Quantitative assessment of soil CO 2  concentration and stable carbon isotope for leakage detection at geological carbon sequestration sites | Zendy

Yang Changbing | Zendy; Jamison Keith | Zendy; Xue Lianqing | Zendy; Dai Zhenxue | Zendy; Hovorka Susan | Zendy; Fredin Leif | Zendy; Treviño Ramón | Zendy

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Quantitative assessment of soil CO 2 concentration and stable carbon isotope for leakage detection at geological carbon sequestration sites

Author(s) -

Yang Changbing,

Jamison Keith,

Xue Lianqing,

Dai Zhenxue,

Hovorka Susan,

Fredin Leif,

Treviño Ramón

Publication year - 2017

Publication title -

greenhouse gases: science and technology

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 0.45

H-Index - 32

ISSN - 2152-3878

DOI - 10.1002/ghg.1679

Subject(s) - carbon sequestration , leakage (economics) , isotopes of carbon , dissolution , soil science , environmental science , soil water , soil carbon , environmental chemistry , carbon dioxide , chemistry , total organic carbon , organic chemistry , economics , macroeconomics

This study presents a quantitative method to evaluate CO 2 concentration ([CO 2 ]) and stable carbon isotope ratio (δ 13 C) as indicators for leakage detection at a geological carbon sequestration site by combining use of field release tests and a numerical modeling approach. A numerical model was developed to simulate CO 2 dynamics by considering diffusion, dissolution in soil water, and soil respiration. The numerical model fits the background dynamics of [CO 2 ] (360 to 550 ppm) and δ 13 C (‐16‰ to ‐6‰) well and reproduces fairly the overall trend observed during the CO 2 release test. The model was further applied to assess detection probability (DP) of [CO 2 ] and δ 13 C for leakage detection in terms of various factors, such as CO 2 leakage rate, background variations, δ 13 C of the CO 2 leaked, and the threshold value of signal‐to‐noise ratio. Modeling results suggest that δ 13 C may have a higher DP than [CO 2 ]. This study also shows that DP of δ 13 C for the IEA Weyburn project is close to 0, implying δ 13 C is inappropriate to be an indicator for CO 2 leakage at the site. The quantitative method developed can also be used to design a monitoring plan or strategy in a near‐surface environment for geological carbon sequestration. © 2017 Society of Chemical Industry and John Wiley & Sons, Ltd.

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