamp.br/jspui/handle/REPOSIP/70997 | |
dc.identifier.uri | http://repositorioslatinoamericanos.uchile.cl/handle/2250/1283993 | |
dc.description | A fluid model allowing for plasma resistivity and anisotropic temperatures, for describing edge-layer and jets in field-reversed configurations, is presented. Jet velocity can be predicted in terms of drops in parallel and perpendicular temperatures, from the separatrix to the throat, and the edge-layer broadness should depend on plasma conductivity. Comparison with experimental measurements suggests that the conductivity should be an order of magnitude lower than classical. | |
dc.description | 63 | |
dc.description | 8 | |
dc.description | 3003 | |
dc.description | 3007 | |
dc.language | en | |
dc.publisher | Physical Soc Japan | |
dc.publisher | Tokyo | |
dc.publisher | Japão | |
dc.relation | Journal Of The Physical Society Of Japan | |
dc.relation | J. Phys. Soc. Jpn. | |
dc.rights | fechado | |
dc.source | Web of Science | |
dc.subject | FRC | |
dc.subject | TRANSPORT | |
dc.subject | EDGE-LAYER | |
dc.subject | JETS | |
dc.subject | ANISOTROPIC | |
dc.subject | Classical Transport | |
dc.title | RESISTIVE ANISOTROPIC FLOW FOR EDGE-LAYER AND JETS IN FIELD-REVERSED CONFIGURATIONS | |
dc.type | Artículos de revistas | |