Calcium K-edge (4038 eV) X-ray absorption spectroscopy (XAS) of wet an
d dry Ca-silicate hydrate (C-S-H) samples and model compounds (calcite
, xonotlite, 11 Angstrom tobermorite, and 14 Angstrom tobermorite) sho
w that the local structure of single-phase C-S-H as viewed from the Ca
-positions is similar to that of tobermorite. The only major effect of
wetting and drying observed by Ca-XAS is an increase in the average C
a-Ca distance, probably due to changes in interlayer spacing. The Ca-X
AS spectrum of a fully hydrated beta-C2S sample, containing C-S-H and
portlandite, is significantly different due to the presence of the por
tlandite. Ca-XAS provides unique information about the structure of C-
S-H and is likely to be a useful tool for investigating the structures
of a wide range of phases of importance to cement science.