Abstract
The observation of aerogels submitted to a pressure of mercury indicates that this porous material is compacted and not intruded by the mercury. Consequently, the classical Washburn equation cannot be applied. A relation is established between the pressure P of compaction and the size L of the largest pores. The size of pores is estimated by using the nitrogen adsorption-desorption isotherms analysis and SEM measurements. A relation is found in which P is proportional to L−4 The new relation is applied to mercury porosimetry. Finally, a mechanical model is proposed that reproduces successfully the behavior of aerogels under high pressure of mercury.
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Pirard, R., Blacher, S., Brouers, F. et al. Interpretation of mercury porosimetry applied to aerogels. Journal of Materials Research 10, 2114–2119 (1995). https://doi.org/10.1557/JMR.1995.2114
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DOI: https://doi.org/10.1557/JMR.1995.2114