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Inward diffusion of tokamak-trapped particles by slow magnetic pumping

A. Samain1972年被引用 4Nuclear FusionIF 3出版社

Particle diffusion in a Tokamak configuration under the influence of a very slow magnetic compression wave is studied. The plasma is assumed to be in regime I of Galeev and Sagdeev. The wave interacts irreversibly with trapped particles only and induces a diffusion of these particles. Inward diffusion for a given species takes place if the wave propagates around the major axis faster than the diamagnetic motion of the trapped particles of this species. By using two waves with proper phase velocities, one of which has a preferential coupling with electrons and the other with ions, ambipolar inward plasma diffusion may be achieved. In typical reactor conditions, it is possible to cancel out the neoclassical particle diffusion using magnetic perturbations less than one percent of the static field at frequencies in the kHz-range.

日本語訳

トカマク配位における粒子拡散が、非常に遅い磁気圧縮波の影響下で研究される。プラズマはガリーブとサグデーフのレジームIにあると仮定される。この波は捕捉粒子とのみ不可逆的に相互作用し、これらの粒子の拡散を誘起する。特定の粒子種に対する内向き拡散は、その粒子種の捕捉粒子の反磁性運動よりも速く、波が主軸の周りを伝播する場合に生じる。適切な位相速度を持つ2つの波を用いることにより、その一方が電子と優先的に結合し、他方がイオンと優先的に結合する場合、両極性の内向きプラズマ拡散が達成され得る。典型的な炉条件では、kHz範囲の周波数において、静磁場の1パーセント未満の磁気摂動を用いて、新古典粒子拡散を打ち消すことが可能である。

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