An Inverse Method for Estimating Layer Thickness 1 and Volume with Time of a Thin CO 2 -filled Layer at 2 the Sleipner Field, North Sea

Cowton, L. R. and Neufeld, J. A. and White, N. J. and Bickle, M. J. and White, J. C. and Chadwick, R. A. (2016) An Inverse Method for Estimating Layer Thickness 1 and Volume with Time of a Thin CO 2 -filled Layer at 2 the Sleipner Field, North Sea. Journal of Geophysical Research-Solid Earth, 121 (7). pp. 5068-5085. ISSN 0148-0227 DOI 10.1002/2016JB012895

	Text cowton-et-al-2016-revised.pdf - Accepted Version Restricted to Registered users only Download (15MB) | Request a copy
Preview	Text Cowton_et_al-2016-Journal_of_Geophysical_Research__Solid_Earth.sup-1.pdf - Supplemental Material Download (2MB) | Preview
Preview	Text Cowton_et_al-2016-Journal_of_Geophysical_Research__Solid_Earth.pdf - Published Version Available under License Creative Commons Attribution. Download (5MB) | Preview

Abstract

Migration of CO 2 through storage reservoirs can be monitored using time-lapse seismic reflection surveys. At the Sleipner Field, injected CO 2 is distributed throughout nine layers within the reservoir. These layers are too thin to be seismically resolvable by direct measurement of the separation between reflections from the top and bottom of each layer. Here, we develop and apply an inverse method for measuring thickness changes of the shallowest layer. Our approach combines differences in travel time down to a specific reflection together with amplitude measurements to determine layer thicknesses from time-lapse surveys. A series of synthetic forward models were used to test the robustness of our inverse approach and to quantify uncer- tainties. In the absence of ambient noise, this approach can unambiguously resolve layer thickness. If a realistic ambient noise distribution is included, layer thicknesses of 1–6 m are accurately retrieved with an uncertainty of ±0.5 m. We used this approach to generate a thickness map of the shallowest layer. The fidelity of this result was tested using measurements of layer thickness determined from the 2010 broadband seismic survey. The calculated volume of CO 2 within the shallowest layer increases at a rate that is quadratic in time, despite an approximately constant injection rate into the base of the reservoir. This result is consistent with a diminished growth rate of the areal extent of underlying layers. Finally, the relationship between caprock topography and layer thickness is explored and potential migration pathways that charge this layer are identified.

Item Type:	Article
Uncontrolled Keywords:	2016AREP; IA70; weekly list
Subjects:	02 - Geodynamics, Geophysics and Tectonics
Divisions:	02 - Geodynamics, Geophysics and Tectonics 08 - Green Open Access
Journal or Publication Title:	Journal of Geophysical Research-Solid Earth
Volume:	121
Page Range:	pp. 5068-5085
Identification Number:	10.1002/2016JB012895
Depositing User:	Sarah Humbert
Date Deposited:	25 May 2016 16:55
Last Modified:	27 Jan 2017 17:22
URI:	http://eprints.esc.cam.ac.uk/id/eprint/3666

Actions (login required)

View Item