Monitoring rock freezing and thawing by novel geoelectrical and acoustic techniques

• Published in: Journal of Geophysical Research: Earth Surface
• Main Authors: Murton, Julian B., Kuras, Oliver, Krautblatter, Michael, Cane, Tim, Tschofen, Dominique, Uhlemann, Sebastian, Schober, Sandra, Watson, Phil
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Geophysical Union 2016
• Subjects: Ice; permafrost
• Online Access: http://nora.nerc.ac.uk/id/eprint/516658/; https://nora.nerc.ac.uk/id/eprint/516658/1/Murton_et_al-2016-Journal_of_Geophysical_Research__Earth_Surface.pdf; https://doi.org/10.1002/2016JF003948

Automated monitoring of freeze-thaw cycles and fracture propagation in mountain rockwalls is needed to provide early warning about rockfall hazards. Conventional geoelectrical methods such as electrical resistivity tomography (ERT) are limited by large and variable ohmic contact resistances, requiring galvanic coupling with metal electrodes inserted into holes drilled into rock, and which can be loosened by rock weathering. We report a novel experimental methodology that combined capacitive resistivity imaging (CRI), ERT, and microseismic event recording to monitor freeze-thaw of six blocks of hard and soft limestones under conditions simulating an active layer above permafrost and seasonally frozen rock in a nonpermafrost environment. Our results demonstrate that the CRI method is highly sensitive to freeze-thaw processes; it yields property information equivalent to that obtained with conventional ERT and offers a viable route for nongalvanic long-term geoelectrical monitoring, extending the benefits of the methodology to soft/hard rock environments. Contact impedances achieved with CRI are less affected by seasonal temperature changes, the aggregate state of the pore water (liquid or frozen), and the presence of low-porosity rock with high matrix resistivities than those achieved with ERT. Microseismic monitoring has the advantage over acoustic emissions that events were recorded in relevant field distances of meters to decameters from cracking events. For the first time we recorded about 1000 microcracking events and clustered them in four groups according to frequency and waveform. Compared to previous studies, mainly on ice-cracking in glaciers, the groups are attributed to single- or multiple-stage cracking events such as crack coalescence.