Shallow Permafrost at the Crystal Site of Peaceful Underground Nuclear Explosion (Yakutia, Russia): Evidence from Electrical Resistivity Tomography

The site where a peaceful underground nuclear explosion, Crystal, was detonated in 1974, at a depth of 98 m in perennially frozen Cambrian limestones, was studied by electrical resistivity tomography (ERT) in 2019. The purpose of our research, the results of which are presented in this article, was...

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Published in:Energies
Main Authors: Svetlana Artamonova, Alexander Shein, Vladimir Potapov, Nikolay Kozhevnikov, Vladislav Ushnitsky
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/en15010301
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spelling ftmdpi:oai:mdpi.com:/1996-1073/15/1/301/ 2023-08-20T04:09:10+02:00 Shallow Permafrost at the Crystal Site of Peaceful Underground Nuclear Explosion (Yakutia, Russia): Evidence from Electrical Resistivity Tomography Svetlana Artamonova Alexander Shein Vladimir Potapov Nikolay Kozhevnikov Vladislav Ushnitsky 2022-01-03 application/pdf https://doi.org/10.3390/en15010301 EN eng Multidisciplinary Digital Publishing Institute H: Geo-Energy https://dx.doi.org/10.3390/en15010301 https://creativecommons.org/licenses/by/4.0/ Energies; Volume 15; Issue 1; Pages: 301 environment research peaceful underground nuclear explosion electrical resistivity tomography permafrost geological environment natural–technical system Yakutia Text 2022 ftmdpi https://doi.org/10.3390/en15010301 2023-08-01T03:43:56Z The site where a peaceful underground nuclear explosion, Crystal, was detonated in 1974, at a depth of 98 m in perennially frozen Cambrian limestones, was studied by electrical resistivity tomography (ERT) in 2019. The purpose of our research, the results of which are presented in this article, was to assess the current permafrost state at the Crystal site and its surroundings by inversion and interpretation of electrical resistivity tomography (ERT) data. Inversion of the ERT data in Res2Dinv verified against ZondRes2D forward models yielded 2D inverted resistivity sections to a depth of 80 m. The ERT images revealed locally degrading permafrost at the Crystal site and its surroundings. The warming effect was caused by two main factors: (i) a damage zone of deformed rocks permeable to heat and fluids, with a radius of 160 m around the emplacement hole; (ii) the removal of natural land cover at the site in 2006. The artificial cover of rock from a nearby quarry, which was put up above the emplacement hole in order to prevent erosion and migration of radionuclides, is currently unfrozen. Text permafrost Yakutia MDPI Open Access Publishing Energies 15 1 301
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic environment research
peaceful underground nuclear explosion
electrical resistivity tomography
permafrost
geological environment
natural–technical system
Yakutia
spellingShingle environment research
peaceful underground nuclear explosion
electrical resistivity tomography
permafrost
geological environment
natural–technical system
Yakutia
Svetlana Artamonova
Alexander Shein
Vladimir Potapov
Nikolay Kozhevnikov
Vladislav Ushnitsky
Shallow Permafrost at the Crystal Site of Peaceful Underground Nuclear Explosion (Yakutia, Russia): Evidence from Electrical Resistivity Tomography
topic_facet environment research
peaceful underground nuclear explosion
electrical resistivity tomography
permafrost
geological environment
natural–technical system
Yakutia
description The site where a peaceful underground nuclear explosion, Crystal, was detonated in 1974, at a depth of 98 m in perennially frozen Cambrian limestones, was studied by electrical resistivity tomography (ERT) in 2019. The purpose of our research, the results of which are presented in this article, was to assess the current permafrost state at the Crystal site and its surroundings by inversion and interpretation of electrical resistivity tomography (ERT) data. Inversion of the ERT data in Res2Dinv verified against ZondRes2D forward models yielded 2D inverted resistivity sections to a depth of 80 m. The ERT images revealed locally degrading permafrost at the Crystal site and its surroundings. The warming effect was caused by two main factors: (i) a damage zone of deformed rocks permeable to heat and fluids, with a radius of 160 m around the emplacement hole; (ii) the removal of natural land cover at the site in 2006. The artificial cover of rock from a nearby quarry, which was put up above the emplacement hole in order to prevent erosion and migration of radionuclides, is currently unfrozen.
format Text
author Svetlana Artamonova
Alexander Shein
Vladimir Potapov
Nikolay Kozhevnikov
Vladislav Ushnitsky
author_facet Svetlana Artamonova
Alexander Shein
Vladimir Potapov
Nikolay Kozhevnikov
Vladislav Ushnitsky
author_sort Svetlana Artamonova
title Shallow Permafrost at the Crystal Site of Peaceful Underground Nuclear Explosion (Yakutia, Russia): Evidence from Electrical Resistivity Tomography
title_short Shallow Permafrost at the Crystal Site of Peaceful Underground Nuclear Explosion (Yakutia, Russia): Evidence from Electrical Resistivity Tomography
title_full Shallow Permafrost at the Crystal Site of Peaceful Underground Nuclear Explosion (Yakutia, Russia): Evidence from Electrical Resistivity Tomography
title_fullStr Shallow Permafrost at the Crystal Site of Peaceful Underground Nuclear Explosion (Yakutia, Russia): Evidence from Electrical Resistivity Tomography
title_full_unstemmed Shallow Permafrost at the Crystal Site of Peaceful Underground Nuclear Explosion (Yakutia, Russia): Evidence from Electrical Resistivity Tomography
title_sort shallow permafrost at the crystal site of peaceful underground nuclear explosion (yakutia, russia): evidence from electrical resistivity tomography
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/en15010301
genre permafrost
Yakutia
genre_facet permafrost
Yakutia
op_source Energies; Volume 15; Issue 1; Pages: 301
op_relation H: Geo-Energy
https://dx.doi.org/10.3390/en15010301
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/en15010301
container_title Energies
container_volume 15
container_issue 1
container_start_page 301
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