Spatio-temporal evolution of temperature and fluid flow through a new 'thermo-lithological' boundary; the case of a pit crater of Karthala volcano (Comoros archipelago) refilled on January 13th 2007 by a lava flow

Autor: Noé Bernabeu, Eric Delcher, Claude Smutek, Anthony Finizola, Pierre Saramito
Přispěvatelé: Equations aux Dérivées Partielles (EDP ), Laboratoire Jean Kuntzmann (LJK ), Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut National de Recherche en Informatique et en Automatique (Inria)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes [2016-2019] (UGA [2016-2019])-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut National de Recherche en Informatique et en Automatique (Inria)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes [2016-2019] (UGA [2016-2019]), Laboratoire GéoSciences Réunion (LGSR), Université de La Réunion (UR)-Institut de Physique du Globe de Paris, ANR-16-CE39-0009,LAVA,Lava et la Ville: l'évaluation des risques, de réduction des risques et de gestion des crises de effusive Désastres(2016), Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris), Institut de Physique du Globe de Paris (IPGP (UMR_7154)), Institut national des sciences de l'Univers (INSU - CNRS)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)
Rok vydání: 2018
Předmět:
Zdroj: Journal of Volcanology and Geothermal Research
Journal of Volcanology and Geothermal Research, Elsevier, 2018, 367, pp.7-19. ⟨10.1016/j.jvolgeores.2018.10.013⟩
Journal of Volcanology and Geothermal Research, 2018, 367, pp.7-19. ⟨10.1016/j.jvolgeores.2018.10.013⟩
ISSN: 0377-0273
Popis: International audience; On January 13 th 2007 the effusive eruption of Karthala volcano, in the Comoros islands, emitted a lava flow which has been perfectly constrained inside the cylindrical shape of the Choungou Chagnoumeni pit crater; 225m in diameter and with a thickness of about 7m. The good knowledge of the geometry of this lava flow allowed modeling its cooling, with the Rheolef code, with a good accuracy. The results of the thermal modeling were compared with other measurements performed on the field: (1) a high resolution electrical resistivity tomography profile crossing the boundary of the crater and (2) the thermal monitoring of temperature with eleven sensors, spaced 1 meter apart, at 30 cm depth, perpendicularly to the boundary of the crater. Thanks to this multidisciplinary approach it has been possible to display that, in the first order, the resistivity distribution in the soil 2 years and 5 months after the eruption is directly influenced by the residual temperature and not by the structural boundary. During the first three years of cooling, an inversion in the shallow lateral temperature gradient was observed in temperature data set collected at 30 cm depth.
Databáze: OpenAIRE