Journal
ORGANIC GEOCHEMISTRY
Volume 42, Issue 7, Pages 781-790Publisher
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.orggeochem.2011.05.005
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Funding
- China National Oil and Gas Project [2008ZX05007-001s]
- PetroChina Science and Technology Development Project [2008A-0600, 2008A-0608, 2009D-5006-01-01]
- Program for Changjiang Scholars and Innovative Research Team in University [IRT0864]
- China National Natural Science Foundation [40973034]
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A suite of natural gases from the northern Songliao Basin in NE China were characterized for their molecular and carbon isotopic composition. Gases from shallow reservoirs display clear geochemical evidence of alteration by biodegradation, with very high dryness (C-1/C2+ > 100), high C-2/C-3 and i-C-4/n-C-4 ratios, high nitrogen content and variable carbon dioxide content. Isotopic values show wide range variations (delta C-13(CH4) from -79.5 parts per thousand to -45.0 parts per thousand, delta C-13(C2H6) from -53.7 parts per thousand to -32.2 parts per thousand, delta C-13(C3H8) from -36.5 parts per thousand to -20.1 parts per thousand, delta C-13(nC4H10) from -32.7 parts per thousand to -24.5 parts per thousand, and delta C-13(CO2) from -21.6 parts per thousand to +10.5 parts per thousand). A variety of genetic types can be recognized on the basis of chemical and isotopic composition together with their geological occurrence. Secondary microbial gas generation was masked by primary microbial gas and the mixing of newly generated methane with thermogenic methane already in place in the reservoir can cause very complicated isotopic signatures. System openness also was considered for shallow biodegraded gas accumulations. Gases from the Daqing Anticline are relatively wet with C-13 enriched methane and C-13 depleted CO2, representing typically thermogenic origin. Gases within the Longhupao-Da'an Terrace have variable dryness, C-13 enriched methane and variable delta C-13 of CO2, suggesting dominant thermogenic origin and minor secondary microbial methane augment. The Puqian-Ao'nan Uplift contains relatively dry gas with C-13 depleted methane and C-13 enriched CO2, typical for secondary microbial gas with a minor part of thermogenic methane. Gas accumulations in the Western Slope are very dry with low carbon dioxide concentrations. Some gases contain C-13 depleted methane, ethane and propane, indicating low maturity/primary microbial origin. Recognition of varying genetic gas types in the Songliao Basin helps explain the observed dominance of gas in the shallow reservoir and could serve as an analogue for other similar shallow gas systems. (C) 2011 Elsevier Ltd. All rights reserved.
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