Please use this identifier to cite or link to this item: https://hdl.handle.net/10216/529
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dc.creatorF. Salzedas
dc.creatorS. Hokin
dc.creatorF. C. Schüller
dc.creatorA. A. M. Oomens
dc.date.accessioned2019-02-07T04:11:25Z-
dc.date.available2019-02-07T04:11:25Z-
dc.date.issued2002
dc.identifier.othersigarra:56311
dc.identifier.urihttps://repositorio-aberto.up.pt/handle/10216/529-
dc.description.abstractMeasurements of the electron temperature, Te, and density, ne, during the energy quench of a major disruption showed that the onset of Te erosion in the neighborhood of the m/n = 2/1 O point at the low field side (LFS) accelerates the well-known m/n = 1/1 erosion of the core temperature. During this phase Te(r) is only partially flat in the region between the q = 2 and the q = 1 surfaces and ne(r) decreases in the core and increases inside the m/n = 2/1 island. Immediately after the flattening of Te(r) a large peak in Te and to a lesser extent in ne has been observed. This peak is radially localized at the q = 2 radius at the LFS, is very short lived and is poloidally asymmetric. Te profiles measured by the heterodyne radiometer and the Thomson scattering agree very well up to the time Te(r) flattens but afterwards can be a factor of two different.
dc.language.isoeng
dc.rightsopenAccess
dc.rights.urihttps://creativecommons.org/licenses/by-nc/4.0/
dc.titleHigh resolution temperature and density profiles during the energy quench of density limit disruptions in Rijnhuizen tokamak project
dc.typeArtigo em Revista Científica Internacional
dc.contributor.uportoFaculdade de Engenharia
dc.identifier.doi10.1063/1.1489675
Appears in Collections:FEUP - Artigo em Revista Científica Internacional

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