Abstract
Crystallization pressure of salt in porous materials is one of the mechanisms that may induce serious damage, for example, weathering of buildings and monuments of cultural heritage. Since this pressure also causes the solubility of the salt inside a porous material to differ from the bulk solubility, it can be assessed experimentally by measuring the solubility inside the pores. We show that this is possible by NMR, and study and in a series of model porous materials. Using the solubility data the crystal-liquid surface energies are estimated as for and for . For pore sizes below about 30 nm, the resulting pressure exceeds the tensile strength of typical building materials (3 MPa). No pressure is induced by the metastable , which suggests for this crystal a value of close to zero.
- Received 27 September 2004
DOI:https://doi.org/10.1103/PhysRevLett.94.075503
©2005 American Physical Society