CO2 ionic trapping at meta-sedimentary aquifer, following a CO2 injection push-pull test

被引:2
|
作者
Assayag, Nelly [1 ,2 ]
Matter, Juerg [3 ]
Ader, Magali [2 ]
Goldberg, Dave [3 ]
Agrinier, Pierre [2 ]
机构
[1] Univ Cambridge, Dept Earth Sci, Downing St, Cambridge CB2 3EZ, England
[2] Res Ctr Co2 Geol Storage total Schlumberger IPG P, F-75252 Paris, France
[3] Columbia Univ, Lamont Doherty Geol Observ, Palisades, NY 10964 USA
来源
关键词
Stable isotopes; dissolved inorganic carbon; CO2-water rock interactions;
D O I
10.1016/j.egypro.2009.01.306
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
In order to study CO2-water-rock reactions relative to effectiveness of CO2 geological storage, small-scale CO2 injection experiments were performed, as single well push-pull tests, at the Lamont Doherty Earth Observatory test well site (New-York, USA). The injection interval was located at the contact zone between the chilled dolerite and the underlying metamorphosed sedimentary rocks. The variations of post-injection chemical and isotopic characteristics of retrieved water samples (major ions, DIC, delta C-13(DIC)) underline the CO2 reactivity in the aquifer and allow to identify reactions of the dissolved CO2 with the surrounding rocks, mainly the dissolution of carbonate minerals and complementary cation exchange. (C) 2008 Elsevier Ltd. All rights reserved
引用
收藏
页码:2357 / 2360
页数:4
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