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dc.contributor.authorHOUILLON, Nicolas
IDREF: 198194978
dc.contributor.authorLASTENNET, Roland
IDREF: 079112056
hal.structure.identifierLaboratoire Inter-universitaire de Psychologie : Personnalité, Cognition, Changement Social [LIP-PC2S ]
dc.contributor.authorDENIS, Alain
IDREF: 095129243
dc.contributor.authorMALAURENT, P.
hal.structure.identifierCentre Hospitalier Universitaire de Nantes = Nantes University Hospital [CHU Nantes]
dc.contributor.authorMINVIELLE, S.
hal.structure.identifierService National d'Observation sur le KARST [SNO Karst]
dc.contributor.authorPEYRAUBE, Nicolas
IDREF: 157074005
dc.date.accessioned2021-05-14T09:30:39Z
dc.date.available2021-05-14T09:30:39Z
dc.date.issued2017-02
dc.identifier.issn1866-6280
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/75828
dc.description.abstractEnCarbon dioxide gas is a key component in dissolution and precipitation of carbonates in karst and cave systems. Therefore, characterizing the internal aerology of a cave is essential to obtain the spatiotemporal distribution of temperature and CO2 level. In this research, Lascaux Cave (France), an important adorned cavity, was studied. First, the spatiotemporal distribution of CO2 and temperatures were examined using continuous monitoring at a per minute basis. High-resolution spatial measurements (14 PCO2 locations and 27 locations for temperature) were carried out for a year in the epikarst and the cave (February 2015 to February 2016). The spatiotemporal analysis presents that air and rock temperatures vary for less than a degree Celsius (12.4–12.9 °C). These are controlled by the conduction of the external thermal waves through the overlying calcarenite massif. As a consequence, two seasonal internal aerologic regimes were identified: stratification and convection. These regimes govern the spatiotemporal distribution of the CO2 levels (1.1–3.7%), showing that this parameter is a good natural marker of the internal air movements. Second, a method was proposed to estimate the calcite mass potentially affected by condensation water (dissolution process) and exfiltration water (precipitation process). This method, based on numerical simulations, relies on CO2 and air and rock temperature spatiotemporal distributions in the cave. Third, the method was applied using the case of the left wall of the Hall of the Bulls (one of the most adorned part of the cave). Results showed that the calcite mass, possibly dissolved, varies from 0.0002 to 0.006 g when the mass potentially precipitated is higher (from 0.013 to 0.067 g) depending on the aerologic conditions. This method allows determining which alteration process (e.g., precipitation or dissolution) could eventually lead to the largest variation of calcite on the wall. The results can serve as useful data to the cave experts of the French Ministry of Culture and Communication in terms of Lascaux Cave management policies.
dc.language.isoen
dc.publisherSpringer
dc.subject.enCarbon dioxide
dc.subject.enComplex monitoring
dc.subject.enKarst cave aerology
dc.subject.enCalcium carbonate
dc.title.enAssessing cave internal aerology in understanding carbon dioxide (CO2) dynamics: implications on calcite mass variation on the wall of Lascaux Cave (France)
dc.typeArticle de revue
dc.identifier.doi10.1007/s12665-017-6498-8
dc.subject.halPlanète et Univers [physics]/Interfaces continentales, environnement
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Hydrologie
dc.subject.halSciences de l'environnement/Milieux et Changements globaux
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Géomorphologie
bordeaux.journalEnvironmental Earth Sciences
bordeaux.page170
bordeaux.volume76
bordeaux.hal.laboratoriesInstitut de Mécanique et d’Ingénierie de Bordeaux (I2M) - UMR 5295*
bordeaux.issue4
bordeaux.institutionUniversité de Bordeaux
bordeaux.institutionBordeaux INP
bordeaux.institutionCNRS
bordeaux.institutionINRAE
bordeaux.institutionArts et Métiers
bordeaux.peerReviewedoui
hal.identifierhal-03166769
hal.version1
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-03166769v1
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Environmental%20Earth%20Sciences&rft.date=2017-02&rft.volume=76&rft.issue=4&rft.spage=170&rft.epage=170&rft.eissn=1866-6280&rft.issn=1866-6280&rft.au=HOUILLON,%20Nicolas&LASTENNET,%20Roland&DENIS,%20Alain&MALAURENT,%20P.&MINVIELLE,%20S.&rft.genre=article


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