Abstract
An idealized model for ion transport across an oscillating plasma sheath is analyzed to obtain insight into qualitative features of the ion energy distributions observed in low-pressure rf discharges. The sheath is characterized by a constant electric field over an extent that varies sinusoidally with time, and ions incident on it correspond to a monoenergetic flux independent of phase \ensuremath{\varphi} in the rf cycle. The dimensionless parameters \ensuremath{\alpha}=${\mathit{qV}}_{\mathit{s}}$/m${\mathrm{\ensuremath{\omega}}}^{2}$${\mathit{d}}^{2}$ and \ensuremath{\beta}=${\mathit{v}}_{0}$/\ensuremath{\omega}d (where d and ${\mathit{V}}_{\mathit{s}}$ are the mean sheath thickness and potential drop, \ensuremath{\omega} is the excitation frequency, and ${\mathit{v}}_{0}$ and q/m are the incoming ion speed and charge-to-mass ratio) govern the ion trajectories, which are found to divide into groups, delimited by two ``critical'' values of \ensuremath{\varphi}, that undergo N and N+1 encounters with the field. The first critical phase depends only weakly on \ensuremath{\beta}, whereas the second is sensitive to both \ensuremath{\alpha} and \ensuremath{\beta} and cycles continuously as these parameters diminish. Correspondingly, within the ``transition regime'' where \ensuremath{\alpha} and \ensuremath{\beta} are neither very small nor greater than (or comparable to) unity, the precise form of the incident-ion energy spectrum exhibits rapid variations, superposed on a systematic narrowing, as the frequency \ensuremath{\omega} is increased.
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