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Volumn 14, Issue 10, 2007, Pages

Comment on "Paleoclassical transport in low-collisionality toroidal plasmas" [Phys. Plasmas 12, 092512 (2005)]

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EID: 36048981913     PISSN: 1070664X     EISSN: None     Source Type: Journal    
DOI: 10.1063/1.2787502     Document Type: Note
Times cited : (1)

References (8)
  • 3
    • 18544385331 scopus 로고    scopus 로고
    • a recent discussion of the existence and uniqueness of magnetic-field-line velocities, including a model time-dependent axisymmetric toroidal example, can be found in A. L. Wilmot-Smith, E. R. Priest, and G. Hornig, Geophys. Astrophys. Fluid Dyn. 99, 177 (2005);
    • a recent discussion of the existence and uniqueness of magnetic-field-line velocities, including a model time-dependent axisymmetric toroidal example, can be found in A. L. Wilmot-Smith, E. R. Priest, and G. Hornig, Geophys. Astrophys. Fluid Dyn. 99, 177 (2005);
  • 4
    • 33646585173 scopus 로고    scopus 로고
    • a brief review including select-but-key references is given in D. H. Nickeler and H.-J. Fahr, Sol. Phys. 235, 191 (2006).
    • a brief review including select-but-key references is given in D. H. Nickeler and H.-J. Fahr, Sol. Phys. 235, 191 (2006).
  • 6
    • 36048942312 scopus 로고    scopus 로고
    • x goes to zero?
    • x goes to zero?
  • 7
    • 36048956864 scopus 로고    scopus 로고
    • This assumes that the magnetic differential equation B·E, B·▽s can be solved for a single-valued ▽s (Ref. 3)-always the case for an electrostatic E
    • This assumes that the magnetic differential equation B·E=- B·▽s can be solved for a single-valued ▽s (Ref. 3)-always the case for an electrostatic E.
  • 8
    • 36048995608 scopus 로고    scopus 로고
    • Often, before transforming from x to a flux-surface coordinate, one first takes the derivative with respect to Ψt of the flux-diffusion equation (A2) or (A3, arriving at a diffusion-equation for q, To the author's knowledge, S. Jardin was the first to point out that solving the transport equation for q rather than for a magnetic flux eases the numerics in coupling to a Grad-Shafranov solver. It eliminates having to take a numerical derivative, One then transforms the independent variable of this diffusion-equation from x to a flux-surface-labelling coordinate other than q, of course, typically chosen as some function of normalized poloidal or toroidal flux for convenience, e.g, to reduce the numerical error in. computational applications, or, in the case of RFP's, to avoid a double-valued problem were Ψt to be used as the independent variable. Note that the choice of Ψt for the independe
    • x, which does not vanish in tokamaks (except in resistive steady state), fully into account.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.