Modelling the potential for permafrost development on a radioactive waste geological disposal facility in Great Britain

The safety case for a geological disposal facility (GDF) for radioactive waste based in Great Britain must consider the potential impact on the repository environment of permafrost during the 1 million years following GDF closure. The depth of penetration of permafrost, defined as ground which remai...

Full description

Bibliographic Details
Published in:Proceedings of the Geologists' Association
Main Authors: Busby, J.P., Lee, J.R., Kender, S., Williamson, J.P., Norris, S.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2015
Subjects:
Ice
Online Access:http://nora.nerc.ac.uk/id/eprint/512436/
https://nora.nerc.ac.uk/id/eprint/512436/1/PGA_v126_p664-674_2015.pdf
https://doi.org/10.1016/j.pgeola.2015.06.001
id ftnerc:oai:nora.nerc.ac.uk:512436
record_format openpolar
spelling ftnerc:oai:nora.nerc.ac.uk:512436 2023-05-15T16:36:40+02:00 Modelling the potential for permafrost development on a radioactive waste geological disposal facility in Great Britain Busby, J.P. Lee, J.R. Kender, S. Williamson, J.P. Norris, S. 2015 text http://nora.nerc.ac.uk/id/eprint/512436/ https://nora.nerc.ac.uk/id/eprint/512436/1/PGA_v126_p664-674_2015.pdf https://doi.org/10.1016/j.pgeola.2015.06.001 en eng Elsevier https://nora.nerc.ac.uk/id/eprint/512436/1/PGA_v126_p664-674_2015.pdf Busby, J.P.; Lee, J.R.; Kender, S.; Williamson, J.P.; Norris, S. 2015 Modelling the potential for permafrost development on a radioactive waste geological disposal facility in Great Britain. Proceedings of the Geologists' Association, 126 (6). 664-674. https://doi.org/10.1016/j.pgeola.2015.06.001 <https://doi.org/10.1016/j.pgeola.2015.06.001> Publication - Article PeerReviewed 2015 ftnerc https://doi.org/10.1016/j.pgeola.2015.06.001 2023-02-04T19:42:27Z The safety case for a geological disposal facility (GDF) for radioactive waste based in Great Britain must consider the potential impact on the repository environment of permafrost during the 1 million years following GDF closure. The depth of penetration of permafrost, defined as ground which remains at or below 0 °C for at least 2 consecutive years, has been modelled for a future climate that uses the climate of the last glacial–interglacial cycle as an analogue. Two future climates are considered; an average estimate case considered to be the best estimate of ground surface temperatures during the last glacial–interglacial cycle, and a cold estimate case considered to be an extreme cold, but plausible future climate. Maximum modelled permafrost thicknesses across Great Britain range from 20 to 180 m for the average estimate climate and 180–305 m for the cold estimate climate. The presence of ice cover is an important determinant on permafrost development. Thick permafrost evolves during long periods of cold-based ice cover and during periods of ice retreat that results in ground exposure to very cold air temperatures. Conversely, warm-based ice has an insulating effect, shielding the ground from cold air temperatures that retards permafrost development. For a GDF at a depth greater than that predicted to be directly affected by permafrost, phenomena associated with permafrost, e.g., enhanced groundwater salinity at depth, will need to be taken into account when considering the impact on the engineered and natural barriers associated with a GDF. Article in Journal/Newspaper Ice permafrost Natural Environment Research Council: NERC Open Research Archive Proceedings of the Geologists' Association 126 6 664 674
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language English
description The safety case for a geological disposal facility (GDF) for radioactive waste based in Great Britain must consider the potential impact on the repository environment of permafrost during the 1 million years following GDF closure. The depth of penetration of permafrost, defined as ground which remains at or below 0 °C for at least 2 consecutive years, has been modelled for a future climate that uses the climate of the last glacial–interglacial cycle as an analogue. Two future climates are considered; an average estimate case considered to be the best estimate of ground surface temperatures during the last glacial–interglacial cycle, and a cold estimate case considered to be an extreme cold, but plausible future climate. Maximum modelled permafrost thicknesses across Great Britain range from 20 to 180 m for the average estimate climate and 180–305 m for the cold estimate climate. The presence of ice cover is an important determinant on permafrost development. Thick permafrost evolves during long periods of cold-based ice cover and during periods of ice retreat that results in ground exposure to very cold air temperatures. Conversely, warm-based ice has an insulating effect, shielding the ground from cold air temperatures that retards permafrost development. For a GDF at a depth greater than that predicted to be directly affected by permafrost, phenomena associated with permafrost, e.g., enhanced groundwater salinity at depth, will need to be taken into account when considering the impact on the engineered and natural barriers associated with a GDF.
format Article in Journal/Newspaper
author Busby, J.P.
Lee, J.R.
Kender, S.
Williamson, J.P.
Norris, S.
spellingShingle Busby, J.P.
Lee, J.R.
Kender, S.
Williamson, J.P.
Norris, S.
Modelling the potential for permafrost development on a radioactive waste geological disposal facility in Great Britain
author_facet Busby, J.P.
Lee, J.R.
Kender, S.
Williamson, J.P.
Norris, S.
author_sort Busby, J.P.
title Modelling the potential for permafrost development on a radioactive waste geological disposal facility in Great Britain
title_short Modelling the potential for permafrost development on a radioactive waste geological disposal facility in Great Britain
title_full Modelling the potential for permafrost development on a radioactive waste geological disposal facility in Great Britain
title_fullStr Modelling the potential for permafrost development on a radioactive waste geological disposal facility in Great Britain
title_full_unstemmed Modelling the potential for permafrost development on a radioactive waste geological disposal facility in Great Britain
title_sort modelling the potential for permafrost development on a radioactive waste geological disposal facility in great britain
publisher Elsevier
publishDate 2015
url http://nora.nerc.ac.uk/id/eprint/512436/
https://nora.nerc.ac.uk/id/eprint/512436/1/PGA_v126_p664-674_2015.pdf
https://doi.org/10.1016/j.pgeola.2015.06.001
genre Ice
permafrost
genre_facet Ice
permafrost
op_relation https://nora.nerc.ac.uk/id/eprint/512436/1/PGA_v126_p664-674_2015.pdf
Busby, J.P.; Lee, J.R.; Kender, S.; Williamson, J.P.; Norris, S. 2015 Modelling the potential for permafrost development on a radioactive waste geological disposal facility in Great Britain. Proceedings of the Geologists' Association, 126 (6). 664-674. https://doi.org/10.1016/j.pgeola.2015.06.001 <https://doi.org/10.1016/j.pgeola.2015.06.001>
op_doi https://doi.org/10.1016/j.pgeola.2015.06.001
container_title Proceedings of the Geologists' Association
container_volume 126
container_issue 6
container_start_page 664
op_container_end_page 674
_version_ 1766027005055205376