Raman spectra were measured for aqueous solutions of alkali sulfates,
Li2SO4, Na2SO4, K2SO4, Rb2SO4 and Cs2SO4 at various concentrations and
al room temperature. The changes in the band parameters and are in th
e band profiles of the v(1)(SO42-) mode were studied as a function of
the salt concentration. The band maximum nu(max) shifts almost linearl
y with concentration for all the salts. The slope of the lines plotted
nu(max) vs. concentration decreases in the order of Li+ > Na+ > K+ >
Rb+ > Cs+, and the former two have positive slope, while the last two
have a negative one. For the case of K+ the line is almost horizontal.
The intercept of the lines converges to a single point of 980.8 +/- 0
.2 cm(-1). The width measured at the half height and the integrated ba
nd width given by beta = A/I(nu(max)), where A denotes the integrated
area of the band and I(nu(max)) the intensity at the band maximum; inc
reased with concentration for all the studied salts. Their behaviour i
s non linear and a polynomial fit on the data shown an intercept at ze
ro concentration of 6.2 +/- 0.1 cm(-1) for the width measured at the h
alf height and of 7.2 +/- 0.1 cm(-1) for the integrated band width. Th
e band profiles which have been measured by several methods found an a
symmetry in the high wavenumber side of the band for Li+ and Na+ while
for the other salts the profile remain symmetrical. The changes in th
e band parameters and band profiles observed for nu(1)(SO42-) mode in
the present work are interpreted in terms of two main factors (a) the
changes in the local field experienced by sulfate surrounded by the wa
ter-screened cations and (b) the perturbation arising from the differe
nt dynamic behaviour of hydration water molecules of the cations. In p
articular, these results are found to be consistent with the concepts
of positive and negative hydration proposed by Samoilov. (C) 1997 Else
vier Science B.V.