Geothermal study to explain man-made permafrost in tailings with raised surface

Deposition of mine tailings in a cold climate requires precautions as temporary sub-zero temperatures can imply considerable consequences to the storage due to creation of permafrost. The risk of creating man-made permafrost lenses due to tailings deposition exists even in regions with no natural pe...

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Published in:Environmental Earth Sciences
Main Authors: Knutsson, Roger, Viklander, Peter, Knutsson, Sven, Laue, Jan
Format: Article in Journal/Newspaper
Language:English
Published: Luleå tekniska universitet, Geoteknologi 2018
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-68239
https://doi.org/10.1007/s12665-018-7465-8
id ftluleatu:oai:DiVA.org:ltu-68239
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spelling ftluleatu:oai:DiVA.org:ltu-68239 2023-05-15T17:55:44+02:00 Geothermal study to explain man-made permafrost in tailings with raised surface Knutsson, Roger Viklander, Peter Knutsson, Sven Laue, Jan 2018 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-68239 https://doi.org/10.1007/s12665-018-7465-8 eng eng Luleå tekniska universitet, Geoteknologi Environmental Earth Sciences, 1866-6280, 2018, 77:7, http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-68239 doi:10.1007/s12665-018-7465-8 ISI:000429985900026 Scopus 2-s2.0-85044986446 info:eu-repo/semantics/openAccess Geotechnical Engineering Geoteknik Article in journal info:eu-repo/semantics/article text 2018 ftluleatu https://doi.org/10.1007/s12665-018-7465-8 2022-10-25T20:54:26Z Deposition of mine tailings in a cold climate requires precautions as temporary sub-zero temperatures can imply considerable consequences to the storage due to creation of permafrost. The risk of creating man-made permafrost lenses due to tailings deposition exists even in regions with no natural permafrost, as material being frozen during winter might not fully thaw by the following summer. When such frozen layers thaw during later longer warmer periods, excess pore water pressure and large settlements might develop. Such implications close to the dam structure have to be avoided and therefore the risk of generating permafrost should be reduced. This paper describes a geothermal model for one-dimensional heat conduction analysis. The model is able to simulate the temperature profile in tailings where the surface elevation is constantly increased due to deposition. At the tailings surface, the boundary condition is the air temperature changing over time during the year. Air temperatures, tailings deposition schedule and tailings properties are given as input to the model and can easily be changed and applied to specific facilities. The model can be used for tailings facilities in cold regions, where the effects of tailings deposition on the temperature regime are of interest. Findings can improve tailings management by explaining man-made permafrost generation. The model can also aid in setting up appropriate deposition schedules and to prevent generation of permafrost layers. Validerad;2018;Nivå 2;2018-04-09 (andbra) Article in Journal/Newspaper permafrost Luleå University of Technology Publications (DiVA) Environmental Earth Sciences 77 7
institution Open Polar
collection Luleå University of Technology Publications (DiVA)
op_collection_id ftluleatu
language English
topic Geotechnical Engineering
Geoteknik
spellingShingle Geotechnical Engineering
Geoteknik
Knutsson, Roger
Viklander, Peter
Knutsson, Sven
Laue, Jan
Geothermal study to explain man-made permafrost in tailings with raised surface
topic_facet Geotechnical Engineering
Geoteknik
description Deposition of mine tailings in a cold climate requires precautions as temporary sub-zero temperatures can imply considerable consequences to the storage due to creation of permafrost. The risk of creating man-made permafrost lenses due to tailings deposition exists even in regions with no natural permafrost, as material being frozen during winter might not fully thaw by the following summer. When such frozen layers thaw during later longer warmer periods, excess pore water pressure and large settlements might develop. Such implications close to the dam structure have to be avoided and therefore the risk of generating permafrost should be reduced. This paper describes a geothermal model for one-dimensional heat conduction analysis. The model is able to simulate the temperature profile in tailings where the surface elevation is constantly increased due to deposition. At the tailings surface, the boundary condition is the air temperature changing over time during the year. Air temperatures, tailings deposition schedule and tailings properties are given as input to the model and can easily be changed and applied to specific facilities. The model can be used for tailings facilities in cold regions, where the effects of tailings deposition on the temperature regime are of interest. Findings can improve tailings management by explaining man-made permafrost generation. The model can also aid in setting up appropriate deposition schedules and to prevent generation of permafrost layers. Validerad;2018;Nivå 2;2018-04-09 (andbra)
format Article in Journal/Newspaper
author Knutsson, Roger
Viklander, Peter
Knutsson, Sven
Laue, Jan
author_facet Knutsson, Roger
Viklander, Peter
Knutsson, Sven
Laue, Jan
author_sort Knutsson, Roger
title Geothermal study to explain man-made permafrost in tailings with raised surface
title_short Geothermal study to explain man-made permafrost in tailings with raised surface
title_full Geothermal study to explain man-made permafrost in tailings with raised surface
title_fullStr Geothermal study to explain man-made permafrost in tailings with raised surface
title_full_unstemmed Geothermal study to explain man-made permafrost in tailings with raised surface
title_sort geothermal study to explain man-made permafrost in tailings with raised surface
publisher Luleå tekniska universitet, Geoteknologi
publishDate 2018
url http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-68239
https://doi.org/10.1007/s12665-018-7465-8
genre permafrost
genre_facet permafrost
op_relation Environmental Earth Sciences, 1866-6280, 2018, 77:7,
http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-68239
doi:10.1007/s12665-018-7465-8
ISI:000429985900026
Scopus 2-s2.0-85044986446
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1007/s12665-018-7465-8
container_title Environmental Earth Sciences
container_volume 77
container_issue 7
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