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Salt and ice crystallisation in porous sandstones

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Environmental Geology

Abstract

Salt and ice crystallisation in the pore spaces causes major physical damage to natural building stones. The damaging effect of these processes can be traced back to physically induced stress inside of the rock while crystallizing. The increasing scientific research done during the past century has shown that there are numerous parameters that have an influence on the weathering resulting from these processes. However, the working mechanisms of the stress development within the rock and its material dependency are still subject to discussion. This article gives an overview of salt and ice weathering. Additionally, laboratory results of various sandstones examined are presented. Salt crystallisation tests and freeze/thaw tests were done to obtain information about how crystallisation weathering depends on material characteristics such as pore space, water transportation, and mechanical features. Simultaneous measuring of the length alternating during the salt and ice crystallisation has revealed detailed information on the development of crystal in the pore spaces as well as the development of stress. These findings can help to understand the damaging mechanisms.

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Acknowledgments

We are grateful to Dirk Kirchner and Madlen Seidel for their help with the salt crystallisation tests. Thanks go to M Steiger for his comments. Our work was supported by the Deutsche Bundesstiftung Umwelt and the Deutsche Forschungsgemeinschaft (Si 438/17-1/2).

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  1. Geoscience Center University Goettingen, Goldschmidtstr. 3, 37077, Goettingen, Germany

    Joerg Ruedrich & Siegfried Siegesmund

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  1. Joerg Ruedrich
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  2. Siegfried Siegesmund
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Correspondence to Joerg Ruedrich.

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Ruedrich, J., Siegesmund, S. Salt and ice crystallisation in porous sandstones. Environ Geol 52, 225–249 (2007). https://doi.org/10.1007/s00254-006-0585-6

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  • DOI: https://doi.org/10.1007/s00254-006-0585-6

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