Abstract
Electrostatic site-potentials can be calculated using the Madelung method in which the crystal structure is divided into parallel slices d hkl . Each slice is divided into a set of parallel identical ionic chains [ uvw ]. Site-potentials calculated for the same ( hkl ) but different [ uvw ] have the same values. However, site-potentials calculated for the same [ uvw ] but different ( hkl ) give inconsistent values. They become consistent when an empirical correction term is added. The corrected site-potentials agree with those calculated by the Ewald method. Examples are given for fluorite and rutile.

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