Research on Point Discharge in the Atmosphere Both from Natural and Artificial Points

摘要

The comparison of measurements of potential gradient at pointe upwind and downwind of the must should show effects depending on the ions relessed in the point-dtschsrge proeess This has been studies theoretically and observationally, the results to date show that the difference peiwean the porential gradients is less, by surtor of about 2, than that predieted for s linear stread of ionn the divergence may be one to ionic diffusion. But is would appear that published emmsonts any aot able to accodnt for the reaults.