Gravitational trapping of carbon dioxide in deep ocean sediments: hydraulic fracturing and mechanical stability

Gravitational trapping of carbon dioxide in deep ocean sediments is attractive both for the long term stability provided by gravity as well as the large volume and hence storage capacity of deep ocean sediments at necessary depths. Unfortunately, most pelagic sediments suffer from extremely low perm...

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Bibliographic Details
Published inEnergy procedia Vol. 1; no. 1; pp. 3647 - 3654
Main Authors Levine, Jonathan S, Matter, Juerg M, Goldberg, Dave, Lackner, Klaus S
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.02.2009
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Summary:Gravitational trapping of carbon dioxide in deep ocean sediments is attractive both for the long term stability provided by gravity as well as the large volume and hence storage capacity of deep ocean sediments at necessary depths. Unfortunately, most pelagic sediments suffer from extremely low permeability and are not expected to have an overlying mechanical seal, making emplacement of CO2 contingent upon large scale hydraulic fracturing and some mechanism of arresting fracture growth before reaching the seafloor. An experimental design is presented with the capability of testing a variety of proposed fracture arrest mechanisms.
ISSN:1876-6102
1876-6102
DOI:10.1016/j.egypro.2009.02.161