Abstract
Summary Results obtained by the laser interferometric and graphical integration techniques reported in Part I and further results at greater distances are compared with extant theories. Only an incomplete analysis has been made of the effects of variable mercury flow but it is obvious that this phenomenon can not account for discrepancies between experiment and modified Ilkovic equations. The effect of a drop emerging into a region of depleted electrolyte in the absence of maximum suppressors is shown to fit the Ilkovic equation modified for depletion. The depletion measured is close to that assumed in the corrected equation.
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