World Journal of Environmental Engineering
ISSN (Print): 2372-3076 ISSN (Online): 2372-3084 Website: https://www.sciepub.com/journal/wjee Editor-in-chief: Apply for this position
Open Access
Journal Browser
Go
World Journal of Environmental Engineering. 2015, 3(2), 23-31
DOI: 10.12691/wjee-3-2-1
Open AccessArticle

Identification of Potential Vertical Gas Migration Pathways above Gas Storage Reservoirs

Eric W. Peterson1, , Lauren I. Martin2 and Dave H. Malone1

1Department of Geography-Geology, Illinois State University, Normal, IL, USA

2CH2M Hill, Chicago, IL USA

Pub. Date: April 28, 2015

Cite this paper:
Eric W. Peterson, Lauren I. Martin and Dave H. Malone. Identification of Potential Vertical Gas Migration Pathways above Gas Storage Reservoirs. World Journal of Environmental Engineering. 2015; 3(2):23-31. doi: 10.12691/wjee-3-2-1

Abstract

Natural gas is stored underground in geologic structures throughout the United States. However, complexities associated with these geologic structures may provide vertical pathways for gas migration, and thus gas loss. Possible upward migration (loss) of natural gas in an underground gas storage field in stimulated this investigation that aims to identify potential migration pathways. Spatial analysis of volume of shale (Vsh) and formation porosity (n) values were conducted in conjunction with high-resolution shallow seismic surveys to identify potential vertical pathways. Surficial gas accumulations within glacial deposits were confirmed by the seismic surveys. These gas pockets accumulated by migration along steeply inclined structural discontinuities, most likely faults and fracture zones within the underlying shallow bedrock units. With the seismic technique limited to a depth of 100 m, Vsh data were used to assess the reservoir’s seal rocks ability to limit vertical gas migration. The Vsh data indicate that the seal rocks are best classified as heterogeneous siltstones. Spatial analysis highlights an aligned pattern of low Vsh values in both the reservoir rocks and the seal rocks. The low Vsh values lie beneath the faults and fracture zones and the documented surficial gas deposit. Higher n values for the sandstones in the reservoir area as opposed to other areas suggest porosity enhancement associated with deformation. Structural deformation, faults and fracture zones, appears to provide a pathway for vertical gas migration. However, stratigraphic (lateral) heterogeneities associated with the reservoir and seal rocks may provide additional vertical pathways.

Keywords:
volume of shale calculations seismic survey structural deformation illinois basin porosity

Creative CommonsThis work is licensed under a Creative Commons Attribution 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

Figures

Figure of 5

References:

[1]  Energy Information Administration (EIA). “The basics of underground natural gas storage.” 2004. [Online]. Available: http://www.eia.doe.gov/pub/oil_gas/natural_gas/analysis_publications/storagebasics/storagebasics.html. [Accessed March 14, 2015].
 
[2]  Energy Information Administration (EIA). “U.S. natural gas summary.” 2006. [Online]. Available: http://tonto.eia.doe.gov/dnav/ng/ng_sum_lsum_dcu_nus_m.htm. [Accessed November 30, 2014].
 
[3]  Nissen, S.E., Watney, W.L., and Xia, J., “High-Resolution seismic detection of shallow natural gas beneath Hutchinson, Kansas,” Environmental Geosciences, 11(3), 129-142. 2004.
 
[4]  Blondin, E. and Mari, J.L., “Detection of Gas Bubble Boundary Movement,” Geophysical Prospecting, 34, 73-93. 1986.
 
[5]  Pugin, A.J.M., Sargent, S.L., and Hunt, L.I. “SH and P-wave seismic reflection using landstreamers to map shallow features and porosity characteristics in Illinois,” in SAGEEP 2006 Meeting, Environmental and Engineering Geophysical Society.
 
[6]  Buschbach, T.C. and Bond, D.C., Underground storage of natural gas in Illinois-1973. Illinois State Geological Survey, Champaign, IL, 1974.
 
[7]  Willman, H.B. and Kolata, D.R., The Platteville and Galena groups in northern Illinois. Illinois State Geological Survey, Champaign, IL, 1978.
 
[8]  Hansel, A.K. and Johnson, W.H., Wedron and Mason groups: lithostratigraphic reclassification of deposits of the Wisconsin Episode, Lake Michigan Lobe area Illinois State Geological Survey, Champaign, IL, 1996.
 
[9]  Nelson, W.J., Structural features in Illinois. Illinois State Geological Survey, 1995.
 
[10]  Nelson, R.S., Kirchner, J.G., and Searight, T.K. “The LaSalle anticline and its influence on Pennsylvanian sedimentation in the LaSalle-Peru area,” in 52nd Tri-State Geological Field Conference, 49.
 
[11]  Fertl, W.H. and Chilingarian, G.V., “Type and distribution modes of clay minerals from well logging data,” Journal of Petroleum Science and Engineering, 3, 321-332. 1990.
 
[12]  Dresser Atlas, Well logging and interpretation techniques: the course for home study. Dresser Atlas, 1982.
 
[13]  Pugin, A.J.M., Larson, T.H., Sargent, S.L., McBride, J.H., and Bexfield, C.E., “Near-surface mapping using SH-wave and P-wave seismic landstreamer data acquisition in Illinois, U.S.,” The Leading Edge, 23(7), 677-682. 2004.