A reconnaissance study of 13C-13C clumping in ethane from natural gas

被引:30
作者
Clog, Matthieu [1 ,2 ]
Lawson, Michael [3 ]
Peterson, Brian [4 ]
Ferreira, Alexandre A. [5 ]
Santos Neto, Eugenio V. [5 ]
Eiler, John M. [2 ]
机构
[1] SUERC, E Kilbride, Lanark, Scotland
[2] CALTECH, 1200 E Calif Blvd, Pasadena, CA 91125 USA
[3] ExxonMobil Res, Houston, TX USA
[4] ExxonMobil Corp Strateg Res, Annandale, NJ USA
[5] Petrobras SA, Ilha Fundao, PETROBRAS Res & Dev Ctr, Div Geochem,CENPES, Rua Horacio Macedo 950, BR-21941915 Rio De Janeiro, RJ, Brazil
关键词
Clumped isotopes; Ethane; High-resolution mass spectrometry; Natural gas; CARBON-ISOTOPE FRACTIONATION; EAST TEXAS; HYDROGEN; METHANE; SHALE; BASIN; HYDROCARBONS; CALIBRATION; GENERATION; ORIGIN;
D O I
10.1016/j.gca.2017.12.004
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Ethane is the second most abundant alkane in most natural gas reservoirs. Its bulk isotopic compositions (delta C-13 and delta D) are used to understand conditions and progress of cracking reactions that lead to the accumulation of hydrocarbons. Bulk isotopic compositions are dominated by the concentrations of singly-substituted isotopologues ((CH3)-C-13-(CH3)-C-12 for delta C-13 and (CDH2)-C-12-(CH3)-C-12 for delta D). However, multiply-substituted isotopologues can bring additional independent constraints on the origins of natural ethane. The (C2H6)-C-13 isotopologue is particularly interesting as it can potentially inform the distribution of C-13 atoms in the parent biomolecules whose thermal cracking lead to the production of natural gas. This work presents methods to purify ethane from natural gas samples and quantify the abundance of the rare isotopologue (C2H6)-C-13 in ethane at natural abundances to a precision of +/- 0.12% using a high-resolution gas source mass spectrometer. To investigate the natural variability in carbon-carbon clumping, we measured twenty-five samples of thermogenic ethane from a range of geological settings, supported by two hydrous pyrolysis of shales experiments and a dry pyrolysis of ethane experiment. The natural gas samples exhibit a range of 'clumped isotope' signatures (Delta(C2H6)-C-13) at least 30 times larger than our analytical precision, and significantly larger than expected for thermodynamic equilibration of the carbon-carbon bonds during or after formation of ethane, inheritance from the distribution of isotopes in organic molecules or different extents of cracking of the source. However we show a relationship between the Delta(C2H6)-C-13 and the proportion of alkanes in natural gas samples, which we believe can be associated to the extent of secondary ethane cracking. This scenario is consistent with the results of laboratory experiments, where breaking down ethane leaves the residue with a low Delta(C2H6)-C-13 compared to the initial gas. Carbon-carbon clumping is therefore a new potential tracer suitable for the study of kinetic processes associated with natural gas. (C) 2017 Elsevier Ltd. All rights reserved.
引用
收藏
页码:229 / 244
页数:16
相关论文
共 49 条
[1]   CARBON ISOTOPE FRACTIONATION IN FORMATION OF AMINO ACIDS BY PHOTOSYNTHETIC ORGANISMS [J].
ABELSON, PH ;
HOERING, TC .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 1961, 47 (05) :623-&
[2]   Seasonal and diurnal variations of 13C18O16O in air:: Initial observations from Pasadena, CA [J].
Affek, Hagit P. ;
Xu, Xiaomi ;
Eiler, John M. .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2007, 71 (21) :5033-5043
[3]   Abundance of mass 47 CO2 in urban air, car exhaust, and human breath [J].
Affek, HP ;
Eiler, JM .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2006, 70 (01) :1-12
[4]  
[Anonymous], 1994, PETROLEUM SYSTEM SOU
[5]  
[Anonymous], THESIS
[6]   Hydrogen isotope systematics of phase separation in submarine hydrothermal systems: Experimental calibration and theoretical models [J].
Berndt, ME ;
Seal, RR ;
Shanks, WC ;
Seyfried, WE .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1996, 60 (09) :1595-1604
[7]   CALCULATION OF EQUILIBRIUM CONSTANTS FOR ISOTOPIC EXCHANGE REACTIONS [J].
BIGELEISEN, J ;
MAYER, MG .
JOURNAL OF CHEMICAL PHYSICS, 1947, 15 (05) :261-267
[8]   Carbon and hydrogen isotopic reversals in deep basin gas: Evidence for limits to the stability of hydrocarbons [J].
Burruss, R. C. ;
Laughrey, C. D. .
ORGANIC GEOCHEMISTRY, 2010, 41 (12) :1285-1296
[9]   ORIGIN OF GASEOUS HYDROCARBONS IN SUBSURFACE ENVIRONMENTS - THEORETICAL CONSIDERATIONS OF CARBON ISOTOPE DISTRIBUTION [J].
CHUNG, HM ;
GORMLY, JR ;
SQUIRES, RM .
CHEMICAL GEOLOGY, 1988, 71 (1-3) :97-103
[10]   CARBON ISOTOPE FRACTIONATION DURING NATURAL-GAS GENERATION FROM KEROGEN [J].
CLAYTON, C .
MARINE AND PETROLEUM GEOLOGY, 1991, 8 (02) :232-240