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Stability of the ion-temperature-gradient-driven mode with negative magnetic shear
Author(s) -
Masaki Uchida,
Siddhartha Sen,
A. Fukuyama,
D. R. McCarthy
Publication year - 2003
Publication title -
physics of plasmas
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.75
H-Index - 160
eISSN - 1089-7674
pISSN - 1070-664X
DOI - 10.1063/1.1616015
Subject(s) - physics , plasma , tokamak , shear (geology) , instability , perturbation (astronomy) , mechanics , ion , time derivative , sign (mathematics) , magnetohydrodynamics , atomic physics , temperature gradient , condensed matter physics , quantum electrodynamics , classical mechanics , quantum mechanics , mathematical analysis , petrology , mathematics , geology
A model for transition to the enhanced reverse shear or negative central shear mode triggered in tokamaks is proposed. This model takes into account the linear behavior of the ion temperature gradient (ITG) driven perturbation, considered nowadays as the dominant source of anomalous energy losses in the low confinement mode, in the presence of a radially varying parallel velocity. Analytic and numerical studies show that when the magnetic shear has the same sign as the second derivative of the parallel velocity with respect to the radial coordinate, the ITG mode may become more unstable. On the other hand, when the magnetic shear has the opposite sign to the second derivative of the parallel velocity, the linear ITG mode may be completely stabilized. This result is similar to our earlier works on parallel velocity shear instability [S. Sen et al., Phys. Plasmas 7, 1192 (2000); D. R. McCarthy et al., Phys. Plasmas 8, 3645 (2001)].

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