1996
DOI: 10.1088/0029-5515/36/7/i02
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Simple models for the radial and poloidal E × B drifts in the scrape-off layer of a divertor tokamak: Effects on in/out asymmetries

Abstract: The influence of radial and poloidal E × B drifts in the scrape-off layer (SOL) of a divertor tokamak is considered. For B in the `forward' direction (the ∇B ion drift towards a lower X point, single null divertor configuration), the poloidal drift tends to increase the plasma pressure and the recycling rates at the outer target, lowering the temperature there - as compared with the inner target. When the radial drift dominates, these asymmetries are reversed. The radial drift is estimated to be more important… Show more

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Cited by 80 publications
(83 citation statements)
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“…This drift has been discussed in previous articles [10][11][12][13] to explain the in/out asymmetry of tokamak divertors. A brief derivation of the radial drift is given below.…”
Section: Derivation Of Radial Driftmentioning
confidence: 82%
“…This drift has been discussed in previous articles [10][11][12][13] to explain the in/out asymmetry of tokamak divertors. A brief derivation of the radial drift is given below.…”
Section: Derivation Of Radial Driftmentioning
confidence: 82%
“…the Pfirsch-Schlüter return current is a direct consequence of these effects. In the scrape-off layer parallel SOL flow can be produced due to the poloidal asymmetry of E r ×B t and ∇p i ×B t drifts [121,122,11].…”
Section: Sol Flow and Classical Drifts Effectsmentioning
confidence: 99%
“…This idea extends to the fluid description of fluid behaviour, although not with a 1:1 mapping between single-particle and fluid drift terms. In the scrape-off layer of Tokamaks, cross-field drift motion has been found to explain asymmetries in particle and power fluxes to inner and outer divertor strike points [8,[77][78][79] during experiments where the toroidal magnetic field has been reversed. During such experiments, it has also been noted that scrape-off layer flows are strongly affected [74,80,81] due to parallel flows induced by poloidal and radial drifts.…”
Section: Cross-field Driftsmentioning
confidence: 99%