Equimolar catanionic monolayers were formed at the air-water interface by m
ixing double- or single-tailed cationic amphiphiles (with chain lengths var
ying from C-12 to C-18) with single-tailed anionic amphiphiles (from C-12 t
o C-16). The mixed systems investigated show strong synergistic behavior be
tween their components: the major part form solid or liquid condensed monol
ayers, with low isothermal compressibilities and high collapse surface pres
sures. The kinetics of monolayer relaxation, after stopping its compression
, was studied for the five most uncompressible systems using two methodolog
ies: (i) surface pressure relaxation, pi -t, at constant area A and (ii) ar
ea relaxation, A-t, at constant pi. The relaxation data could be fitted to
a sum of three exponentials. The two shorter lifetimes (of few minutes and
tens of minutes) were assigned, respectively, to short- and long-range mono
layer reorganization processes at the interface. The third, much longer lif
etime (of hundreds to thousands of minutes) was assigned to a monolayer des
orption into the subphase. The two relaxation methods (at constant A or pi)
gave equivalent reorganization lifetimes, within the experimental error. H
owever, different desorption lifetimes were obtained by one or the other pr
ocedure. The experimental pi -A, pi -t, and A-t isotherm data were intercon
nected by Euler's chain relation at a common point of the three isotherms w
here desorption can be ignored, {pi (0), A(0), t(0)}.