西南石油大学学报(自然科学版) ›› 2018, Vol. 40 ›› Issue (4): 61-68.DOI: 10.11885/j.issn.1674-5086.2017.02.21.01

• 地质勘探 • 上一篇    下一篇

三种端元气δ13C1-Ro模型建立与应用

程付启, 朱亚杰, 金强, 洪国郎   

  1. 中国石油大学(华东)地球科学与技术学院, 山东 青岛 266580
  • 收稿日期:2017-02-21 出版日期:2018-08-01 发布日期:2018-08-01
  • 通讯作者: 程付启,E-mail:chengfq9804@163.com
  • 作者简介:程付启,1978年生,男,汉族,河南杞县人,副教授,博士,主要从事石油地质与油气地球化学方面的研究工作。E-mail:chengfq9804@163.com;朱亚杰,1992年生,男,汉族,河南中牟人,硕士研究生,主要从事石油地质与油气地球化学方面的研究工作。E-mail:yjzhu2017@163.com;金强,1956年生,男,汉族,江苏无锡人,教授,博士,博士生导师,主要从事油气地质方面的研究工作。E-mail:jinqiang@upc.edu.cn;洪国郎,1993年生,男,汉族,湖南衡阳人,硕士研究生,主要从事油气成藏方面的研究工作。E-mail:hongguolang@163.com
  • 基金资助:
    国家科技重大专项(2016ZX05006- 007,2016ZX05014 -002);山东省自然科学基金(ZR2014DL004)

Development and Application of Three End-member Gas δ13C1-Ro Models

CHENG Fuqi, ZHU Yajie, JIN Qiang, HONG Guolang   

  1. School of Geosciences, China University of Petroleum, Shandong, Qingdao 266580, China
  • Received:2017-02-21 Online:2018-08-01 Published:2018-08-01

摘要: 端元气δ13C1-Ro模型是天然气成因判识、气源对比及混源气定量判识的重要工具。为了满足Ⅱ型有机质生成天然气识别及评价的需要,根据母质类型将有机热成因天然气划分为I、Ⅱ和Ⅲ型等3种端元气,并利用126组实测天然气数据得到3种端元气的δ13C1-Ro模型。I型,δ13C1=27.55 lg Ro-47.20;Ⅱ型,δ13C1=25.55 lg Ro-40.76;Ⅲ型,δ13C1=48.77 lg Ro-34.10(Ro < 0.9%),δ13C1=22.42 lg Ro-34.80(Ro ≥ 0.9%)。为了方便模型应利用建模样品的δ13C1、δ13C2数据,绘制了三端元气及其混源气的别图版。根据该图版,济阳拗陷坨165、车571与孤东9井天然气分别为I和Ⅱ型端元气混源、Ⅱ型端元气与I型端元气。

关键词: 端元气, δ13C1-Ro模型, 类型判识, 济阳拗陷

Abstract: End-member gas δ13C1-Ro modeling is an important tool for natural gas origin identification, gas-source correlation, and mixed-source gas quantitative processing. In order to identify and evaluate type Ⅱ natural gas generated by organic matter, organic thermogenic gas is broken down into the following three types of end-member gas according to the type of parent material:Type I, Ⅱ, and I. δ13C1 -Ro models for the three types of end-member gas were then developed using 126 endmember gas were then developed using 126 data sets obtained from natural I:δ13C1=27.55 lg Ro -47.2; Type Ⅱ:δ13C1=25.55 lg Ro -40.76; Type Ⅲ:δ13C1=48.77 lg Ro -34.1, if Ro < 0.9%, and δ13C1=22.42 lg Ro -34.8, if Ro > 0.9%. To facilitate application of the models, a chart was generated to identify the δ13C113C2 values of the three end-member gases and their mixtures using δ13C1 and δ13C2 data obtained from the samples for modeling. from the samples for modeling. According to the chart, the natural gases from Jiyang Depression Tuo 165, Che 571, and Gudong 9 wells are mixture of Type I and Ⅱ end-member gas, Type Ⅱ end-member gas, and Type I end-member gas, respectively.

Key words: end-member gas, δ13C1-Ro model, type recognition, Jiyang Depression

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