Clay/CO2 interactions in the context of geological storage of carbon dioxide

Andreas Busch; Pieter Bertier; Yves Gensterblum; Paul Giesting; Stephen Guggenheim; August F. Koster Van Groos; Philipp Weniger

doi:10.3997/2214-4609.20143935

Clay/CO2 interactions in the context of geological storage of carbon dioxide

Andreas Busch, Pieter Bertier, Yves Gensterblum, Paul Giesting, Stephen Guggenheim, August F. Koster Van Groos, Philipp Weniger

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution

1 Citation (Scopus)

Abstract

A major concern when storing CO2 in geological formations is the sealing efficiency of lowpermeable sequences overlying potential storage reservoirs. The long-term integrity of these sealing layers (caprocks) is a prerequisite to maintain CO2 in place and avoid dissipative loss to the atmosphere. Such leakage will occur either by capillary leakage, via diffusion or through existing or induced faults and fractures The assessment of leakage risks and leakage rates, considering different potential mechanisms, is therefore an important issue for site approval and public acceptance.

Original language	English
Title of host publication	3rd EAGE Shale Workshop: Shale Physics and Shale Chemistry
Publisher	EAGE Publishing BV
DOIs	https://doi.org/10.3997/2214-4609.20143935
Publication status	Published - 23 Jan 2012
Event	3rd EAGE Shale Workshop: Shale Physics and Shale Chemistry - Barcelona, Spain Duration: 23 Jan 2012 → 25 Jan 2012

Conference

Conference	3rd EAGE Shale Workshop: Shale Physics and Shale Chemistry
Country/Territory	Spain
City	Barcelona
Period	23/01/12 → 25/01/12

ASJC Scopus subject areas

Geophysics

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10.3997/2214-4609.20143935

Cite this

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title = "Clay/CO2 interactions in the context of geological storage of carbon dioxide",

abstract = "A major concern when storing CO2 in geological formations is the sealing efficiency of lowpermeable sequences overlying potential storage reservoirs. The long-term integrity of these sealing layers (caprocks) is a prerequisite to maintain CO2 in place and avoid dissipative loss to the atmosphere. Such leakage will occur either by capillary leakage, via diffusion or through existing or induced faults and fractures The assessment of leakage risks and leakage rates, considering different potential mechanisms, is therefore an important issue for site approval and public acceptance.",

author = "Andreas Busch and Pieter Bertier and Yves Gensterblum and Paul Giesting and Stephen Guggenheim and {Koster Van Groos}, {August F.} and Philipp Weniger",

year = "2012",

month = jan,

day = "23",

doi = "10.3997/2214-4609.20143935",

language = "English",

booktitle = "3rd EAGE Shale Workshop: Shale Physics and Shale Chemistry",

publisher = "EAGE Publishing BV",

address = "Netherlands",

note = "3rd EAGE Shale Workshop: Shale Physics and Shale Chemistry ; Conference date: 23-01-2012 Through 25-01-2012",

}

Busch, A, Bertier, P, Gensterblum, Y, Giesting, P, Guggenheim, S, Koster Van Groos, AF & Weniger, P 2012, Clay/CO2 interactions in the context of geological storage of carbon dioxide. in 3rd EAGE Shale Workshop: Shale Physics and Shale Chemistry. EAGE Publishing BV, 3rd EAGE Shale Workshop: Shale Physics and Shale Chemistry, Barcelona, Spain, 23/01/12. https://doi.org/10.3997/2214-4609.20143935

TY - GEN

T1 - Clay/CO2 interactions in the context of geological storage of carbon dioxide

AU - Busch, Andreas

AU - Bertier, Pieter

AU - Gensterblum, Yves

AU - Giesting, Paul

AU - Guggenheim, Stephen

AU - Koster Van Groos, August F.

AU - Weniger, Philipp

PY - 2012/1/23

Y1 - 2012/1/23

N2 - A major concern when storing CO2 in geological formations is the sealing efficiency of lowpermeable sequences overlying potential storage reservoirs. The long-term integrity of these sealing layers (caprocks) is a prerequisite to maintain CO2 in place and avoid dissipative loss to the atmosphere. Such leakage will occur either by capillary leakage, via diffusion or through existing or induced faults and fractures The assessment of leakage risks and leakage rates, considering different potential mechanisms, is therefore an important issue for site approval and public acceptance.

AB - A major concern when storing CO2 in geological formations is the sealing efficiency of lowpermeable sequences overlying potential storage reservoirs. The long-term integrity of these sealing layers (caprocks) is a prerequisite to maintain CO2 in place and avoid dissipative loss to the atmosphere. Such leakage will occur either by capillary leakage, via diffusion or through existing or induced faults and fractures The assessment of leakage risks and leakage rates, considering different potential mechanisms, is therefore an important issue for site approval and public acceptance.

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U2 - 10.3997/2214-4609.20143935

DO - 10.3997/2214-4609.20143935

M3 - Conference contribution

AN - SCOPUS:84898450972

BT - 3rd EAGE Shale Workshop: Shale Physics and Shale Chemistry

PB - EAGE Publishing BV

T2 - 3rd EAGE Shale Workshop: Shale Physics and Shale Chemistry

Y2 - 23 January 2012 through 25 January 2012

ER -

Clay/CO2 interactions in the context of geological storage of carbon dioxide

Abstract

Conference

ASJC Scopus subject areas

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