Conductivity equations, based on the mean spherical approximation (MSA), ha
ve recently been derived. We compare their performance with that of classic
al equations at the level of experimental uncertainty using conductivity da
ta for some typical electrolyte solutions. For symmetrical electrolytes, th
e picture is consistent showing a better performance for the classical equa
tions. The Lee and Wheaten equation also shows advantages at moderate conce
ntrations. For unsymmetrical electrolytes, the differences between MSA and
classical equations is larger. There is, however, an inherent inconsistency
with the equilibrium information, which cannot be resolved at present.