A small-angle X-ray scattering experimental study of tricalcium silicate (C3S) porous gel has been performed with synchrotron radiation. The experimental scattering intensity data are in accordance with the prediction for a porous fractal model. It is concluded that the porous fractal model describes the real structure better than the classical model which assumes the existence of differentiated macro-, meso- and microporosity.
CITATION STYLE
Craievich, A. F. (1987). SAXS study of the porous fractal structure of tricalcium silicate dry gels. Journal of Applied Crystallography, 20(5), 327–329. https://doi.org/10.1107/S0021889887086539
Mendeley helps you to discover research relevant for your work.