A GEOCHEMICAL PERSPECTIVE OF NATURAL-GAS AND ATMOSPHERIC METHANE

被引:155
作者
WHITICAR, MJ
机构
[1] Bundesanstalt für Geowissenschaften und Rohstoffe, 3000 Hannover 51
关键词
NATURAL GAS; CARBON ISOTOPE; HYDROGEN ISOTOPE; ATMOSPHERIC METHANE; FLUX; MASS BALANCE; GLOBAL WARMING;
D O I
10.1016/0146-6380(90)90068-B
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
Natural gases are key components in the description of the global carbon cycle. Although the estimated 120 Gt C reserves of natural gas are minute compared to the total carbon reservoir (c. 1.4 x 10(8) Gt C), the variations in composition and distribution can provide information on the magnitude of carbon fluxes between specific geo-, hydro- and atmospheric reservoirs. Natural gases, and in particular methane, influence not only our economies, but our atmosphere and ultimately our climate as well. Volatile hydrocarbons also represent, in certain environments, a significant carbon nutrient source for specialized organisms. The magnitudes of natural gas reservoirs and fluxes are put into perspective. On a global basis, natural gas supplies c. 20% of man's primary, external energy needs; following the consumption of oil an coal (38 and 30%, respectively). Currently, worldwide production of natural gas amasses 1.8 x 10(12) m3 y-1 or c. 2% y-1 of the proven geogas reserves (estimated total geogas reserves > 200 x 10(12) m3). Geochemical exploration for hydrocarbons relies heavily on the characterization of natural gases. As the volatile hydrocarbon phase, natural gases have physical and chemical properties which assist in their detection and application. They migrate readily, and are widely distributed in the sediment column. In addition, the significant range in molecular and isotope composition of natural gases provides interpretative information on the gases (e.g. conventional bacterial/diagenetic, thermogenic, geothermal or unconventional "deep gas") and on the maturity/type of the precursors source material from which they are derived. Reliable interpretation of natural gas data requires that secondary effects (e.g. migration, mixing, oxidation) can be identified. Artifacts, such as hydrocarbons generated during drilling or analysis, and sampling contamination/alteration must also be considered. These various aspects are reviewed. Occasionally, anomalous natural gas data lead us to the recognition of new gas types or processes. Some recent geochemical enigmas are presented for both the adventurous and skeptics.
引用
收藏
页码:531 / 547
页数:17
相关论文
共 87 条
[1]   METHANE HYDROGEN GAS SEEPS, ZAMBALES OPHIOLITE, PHILIPPINES - DEEP OR SHALLOW ORIGIN [J].
ABRAJANO, TA ;
STURCHIO, NC ;
BOHLKE, JK ;
LYON, GL ;
POREDA, RJ ;
STEVENS, CM .
CHEMICAL GEOLOGY, 1988, 71 (1-3) :211-222
[2]   CARBON AND HYDROGEN ISOTOPE FRACTIONATION RESULTING FROM ANAEROBIC METHANE OXIDATION [J].
Alperin, M. ;
Reeburgh, W. ;
Whiticar, M. .
GLOBAL BIOGEOCHEMICAL CYCLES, 1988, 2 (03) :279-288
[3]   LIGHT-HYDROCARBONS IN RECENT TEXAS CONTINENTAL-SHELF AND SLOPE SEDIMENTS [J].
BERNARD, BB ;
BROOKS, JM ;
SACKETT, WM .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1978, 83 (NC8) :4053-4061
[4]   MATURITY RELATED MIXING MODEL FOR METHANE, ETHANE AND PROPANE, BASED ON CARBON ISOTOPES [J].
BERNER, U ;
FABER, E .
ORGANIC GEOCHEMISTRY, 1988, 13 (1-3) :67-72
[5]   CONTINUING WORLDWIDE INCREASE IN TROPOSPHERIC METHANE, 1978 TO 1987 [J].
BLAKE, DR ;
ROWLAND, FS .
SCIENCE, 1988, 239 (4844) :1129-1131
[6]  
BOIGK H, 1976, ERDOL KOHLE ERDGAS P, V29, P103
[7]   NONMETHANE HYDROCARBONS IN AN OCEANIC ATMOSPHERE [J].
BONSANG, B ;
LAMBERT, G .
JOURNAL OF ATMOSPHERIC CHEMISTRY, 1985, 2 (03) :257-271
[8]  
CASTLE JE, 1988, P EUROCORR BRIGHTON, P15
[9]   BIOGEOCHEMICAL ASPECTS OF ATMOSPHERIC METHANE [J].
Cicerone, R. ;
Oremland, R. .
GLOBAL BIOGEOCHEMICAL CYCLES, 1988, 2 (04) :299-327
[10]  
Claypool G. E., 1974, NATURAL GASES MARINE, P99, DOI DOI 10.1007/978-1-4684-2757-8_8