Base of negative bouyancy zone for 96% C02. Extended 200M in the FISU Area, Celtic Sea.
Base of negative bouyancy zone for 96% C02. Extended 200M in the FISU Area, Celtic Sea. The FISU area is defined by the joint submission made by by Spain, Ireland and the United Kingdom of Great Britain and Northern Ireland (FISU) to the Commission on the Limits of the Continental Shelf (Article 76) References: Burnol, A. (2018). Roles of Gas Hydrates for CO2 Geological Storage Purposes. Gas Hydrates 2, 267-284. doi:https://doi.org/10.1002/9781119451174.ch13 Burnol, A., Thinon, I., Ruffine, L., & Herri, J. M. (2015). Influence of impurities (nitrogen and methane) on the CO2 storage capacity as sediment-hosted gas hydrates – Application in the area of the Celtic Sea and the Bay of Biscay. International Journal of Greenhouse Gas Control, 35, 96-109. doi:https://doi.org/10.1016/j.ijggc.2015.01.018
dataset
https://www.europe-geology.eu/b-nbz-co2-96-ext-200m-celticsea-fisu
English
Geoscientific information
-21.091,
40.179,
2.112,
51.179
publication: 2020-10-15
grid
Instituto Geológico y Minero de España – IGME
Ricardo León Buendia
c/ Rios Rosas 23,
Madrid,
28003,
Spain
email:
r.leon@igme.es
Role: custodian
Data Quality
The data source and calculation methods are described here: Burnol, A. (2018). Roles of Gas Hydrates for CO2 Geological Storage Purposes. Gas Hydrates 2, 267-284. doi:https://doi.org/10.1002/9781119451174.ch13 Burnol, A., Thinon, I., Ruffine, L., & Herri, J. M. (2015). Influence of impurities (nitrogen and methane) on the CO2 storage capacity as sediment-hosted gas hydrates – Application in the area of the Celtic Sea and the Bay of Biscay. International Journal of Greenhouse Gas Control, 35, 96-109. doi:https://doi.org/10.1016/j.ijggc.2015.01.018
Minimal Distance:
322 m
Constraints
Metadata about metadata
5f88c237-60e4-432d-ac00-6c190a010833
Geological Survey of Denmark and Greenland (GEUS)
Uffe Larsen
Øster Voldgade 10,
Copenhagen,
1350,
Denmark
email:
ul@geus.dk
Role: point of contact
2021-11-25