Abstract
Dislocation charges in Ca2+ ‐doped KC1 single crystals were determined by measuring the potential difference developed between the side surfaces while a specimen was being compressed between tilted plates. The dislocation charge was found to be negative, and its magnitude increased with Ca2+ concentration (up to a critical resolved shear stress of 4–5MPa) as well as with temperature (between 82 K and room temperature). A sweep-up mechanism for the edge dislocations to collect K+ vacancies with thermally activated adsorption and desorption processes is proposed and found to be consistent with experimental observations.