Authors / CoAuthors
Schroder, I.F. | Zhang, H. | Zhang, C. | Feitz, A.J.
Abstract
Following the drilling of a shallow natural CO<sub>2</sub> reservoir at the Qinghai research site, west of Haidong, China, it was discovered that CO<sub>2</sub> was continuously leaking from the wellbore due to well-failure. The site has become a useful research facility in China for studying CO<sub>2</sub> leakage and monitoring technologies for application to geological storage sites of CO<sub>2</sub>. During an eight day period in 2014, soil gas and soil flux surveys were conducted to characterise the distribution, magnitude and likely source of the leaking CO<sub>2</sub> . Two different sampling patterns were utilised during soil flux surveys. A regular sampling grid was used to spatially map out the two high-flux zones which were located 20–50 m away from the wellhead. An irregular sampling grid, with higher sampling density in the high-flux zones, allowed for more accurate mapping of the leak distribution and estimation of total field emission rate using cubic interpolation. The total CO<sub>2</sub> emission rate for the site was estimated at 649-1015 kgCO<sub>2</sub>/d and there appeared to be some degree of spatial correlation between observed CO<sub>2</sub> fluxes and elevated surface H<sub>2</sub>O fluxes. Sixteen soil gas wells were installed across the field to test the real-time application of Romanak et al.’s (2012) process-based approach for soil gas measurements (using ratios of major soil gas components to identify the CO<sub>2</sub> source) using a portable multi-gas analyser. Results clearly identified CO<sub>2</sub> as being derived from one exogenous source, and are consistent with gas samples collected for laboratory analysis. Carbon-13 isotopes in the centre of each leak zone (−0.21‰ and −0.22‰) indicate the underlying CO<sub>2</sub> is likely sourced from the thermal decomposition of marine carbonates. Surface soil mineralisation (predominantly calcite) can be used to infer prior distribution of the CO<sub>2</sub> hotspots and as a consequence highlighted plume migration of 20m in 11 years. The broadening of the affected area beyond the wellbore at the Qinghai research site markedly increases the area that needs surveying at sufficient density to detect a leak. This challenges the role of soil gas and soil flux in a CCS monitoring and verification program for leak detection, suggesting that these techniques may be better applied for characterising the source and emission rate of a CO<sub>2</sub> leak, respectively. <b>Citation:</b> I.F. Schroder, H. Zhang, C. Zhang, A.J. Feitz, The role of soil flux and soil gas monitoring in the characterisation of a CO2 surface leak: A case study in Qinghai, China, International Journal of Greenhouse Gas Control, Volume 54, Part 1, 2016, Pages 84-95, ISSN 1750-5836, https://doi.org/10.1016/j.ijggc.2016.07.030.
Product Type
document
eCat Id
90040
Contact for the resource
Point of contact
Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
Canberra
ACT
2601
Australia
Resource provider
Point of contact
- Contact instructions
- MEG
Keywords
- theme.ANZRC Fields of Research.rdf
-
- EARTH SCIENCES
-
- soil gas
-
- soil flux
-
- surface monitoring
-
- CO2 leak
-
- well failure
-
- China
-
- emissions
-
- gas migration
-
- Published_External
Publication Date
2016-01-01T00:00:00
Creation Date
Security Constraints
Legal Constraints
Status
Purpose
Maintenance Information
asNeeded
Topic Category
climatologyMeteorologyAtmosphere
Series Information
Lineage
This publication was prepared in collaboration between Geoscience Australia and the Chinese Geological Survey under the auspices of the China Australia Geological Storage of CO2 (CAGS) Project
Parent Information
Extents
[-44.00, -9.00, 112.00, 154.00]
Reference System
Spatial Resolution
Service Information
Associations
Source Information
Source data not available.