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The gross features of previous computer results on stable accumulation and depletion layers are explained analytically. Further, the drift velocity of the accumulation plane in the singular limit, D=0, is obtained by a simple geometric construction based solely on the velocity-field characteristic. This result is related to the drift velocity of the finite accumulation layer, at the same outside velocity, for the D≠0 case via a stringent inequality. For the general case, D=D(F), a new integral equation is derived from the starting differential equations.
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Murray A. Lampert (1969) studied this question.
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