More than eleven years of temperature and displacements recorded on and in a limestone cliff: Dataset

This data set gives more than 11 years of temperature and displacements recorded on and in a limestone cliff. An extensive presentation of the monitoring devices and interpretation of data is proposed in Gasc-Barbier et al. (2021) [1].The hazard-monitored zone is a perched cave in a limestone cliff...

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Autores principales:	Didier Virely, Muriel Gasc-Barbier, Véronique Merrien-Soukatchoff
Formato:	article
Lenguaje:	EN
Publicado:	Elsevier 2021
Materias:	Rock joints Rock cliff stability In situ monitoring Temperature and displacement recording In depth evolution of the rock mass Computer applications to medicine. Medical informatics R858-859.7 Science (General) Q1-390
Acceso en línea:	https://doaj.org/article/2ded0899093a403e9957611a3f929b81
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spelling	oai:doaj.org-article:2ded0899093a403e9957611a3f929b812021-11-22T04:26:47ZMore than eleven years of temperature and displacements recorded on and in a limestone cliff: Dataset2352-340910.1016/j.dib.2021.107568https://doaj.org/article/2ded0899093a403e9957611a3f929b812021-12-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S2352340921008441https://doaj.org/toc/2352-3409This data set gives more than 11 years of temperature and displacements recorded on and in a limestone cliff. An extensive presentation of the monitoring devices and interpretation of data is proposed in Gasc-Barbier et al. (2021) [1].The hazard-monitored zone is a perched cave in a limestone cliff where a part of its roof had collapsed. On its roof, an unstable beam reminds. A horizontal interlayer thinning from East to West, hanging to the roof of the cave at the west and east-clamped in the rock mass, delimits this remaining beam. Opened fractures can be observed all around the beam. In order to assess the remaining hazard, four fissurometers (F1 to F4) and a thermal probe were installed on the roof of the cave and two borehole extensometers (D1 and D2) were drilled perpendicular to the face of the cliff, above the cave, to understand the global behaviour of the rock mass. Measurements have been made between sockets embedded in the rock mass by means of INVAR wire measurements. Four bases made of two sockets each have been installed inside the cavity and five were put on the face of the cliff outside and above the cavity. Measurements last between January 2011 and June 2021. A 1.5-year gap is observed in the measurements because they were temporally stopped when reinforcement works were preceded carried out in the cave in order to secure the village.Thus, datasets provide more than 11 years of temperature and displacements recorded on and in the cliff, providing insight on the relation between climate and the deformation inside the rock mass. This dataset is novel because this type of data is not readily available in the literature, on the one hand, because of its length (nearly 11 years) and, on the other hand, because it is not only surface evolution of temperature and aperture but because the evolution of temperature and deformation inside the rock mass was monitored. Researchers could use these data for a better understanding of the thermomechanical coupling in rock. They could test their own modelling, constitutive laws specifically on crack propagation or thermal fatigue.Didier VirelyMuriel Gasc-BarbierVéronique Merrien-SoukatchoffElsevierarticleRock jointsRock cliff stabilityIn situ monitoringTemperature and displacement recordingIn depth evolution of the rock massComputer applications to medicine. Medical informaticsR858-859.7Science (General)Q1-390ENData in Brief, Vol 39, Iss , Pp 107568- (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Rock joints Rock cliff stability In situ monitoring Temperature and displacement recording In depth evolution of the rock mass Computer applications to medicine. Medical informatics R858-859.7 Science (General) Q1-390
spellingShingle	Rock joints Rock cliff stability In situ monitoring Temperature and displacement recording In depth evolution of the rock mass Computer applications to medicine. Medical informatics R858-859.7 Science (General) Q1-390 Didier Virely Muriel Gasc-Barbier Véronique Merrien-Soukatchoff More than eleven years of temperature and displacements recorded on and in a limestone cliff: Dataset
description	This data set gives more than 11 years of temperature and displacements recorded on and in a limestone cliff. An extensive presentation of the monitoring devices and interpretation of data is proposed in Gasc-Barbier et al. (2021) [1].The hazard-monitored zone is a perched cave in a limestone cliff where a part of its roof had collapsed. On its roof, an unstable beam reminds. A horizontal interlayer thinning from East to West, hanging to the roof of the cave at the west and east-clamped in the rock mass, delimits this remaining beam. Opened fractures can be observed all around the beam. In order to assess the remaining hazard, four fissurometers (F1 to F4) and a thermal probe were installed on the roof of the cave and two borehole extensometers (D1 and D2) were drilled perpendicular to the face of the cliff, above the cave, to understand the global behaviour of the rock mass. Measurements have been made between sockets embedded in the rock mass by means of INVAR wire measurements. Four bases made of two sockets each have been installed inside the cavity and five were put on the face of the cliff outside and above the cavity. Measurements last between January 2011 and June 2021. A 1.5-year gap is observed in the measurements because they were temporally stopped when reinforcement works were preceded carried out in the cave in order to secure the village.Thus, datasets provide more than 11 years of temperature and displacements recorded on and in the cliff, providing insight on the relation between climate and the deformation inside the rock mass. This dataset is novel because this type of data is not readily available in the literature, on the one hand, because of its length (nearly 11 years) and, on the other hand, because it is not only surface evolution of temperature and aperture but because the evolution of temperature and deformation inside the rock mass was monitored. Researchers could use these data for a better understanding of the thermomechanical coupling in rock. They could test their own modelling, constitutive laws specifically on crack propagation or thermal fatigue.
format	article
author	Didier Virely Muriel Gasc-Barbier Véronique Merrien-Soukatchoff
author_facet	Didier Virely Muriel Gasc-Barbier Véronique Merrien-Soukatchoff
author_sort	Didier Virely
title	More than eleven years of temperature and displacements recorded on and in a limestone cliff: Dataset
title_short	More than eleven years of temperature and displacements recorded on and in a limestone cliff: Dataset
title_full	More than eleven years of temperature and displacements recorded on and in a limestone cliff: Dataset
title_fullStr	More than eleven years of temperature and displacements recorded on and in a limestone cliff: Dataset
title_full_unstemmed	More than eleven years of temperature and displacements recorded on and in a limestone cliff: Dataset
title_sort	more than eleven years of temperature and displacements recorded on and in a limestone cliff: dataset
publisher	Elsevier
publishDate	2021
url	https://doaj.org/article/2ded0899093a403e9957611a3f929b81
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More than eleven years of temperature and displacements recorded on and in a limestone cliff: Dataset

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