Abstract

A numerical simulation of silica aerogels is performed using diffusion-limited cluster-cluster aggregation of spheres inside a cubic box (with periodic boundary conditions). The volume fraction cc is taken to be sufficiently large to get a gel structure at the end of the process. In the case of monodisperse spheres, the wavevector dependent scattered intensity I(q)I(q) is calculated from the product of the form factor P(q)P(q) of a sphere by the structure factor S(q)S(q), which is related to the Fourier transform of g(r)1g(r)-1, where g(r)g(r) is the pair correlation function between sphere centers. The structure factor S(q)S(q) exhibits large-qq damped oscillations characteristics of the short range (intra-aggregate) correlations between spheres. These oscillations influence the I(q)I(q) curve in the qq-region between the fractal regime and the Porod regime and quantitative comparisons are made with experiments on colloidal aerogels. Moreover, at small-qq values, S(q)S(q) goes through a maximum characteristic of large range (inter-aggregate) correlations. Quantitative fits of the maximum in the experimental I(q)I(q) curves of base-catalyzed aerogel are presented. In the case of polydisperse spheres, I(q)I(q) is calculated directly from a single aggregate simulation. It is shown that increasing polydispersity shifts the location of the cross-over between the fractal and Porod regimes towards low qq-value.Comment: RevTex, 9 pages + 11 postscript figures, compressed using "uufiles". Proceeding of the 4th International Simposium on Aerogels (To appear in J. of Non-Cryst. Solids

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