The Type of Mixed Gases and Their Identification
-
摘要: 通过对天然气独特的物理、化学特征研究,探讨了不同成因来源天然气混合的机理和条件,将天然气混合划分为有机来源与无机来源的混合、有机质不同母质形成天然气的混合和不同成熟阶段有机成因气混合等三大类型。通过具体实例解剖研究了天然气混合的判识,初步建立了不同成因类型天然气的混合的模式。Abstract: The mixing of gases is ubiquitous in nature because of their special physical property. The mixed gas is formed by mixing of different genetic types of natural gases,and reflected obviously the gas geochemical features. If define one origin type of natural gas as one end member, the mixed gases would be divided into two. three and multiple end members. The common and significant type of mixed gas is of two end members which consists of three large groups: (a)mixing of gas with inorganic and organic origins ;(b)mixing of organic origin gases with different source type; (c)mixing of gases with different evloution stags; Gas migration, especially second migration that caused by diffusion and infiltration, is the main way which make the mixing of different types of gases. The first condition for mixing of natural gases is the existence of gas sources of different types and evolution stages. The chemical composition,stable isotopic composition of carbon and hydrogen and the noble gas isotopic composition are the main markers to differentiate mixed gases. Isotopic composition of the noble gas is an important tool to differentiate the mixed natural gases with crust and mantle sources,while the stable isotopes are to differentiate the mixed natural gases with different genetic types and evlution stages. It should be pointed out that it could effectively differentiate mixed gases by comobining geologic backgrounds and various geo-chemical parameters. By study the mechannism and conditions of mixed gases formation and analyse some examples,the mixing model of two -member gases was established.
-
[1] 朱家蔚.徐永昌等.1984,东濮凹陷天然氛同位素特征及谋成气判识.科学通报.1期,41-94页. [2] 沈平等.1987,气态烃同位素组成特征及煤型气判识.中国科学(B辑).3期.647-657页. [3] 杜建国、涂永昌.1988,三水盆地天然气地球化学特征及其成因.中国科学院兰州地质研究所生物、气体地球化学开放研究实验室研究年报(1987).甘肃科学技术出版社,150-166页. [4] 徐永昌.1976.稀有气体及其同位索在石油地质学上的应用,石油地质学译文集(第三集),科学出版社,299-308页。 [5] 徐水昌等.1990.我国非烃及稀有气体地球化学,中国科学((B辑).6期. 645-651页。 [6] 唐忠驭.1983,天然气,二氧化碳气藏的地质特征及其利用,天然气工业,3卷.3期. [7] 陶庆才,陈文正,1989.四川盆地夭然气成因类型判别与气探探讨.天然气工业.2期,1-6页。 [8] 黄籍中.1991.油气区天然气成因分类及其在四川盆地的应用。天然气地球化学.1期.6-15页. [9] 廖永胜,1981,应用碳同位素控讨油、气成因,石油学报,增刊. 52-60页。 [10] 戴金星.1990.我国有机烷经气的氢同位索若干特征,石油勘控与开发,5期.27-32页。 [11] 坂田将等.1986.深部火山岩中的天然气成因的地球化学考察.石油技术协会志.51卷.3号.228-237页. [12] James A. T.,1983,Correlation of natural gas by use of carbon isotopic distribution between hydrocarbon components.AAPG Bulletin,V. 67,p. 1176-1191. [13] Lwoton J. E.,1983, Terrestrial inert ga.es:lsutopic trace studies and clues、pnmrdiul components|Anual Reniew Earth plant scienme. V o1. 11, p. 371-414. [14] Schioll M, 1980.The hydrogen and carbon isotope composition of methane from nutural gases of various orgins.Geoch et Cosmoch Acta.V.44.N.5.p.649-149. [15] Stahl W. J.、 1977.Carbon and nitrogen isotopes in hydrocarbon research and expforation.Chem.Geol.V.20. p. 121-149.
计量
- 文章访问数: 439
- HTML全文浏览量: 2
- PDF下载量: 486
- 被引次数: 0