You learn as long as you drill; research synthesis from the Longyearbyen CO2 Laboratory, Svalbard, Norway
From 2007 to 2015, eight wells were drilled and fully cored to test the feasibility of storing CO 2 emitted from the coal-fueled power plant in Longyearbyen, Svalbard. The drilling campaign identified three water-bearing sandstone aquifers; i) a lower aquifer in Upper Triassic strata; ii) a middle a...
Published in: | Norwegian Journal of Geology |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Norwegian Journal of Geology
2020
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Subjects: | |
Online Access: | https://hdl.handle.net/10037/17559 https://doi.org/10.17850/njg008 |
_version_ | 1829311099309129728 |
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author | Olaussen, Snorre Senger, Kim Braathen, Alvar Grundvåg, Sten-Andreas Mørk, Atle |
author_facet | Olaussen, Snorre Senger, Kim Braathen, Alvar Grundvåg, Sten-Andreas Mørk, Atle |
author_sort | Olaussen, Snorre |
collection | University of Tromsø: Munin Open Research Archive |
container_title | Norwegian Journal of Geology |
description | From 2007 to 2015, eight wells were drilled and fully cored to test the feasibility of storing CO 2 emitted from the coal-fueled power plant in Longyearbyen, Svalbard. The drilling campaign identified three water-bearing sandstone aquifers; i) a lower aquifer in Upper Triassic strata; ii) a middle aquifer in Upper Triassic to Middle Jurassic; and iii) an upper aquifer in Lower Cretaceous strata. Only the two former are regarded as potential CO 2 storage units. Both units are unconventional reservoirs (storage units) consisting of fractured, low-porosity and low-permeability sandstones. The storage units are capped by a c. 400 m-thick Middle Jurassic to Lower Cretaceous mudstone-dominated succession, which acts as an efficient top seal. In addition, a c. 120 m-thick zone of permafrost provides an additional seal. Apart from characterising the CO 2 storage and cap-rock system, the drilling resulted in several unexpected results. These include: (a) the detection of severe underpressure of approximately 50 bar in the two storage units, (b) the discovery of gravity-flow deposits attributed to a hitherto unknown Hauterivian clastic wedge, and (c) the detection of producible thermogenic shale gas at a depth of 640 to 700 m. Moreover, core and wireline data from the wells combined with correlation to equivalent strata in nearby outcrops provide new insights into the age and depositional evolution of the succession. Thus, the data obtained from this project contributes to the regional stratigraphic understanding of the Mesozoic succession in Svalbard and the northern Barents Shelf. Until now, nearly 70 papers have been published in international peer-reviewed journals using data from or part of the Longyearbyen CO 2 Laboratory. In addition, 13 PhD candidates and 27 master students, linked to the project or using obtained data from the project, have graduated. The main achievement of our studies is that we have shown that unconventional fractured reservoirs are suitable for storing CO 2 . |
format | Article in Journal/Newspaper |
genre | Longyearbyen permafrost Svalbard wedge* |
genre_facet | Longyearbyen permafrost Svalbard wedge* |
geographic | Longyearbyen Norway Svalbard |
geographic_facet | Longyearbyen Norway Svalbard |
id | ftunivtroemsoe:oai:munin.uit.no:10037/17559 |
institution | Open Polar |
language | English |
op_collection_id | ftunivtroemsoe |
op_doi | https://doi.org/10.17850/njg008 |
op_relation | Norwegian Journal of Geology Norges forskningsråd: 228107 Norges forskningsråd: 257579 https://njg.geologi.no/images/NJG_articles/NJG_Vol99_Nr2_Art1_Olaussen_etal.pdf FRIDAID 1749286 doi:10.17850/njg008 https://hdl.handle.net/10037/17559 |
op_rights | openAccess Copyright 2019 The Author(s) |
publishDate | 2020 |
publisher | Norwegian Journal of Geology |
record_format | openpolar |
spelling | ftunivtroemsoe:oai:munin.uit.no:10037/17559 2025-04-13T14:22:24+00:00 You learn as long as you drill; research synthesis from the Longyearbyen CO2 Laboratory, Svalbard, Norway Olaussen, Snorre Senger, Kim Braathen, Alvar Grundvåg, Sten-Andreas Mørk, Atle 2020-01-21 https://hdl.handle.net/10037/17559 https://doi.org/10.17850/njg008 eng eng Norwegian Journal of Geology Norwegian Journal of Geology Norges forskningsråd: 228107 Norges forskningsråd: 257579 https://njg.geologi.no/images/NJG_articles/NJG_Vol99_Nr2_Art1_Olaussen_etal.pdf FRIDAID 1749286 doi:10.17850/njg008 https://hdl.handle.net/10037/17559 openAccess Copyright 2019 The Author(s) VDP::Mathematics and natural science: 400::Geosciences: 450 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 Journal article Tidsskriftartikkel Peer reviewed publishedVersion 2020 ftunivtroemsoe https://doi.org/10.17850/njg008 2025-03-14T05:17:57Z From 2007 to 2015, eight wells were drilled and fully cored to test the feasibility of storing CO 2 emitted from the coal-fueled power plant in Longyearbyen, Svalbard. The drilling campaign identified three water-bearing sandstone aquifers; i) a lower aquifer in Upper Triassic strata; ii) a middle aquifer in Upper Triassic to Middle Jurassic; and iii) an upper aquifer in Lower Cretaceous strata. Only the two former are regarded as potential CO 2 storage units. Both units are unconventional reservoirs (storage units) consisting of fractured, low-porosity and low-permeability sandstones. The storage units are capped by a c. 400 m-thick Middle Jurassic to Lower Cretaceous mudstone-dominated succession, which acts as an efficient top seal. In addition, a c. 120 m-thick zone of permafrost provides an additional seal. Apart from characterising the CO 2 storage and cap-rock system, the drilling resulted in several unexpected results. These include: (a) the detection of severe underpressure of approximately 50 bar in the two storage units, (b) the discovery of gravity-flow deposits attributed to a hitherto unknown Hauterivian clastic wedge, and (c) the detection of producible thermogenic shale gas at a depth of 640 to 700 m. Moreover, core and wireline data from the wells combined with correlation to equivalent strata in nearby outcrops provide new insights into the age and depositional evolution of the succession. Thus, the data obtained from this project contributes to the regional stratigraphic understanding of the Mesozoic succession in Svalbard and the northern Barents Shelf. Until now, nearly 70 papers have been published in international peer-reviewed journals using data from or part of the Longyearbyen CO 2 Laboratory. In addition, 13 PhD candidates and 27 master students, linked to the project or using obtained data from the project, have graduated. The main achievement of our studies is that we have shown that unconventional fractured reservoirs are suitable for storing CO 2 . Article in Journal/Newspaper Longyearbyen permafrost Svalbard wedge* University of Tromsø: Munin Open Research Archive Longyearbyen Norway Svalbard Norwegian Journal of Geology |
spellingShingle | VDP::Mathematics and natural science: 400::Geosciences: 450 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 Olaussen, Snorre Senger, Kim Braathen, Alvar Grundvåg, Sten-Andreas Mørk, Atle You learn as long as you drill; research synthesis from the Longyearbyen CO2 Laboratory, Svalbard, Norway |
title | You learn as long as you drill; research synthesis from the Longyearbyen CO2 Laboratory, Svalbard, Norway |
title_full | You learn as long as you drill; research synthesis from the Longyearbyen CO2 Laboratory, Svalbard, Norway |
title_fullStr | You learn as long as you drill; research synthesis from the Longyearbyen CO2 Laboratory, Svalbard, Norway |
title_full_unstemmed | You learn as long as you drill; research synthesis from the Longyearbyen CO2 Laboratory, Svalbard, Norway |
title_short | You learn as long as you drill; research synthesis from the Longyearbyen CO2 Laboratory, Svalbard, Norway |
title_sort | you learn as long as you drill; research synthesis from the longyearbyen co2 laboratory, svalbard, norway |
topic | VDP::Mathematics and natural science: 400::Geosciences: 450 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 |
topic_facet | VDP::Mathematics and natural science: 400::Geosciences: 450 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 |
url | https://hdl.handle.net/10037/17559 https://doi.org/10.17850/njg008 |