http://www.cnr.it/ontology/cnr/individuo/prodotto/ID236183
Recording non-local temperature rise in the RTP tokamak (Articolo in rivista)
- Type
- Label
- Recording non-local temperature rise in the RTP tokamak (Articolo in rivista) (literal)
- Anno
- 2000-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1088/0741-3335/42/10/310 (literal)
- Alternative label
G M D Hogeweij (1), P Mantica (2), G Gorini (2,3), J de Kloe (1), N J Lopes Cardozo (1) and the RTP team (1) (2000)
Recording non-local temperature rise in the RTP tokamak
in Plasma physics and controlled fusion (Online)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- G M D Hogeweij (1), P Mantica (2), G Gorini (2,3), J de Kloe (1), N J Lopes Cardozo (1) and the RTP team (1) (literal)
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- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
- http://iopscience.iop.org/0741-3335/42/10/310/ (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- (1) FOM Instituut voor Plasmafysica `Rijnhuizen', Associatie EURATOM-FOM, Trilateral Euregio Cluster, PO Box 1207, 3430 BE Nieuwegein, The Netherlands
(2) Istituto di Fisica del Plasma, Ass. Euratom-ENEA-CNR, Milano, Italy
(3) INFM and Dipartimento di Fisica `G Occhialini', Università degli Studi di Milano-Bicocca, Milano, Italy (literal)
- Titolo
- Recording non-local temperature rise in the RTP tokamak (literal)
- Abstract
- In the Rijnhuizen Tokamak Project (RTP) plasmas with electron cyclotron heating (ECH), a transient rise of the core T-e is observed when hydrogen pellets are injected tangentially to induce fast cooling of the peripheral region. The core T-e rise is a sharp function of the normalized power deposition radius (rho (dep)). The strongest effect (deltaT(e) up to 80%) is observed when rho (dep) is just inside the q = 1 surface, whereas only modest effects are seen with larger or smaller rho (dep). The rise is due to both a steepening of the T-e profile between the q = 1 and q = 2 surfaces, and a peaking inside rho (dep). (literal)
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