Utility of natural and artificial geochemical tracers for leakage monitoring and quantification during an offshore controlled CO2 release experiment

Flohr, Anita ORCID: https://orcid.org/0000-0002-5018-5379; Matter, Juerg M.; James, Rachael H.; Saw, Kevin; Brown, Robin; Gros, Jonas; Flude, Stephanie; Day, Christopher; Peel, Kate; Connelly, Douglas; Pearce, Christopher R. ORCID: https://orcid.org/0000-0002-4382-2341; Strong, James A. ORCID: https://orcid.org/0000-0001-8603-097X; Lichtschlag, Anna ORCID: https://orcid.org/0000-0001-8281-2165; Hillegonds, Darren J.; Ballentine, Christopher J.; Tyne, Rebecca L.. 2021 Utility of natural and artificial geochemical tracers for leakage monitoring and quantification during an offshore controlled CO2 release experiment. International Journal of Greenhouse Gas Control, 111, 103421. 10.1016/j.ijggc.2021.103421

Before downloading, please read NORA policies.

[thumbnail of 1-s2.0-S1750583621001730-main.pdf]

Preview

Text
1-s2.0-S1750583621001730-main.pdf - Published Version
Available under License Creative Commons Attribution Non-commercial No Derivatives 4.0.
Download (5MB) | Preview

Official URL: http://dx.doi.org/10.1016/j.ijggc.2021.103421

Abstract/Summary

To inform cost-effective monitoring of offshore geological storage of carbon dioxide (CO2), a unique field experiment, designed to simulate leakage of CO2 from a sub-seafloor storage reservoir, was carried out in the central North Sea. A total of 675 kg of CO2 were released into the shallow sediments (∼3 m below seafloor) for 11 days at flow rates between 6 and 143 kg d-1. A set of natural, inherent tracers (13C, 18O) of injected CO2 and added, non-toxic tracer gases (octafluoropropane, sulfur hexafluoride, krypton, methane) were used to test their applicability for CO2 leakage attribution and quantification in the marine environment. All tracers except 18O were capable of attributing the CO2 source. Tracer analyses indicate that CO2 dissolution in sediment pore waters ranged from 35 % at the lowest injection rate to 41% at the highest injection rate. Direct measurements of gas released from the sediment into the water column suggest that 22 % to 48 % of the injected CO2 exited the seafloor at, respectively, the lowest and the highest injection rate. The remainder of injected CO2 accumulated in gas pockets in the sediment. The methodologies can be used to rapidly confirm the source of leaking CO2 once seabed samples are retrieved.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1016/j.ijggc.2021.103421
ISSN:	17505836
Date made live:	14 Oct 2021 15:42 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/531244

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1016/j.ijggc.2021.103421

ISSN:

17505836

Date made live:

14 Oct 2021 15:42 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/531244