Exploring the in situ high temperature emissivity of 2014-2015 Bardarbunga magmas

International audience Temperature is a key parameter controlling the rheology of lava flows. Unfortunately, the hazardous behavior of eruptions prevents direct measurements of hot magmatic bodies. Hence, the temperature of magma is mostly retrieved by using remote sensing methods (ground-based or s...

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Main Authors: Biren, Jonas, Cosson, Lionel, del Campo, Leire, Genevois, Cécile, Veron, Emmanuel, Ory, Sandra, Li, Hao, Slodczyk, Aneta, Andújar, Joan
Other Authors: Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO), Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS), Magma - UMR7327, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Conditions Extrêmes et Matériaux : Haute Température et Irradiation (CEMHTI), Université d'Orléans (UO)-Institut de Chimie - CNRS Chimie (INC-CNRS)-Centre National de la Recherche Scientifique (CNRS)
Format: Conference Object
Language:English
Published: HAL CCSD 2021
Subjects:
Online Access:https://hal.science/hal-03554570
https://hal.science/hal-03554570/document
https://hal.science/hal-03554570/file/EGU21-714-print.pdf
https://doi.org/10.5194/egusphere-egu21-714
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institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic [SDU.STU]Sciences of the Universe [physics]/Earth Sciences
spellingShingle [SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Biren, Jonas
Cosson, Lionel
del Campo, Leire
Genevois, Cécile
Veron, Emmanuel
Ory, Sandra
Li, Hao
Slodczyk, Aneta
Andújar, Joan
Exploring the in situ high temperature emissivity of 2014-2015 Bardarbunga magmas
topic_facet [SDU.STU]Sciences of the Universe [physics]/Earth Sciences
description International audience Temperature is a key parameter controlling the rheology of lava flows. Unfortunately, the hazardous behavior of eruptions prevents direct measurements of hot magmatic bodies. Hence, the temperature of magma is mostly retrieved by using remote sensing methods (ground-based or satellite-based detectors) build on measuring the infrared (IR) radiance of the body [1]. These well-established techniques are however subjected to important errors related to, among others, the poor knowledge of the spectral emissivity (ɛ), which is one of the most critical parameters in IR radiance measurement [2, 3]. In this study, we performed in situ optical measurements at relevant magmatic temperatures of basaltic magma from the 2014-2015 Holuhraun eruption (Bardarbunga volcano, Iceland). Spectral emissivity has been systematically determined over a wide spectral range (400-15000 cm‑1) covering TIR, MIR and SWIR regions, from room temperature up to 1473 K using a non-contact in situ IR emissivity apparatus [4]. SEM, EMPA, Raman spectroscopy, DSC, XRD and TEM techniques helped characterize and understand the complex radiative behavior of this natural magmatic composition. The results show not only that spectral emissivity varies accordingly with temperature and wavenumber but also that small changes in bulk rock composition or texture produce drastic changes in emissivity at given temperature, with iron content and its oxidation state being the main agents controlling this parameter. Appropriate emissivity values can then be used to refine current radiative data from IR remote sensing and to implement the thermo-rheological models of lava flows [5] as to support hazard assessment and risk mitigation.References: [1] Kolzenburg et al. 2017. Bull. Volc. 79:45. [2] Harris, A. 2013: Cambridge University press. 728. [3] Rogic et al. 2019 Remote Sens., 11, 662 [4] De Sousa Meneses et al. 2015. Infrared Physics & Technology 69. [5] Ramsey et al. 2019. Annals of Geophysics, 62, 2.Keywords: Spectral emissivity, ...
author2 Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO)
Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC)
Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)
Magma - UMR7327
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC)
Conditions Extrêmes et Matériaux : Haute Température et Irradiation (CEMHTI)
Université d'Orléans (UO)-Institut de Chimie - CNRS Chimie (INC-CNRS)-Centre National de la Recherche Scientifique (CNRS)
format Conference Object
author Biren, Jonas
Cosson, Lionel
del Campo, Leire
Genevois, Cécile
Veron, Emmanuel
Ory, Sandra
Li, Hao
Slodczyk, Aneta
Andújar, Joan
author_facet Biren, Jonas
Cosson, Lionel
del Campo, Leire
Genevois, Cécile
Veron, Emmanuel
Ory, Sandra
Li, Hao
Slodczyk, Aneta
Andújar, Joan
author_sort Biren, Jonas
title Exploring the in situ high temperature emissivity of 2014-2015 Bardarbunga magmas
title_short Exploring the in situ high temperature emissivity of 2014-2015 Bardarbunga magmas
title_full Exploring the in situ high temperature emissivity of 2014-2015 Bardarbunga magmas
title_fullStr Exploring the in situ high temperature emissivity of 2014-2015 Bardarbunga magmas
title_full_unstemmed Exploring the in situ high temperature emissivity of 2014-2015 Bardarbunga magmas
title_sort exploring the in situ high temperature emissivity of 2014-2015 bardarbunga magmas
publisher HAL CCSD
publishDate 2021
url https://hal.science/hal-03554570
https://hal.science/hal-03554570/document
https://hal.science/hal-03554570/file/EGU21-714-print.pdf
https://doi.org/10.5194/egusphere-egu21-714
op_coverage Online, France
long_lat ENVELOPE(-17.528,-17.528,64.635,64.635)
ENVELOPE(-16.831,-16.831,64.852,64.852)
ENVELOPE(-62.167,-62.167,-64.650,-64.650)
geographic Bardarbunga
Holuhraun
Meneses
geographic_facet Bardarbunga
Holuhraun
Meneses
genre Iceland
genre_facet Iceland
op_source vEGU21: Gather Online
https://hal.science/hal-03554570
vEGU21: Gather Online, Apr 2021, Online, France. ⟨10.5194/egusphere-egu21-714⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/egusphere-egu21-714
hal-03554570
https://hal.science/hal-03554570
https://hal.science/hal-03554570/document
https://hal.science/hal-03554570/file/EGU21-714-print.pdf
BIBCODE: 2021EGUGA.23.714B
doi:10.5194/egusphere-egu21-714
op_rights http://creativecommons.org/licenses/by/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/egusphere-egu21-714
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spelling ftccsdartic:oai:HAL:hal-03554570v1 2024-01-14T10:08:04+01:00 Exploring the in situ high temperature emissivity of 2014-2015 Bardarbunga magmas Biren, Jonas Cosson, Lionel del Campo, Leire Genevois, Cécile Veron, Emmanuel Ory, Sandra Li, Hao Slodczyk, Aneta Andújar, Joan Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO) Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS) Magma - UMR7327 Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC) Conditions Extrêmes et Matériaux : Haute Température et Irradiation (CEMHTI) Université d'Orléans (UO)-Institut de Chimie - CNRS Chimie (INC-CNRS)-Centre National de la Recherche Scientifique (CNRS) Online, France 2021-04-19 https://hal.science/hal-03554570 https://hal.science/hal-03554570/document https://hal.science/hal-03554570/file/EGU21-714-print.pdf https://doi.org/10.5194/egusphere-egu21-714 en eng HAL CCSD info:eu-repo/semantics/altIdentifier/doi/10.5194/egusphere-egu21-714 hal-03554570 https://hal.science/hal-03554570 https://hal.science/hal-03554570/document https://hal.science/hal-03554570/file/EGU21-714-print.pdf BIBCODE: 2021EGUGA.23.714B doi:10.5194/egusphere-egu21-714 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess vEGU21: Gather Online https://hal.science/hal-03554570 vEGU21: Gather Online, Apr 2021, Online, France. ⟨10.5194/egusphere-egu21-714⟩ [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/conferenceObject Conference papers 2021 ftccsdartic https://doi.org/10.5194/egusphere-egu21-714 2023-12-17T00:24:42Z International audience Temperature is a key parameter controlling the rheology of lava flows. Unfortunately, the hazardous behavior of eruptions prevents direct measurements of hot magmatic bodies. Hence, the temperature of magma is mostly retrieved by using remote sensing methods (ground-based or satellite-based detectors) build on measuring the infrared (IR) radiance of the body [1]. These well-established techniques are however subjected to important errors related to, among others, the poor knowledge of the spectral emissivity (ɛ), which is one of the most critical parameters in IR radiance measurement [2, 3]. In this study, we performed in situ optical measurements at relevant magmatic temperatures of basaltic magma from the 2014-2015 Holuhraun eruption (Bardarbunga volcano, Iceland). Spectral emissivity has been systematically determined over a wide spectral range (400-15000 cm‑1) covering TIR, MIR and SWIR regions, from room temperature up to 1473 K using a non-contact in situ IR emissivity apparatus [4]. SEM, EMPA, Raman spectroscopy, DSC, XRD and TEM techniques helped characterize and understand the complex radiative behavior of this natural magmatic composition. The results show not only that spectral emissivity varies accordingly with temperature and wavenumber but also that small changes in bulk rock composition or texture produce drastic changes in emissivity at given temperature, with iron content and its oxidation state being the main agents controlling this parameter. Appropriate emissivity values can then be used to refine current radiative data from IR remote sensing and to implement the thermo-rheological models of lava flows [5] as to support hazard assessment and risk mitigation.References: [1] Kolzenburg et al. 2017. Bull. Volc. 79:45. [2] Harris, A. 2013: Cambridge University press. 728. [3] Rogic et al. 2019 Remote Sens., 11, 662 [4] De Sousa Meneses et al. 2015. Infrared Physics & Technology 69. [5] Ramsey et al. 2019. Annals of Geophysics, 62, 2.Keywords: Spectral emissivity, ... Conference Object Iceland Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Bardarbunga ENVELOPE(-17.528,-17.528,64.635,64.635) Holuhraun ENVELOPE(-16.831,-16.831,64.852,64.852) Meneses ENVELOPE(-62.167,-62.167,-64.650,-64.650)