1. Monitoring and Modelling the Thermally Assisted Deformation of a Rock Column Above Tomb KV42 in the Valley of the Kings, Egypt.
- Author
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Alcaíno-Olivares, Rodrigo, Ziegler, Martin, Bickel, Susanne, Leith, Kerry, and Perras, Matthew A.
- Subjects
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ROCK deformation , *COLUMNS , *WORLD Heritage Sites , *COMPOUND fractures , *DISPLACEMENT (Mechanics) , *FINITE differences - Abstract
The Valley of the Kings (KV) is located within a large funerary landscape called the Theban Necropolis, in Luxor, Egypt. In 2018, our team started to monitor the transient conditions of a 15 m rock column of micritic limestone above the tomb KV42 and a fracture located at the west end of the column (lateral fracture), registering thermo-mechanical displacements with a crack metre, infrared thermographic sensor, and a weather station. The data from April 2018 to May 2021 showed seasonal fluctuations in the rock surface temperature (RST) from 12°C (winter) to 45°C (summer), as well as an average reversible fracture opening (FO) rate of 1 mm/year. The measured average thermo-mechanical ratio of FO to RST was 0.05 mm/°C. Data collected at the site were used to calibrate a finite difference model in FLAC®8.0 for thermo-mechanical simulations. The results showed a correlation (R2) of 0.8 between measured data and elastic isotropic mechanical constitutive model results, with a ratio of FO to RST equal to 0.03 mm/°C and rates of reversible displacements of 0.8 mm/year, whereas the average irreversible displacement for the monitored period of 2018–2021 was 0.2 mm/year. The insights from this study can help provide a preservation approach for this area of the UNESCO World Heritage site and also enhance our understanding of environmentally driven long-term fracture growth mechanisms, such as thermo-mechanical fatigue. In the future, such insights could become more important as the global and local magnitude of daily and annual temperature fluctuations continue to increase. Highlights: Our team conducts fieldwork in the Valley of the Kings (Luxor, Egypt), monitoring a rock column of 15 m which is attached at the bottom to the adjacent cliff. Cyclic behaviour of temperature and fracture opening were registered between April 2018 and May 2021, at a ratio of 0.05 mm/°C. The fracture opening trend increased throughout the monitored period at rates of 0.2 mm/year, showing irreversible deformation of the rock column. Thermo-mechanical numerical model in FLAC (R) software intended to fit the observed data, under elastic conditions with an R2 of 0.8. The thermal inputs showed that thermal regions change in extension, associated to the shading patterns from the cliffs and hills around the rock column. For FLAC simulations, the ratio between fracture opening and rock surface temperature is 0.03 mm/°C. Because of the cyclic nature of the displacement with the rock temperature, thermally assisted deformations are relevant to determine stability of the rock mass. This is impacted by the presence of joints, affecting the stability and the heat transfer process inwards the column. This could explain differences between observed and simulated data. [ABSTRACT FROM AUTHOR]
- Published
- 2023
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