Timescales of spherulite crystallization in obsidian inferred from water concentration profiles
International audience We determined the kinetics of spherulite growth in obsidians from Krafla volcano, Iceland. We measured water concentration profiles around spherulites in obsidian by synchrotron Fourier transform infrared spectroscopy. The distribution of OH– groups surrounding spherulites dec...
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ftinsu:oai:HAL:insu-00363340v1 2024-04-21T08:05:39+00:00 Timescales of spherulite crystallization in obsidian inferred from water concentration profiles Castro, J. M. Beck, Pierre Tuffen, H. Nichols, Alexander R.L. Dingwell, Donald B. Martin, Michael C. Department of Mineral Sciences Washington Smithsonian Institution Laboratoire de Planétologie de Grenoble (LPG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Department of Environmental Science Lancaster Lancaster University Institute for Research on Earth Evolution Yokosuka (IFREE) Japan Agency for Marine-Earth Science and Technology (JAMSTEC) Department of Earth and Environmental Sciences Munich Ludwig Maximilian University Munich = Ludwig Maximilians Universität München (LMU) Advanced Light Source LBNL Berkeley (ALS) Lawrence Berkeley National Laboratory Berkeley (LBNL) 2008 https://insu.hal.science/insu-00363340 https://doi.org/10.2138/am.2008.2904 en eng HAL CCSD Mineralogical Society of America info:eu-repo/semantics/altIdentifier/doi/10.2138/am.2008.2904 insu-00363340 https://insu.hal.science/insu-00363340 doi:10.2138/am.2008.2904 ISSN: 0003-004X EISSN: 1945-3027 The American Mineralogist https://insu.hal.science/insu-00363340 The American Mineralogist, 2008, 93 (11-12), pp.1816-1822. ⟨10.2138/am.2008.2904⟩ Spherulite • diffusion • obsidian • crystallization info:eu-repo/semantics/article Journal articles 2008 ftinsu https://doi.org/10.2138/am.2008.2904 2024-04-05T00:34:31Z International audience We determined the kinetics of spherulite growth in obsidians from Krafla volcano, Iceland. We measured water concentration profiles around spherulites in obsidian by synchrotron Fourier transform infrared spectroscopy. The distribution of OH– groups surrounding spherulites decreases exponentially away from the spherulite-glass border, reflecting expulsion of water during crystallization of an anhydrous paragenesis (plagioclase + SiO2 + clinopyroxene + magnetite). This pattern is controlled by a balance between the growth rate of the spherulites and the diffusivity of hydrous solute in the rhyolitic melt. We modeled advective and diffusive transport of the water away from the growing spherulites by numerically solving the diffusion equation with a moving boundary. Numerical models fit the natural data best when a small amount of post-growth diffusion is incorporated in the model. Comparisons between models and data constrain the average spherulite growth rates for different temperatures and highlight size-dependent growth among a small population of spherulites. Article in Journal/Newspaper Iceland Institut national des sciences de l'Univers: HAL-INSU American Mineralogist 93 11-12 1816 1822 |
institution |
Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
Spherulite • diffusion • obsidian • crystallization |
spellingShingle |
Spherulite • diffusion • obsidian • crystallization Castro, J. M. Beck, Pierre Tuffen, H. Nichols, Alexander R.L. Dingwell, Donald B. Martin, Michael C. Timescales of spherulite crystallization in obsidian inferred from water concentration profiles |
topic_facet |
Spherulite • diffusion • obsidian • crystallization |
description |
International audience We determined the kinetics of spherulite growth in obsidians from Krafla volcano, Iceland. We measured water concentration profiles around spherulites in obsidian by synchrotron Fourier transform infrared spectroscopy. The distribution of OH– groups surrounding spherulites decreases exponentially away from the spherulite-glass border, reflecting expulsion of water during crystallization of an anhydrous paragenesis (plagioclase + SiO2 + clinopyroxene + magnetite). This pattern is controlled by a balance between the growth rate of the spherulites and the diffusivity of hydrous solute in the rhyolitic melt. We modeled advective and diffusive transport of the water away from the growing spherulites by numerically solving the diffusion equation with a moving boundary. Numerical models fit the natural data best when a small amount of post-growth diffusion is incorporated in the model. Comparisons between models and data constrain the average spherulite growth rates for different temperatures and highlight size-dependent growth among a small population of spherulites. |
author2 |
Department of Mineral Sciences Washington Smithsonian Institution Laboratoire de Planétologie de Grenoble (LPG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Department of Environmental Science Lancaster Lancaster University Institute for Research on Earth Evolution Yokosuka (IFREE) Japan Agency for Marine-Earth Science and Technology (JAMSTEC) Department of Earth and Environmental Sciences Munich Ludwig Maximilian University Munich = Ludwig Maximilians Universität München (LMU) Advanced Light Source LBNL Berkeley (ALS) Lawrence Berkeley National Laboratory Berkeley (LBNL) |
format |
Article in Journal/Newspaper |
author |
Castro, J. M. Beck, Pierre Tuffen, H. Nichols, Alexander R.L. Dingwell, Donald B. Martin, Michael C. |
author_facet |
Castro, J. M. Beck, Pierre Tuffen, H. Nichols, Alexander R.L. Dingwell, Donald B. Martin, Michael C. |
author_sort |
Castro, J. M. |
title |
Timescales of spherulite crystallization in obsidian inferred from water concentration profiles |
title_short |
Timescales of spherulite crystallization in obsidian inferred from water concentration profiles |
title_full |
Timescales of spherulite crystallization in obsidian inferred from water concentration profiles |
title_fullStr |
Timescales of spherulite crystallization in obsidian inferred from water concentration profiles |
title_full_unstemmed |
Timescales of spherulite crystallization in obsidian inferred from water concentration profiles |
title_sort |
timescales of spherulite crystallization in obsidian inferred from water concentration profiles |
publisher |
HAL CCSD |
publishDate |
2008 |
url |
https://insu.hal.science/insu-00363340 https://doi.org/10.2138/am.2008.2904 |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
ISSN: 0003-004X EISSN: 1945-3027 The American Mineralogist https://insu.hal.science/insu-00363340 The American Mineralogist, 2008, 93 (11-12), pp.1816-1822. ⟨10.2138/am.2008.2904⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.2138/am.2008.2904 insu-00363340 https://insu.hal.science/insu-00363340 doi:10.2138/am.2008.2904 |
op_doi |
https://doi.org/10.2138/am.2008.2904 |
container_title |
American Mineralogist |
container_volume |
93 |
container_issue |
11-12 |
container_start_page |
1816 |
op_container_end_page |
1822 |
_version_ |
1796945089578139648 |