High resolution Si-29, Na-23, and Cs-133 solid-state NMR spectroscopy was u
sed to study the interaction of sodium and cesium chloride salts with calci
um silicate hydrates (C-S-H), the main components of hydrated Portland ceme
nt. Spectra were collected at different levels of moisture and suggested th
at Cs+ and Na+ in contact with C-S-H behaved differently, mainly because of
their different hydration energy, which is smaller for Cs+ than for Na+. A
n interpretation of the results is given, using a conceptual model based on
an analogy between C-S-H and smectites, which present analogous structural
features. The results suggest that cesium and sodium have an affinity for
the C-S-H surface. In hydrated C-S-H, the cations may be located in a diffu
se ion swarm. In dry C-S-H, sodium cations would form outer-sphere complexe
s, i.e., they would be adsorbed with their hydration sphere, whereas cesium
cations would be adsorbed as inner-sphere complexes with two distinct envi
ronments, one without chloride and the other with chloride anions in their
coordination sphere. At low Ca/Si ratios, the mechanism involved for cation
ic adsorption is probably a compensation of the negative surface charge of
C-S-H.