加水热模拟中深湖与煤系泥岩地化特征比较

梁春秀; 魏志平; 毛超林; 李本才

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

加水热模拟中深湖与煤系泥岩地化特征比较

梁春秀, 魏志平, 毛超林, 李本才

文章导航 > 沉积学报 > 2002 > 20(1): 165-168

梁春秀, 魏志平, 毛超林, 李本才. 加水热模拟中深湖与煤系泥岩地化特征比较[J]. 沉积学报, 2002, 20(1): 165-168.

引用本文:

梁春秀, 魏志平, 毛超林, 李本才. 加水热模拟中深湖与煤系泥岩地化特征比较[J]. 沉积学报, 2002, 20(1): 165-168.

LIANG Chun-xiu, WEI Zhi-ping, MAO Chao-lin, LI Ben-cai. Comparison of Geochemistry Character between Mudstones from Deep Lacustrine Facies and Coal Measures by Hydrous Pyrolysis[J]. Acta Sedimentologica Sinica, 2002, 20(1): 165-168.

Citation:

梁春秀, 魏志平, 毛超林, 李本才. 加水热模拟中深湖与煤系泥岩地化特征比较[J]. 沉积学报, 2002, 20(1): 165-168.

引用本文:

梁春秀, 魏志平, 毛超林, 李本才. 加水热模拟中深湖与煤系泥岩地化特征比较[J]. 沉积学报, 2002, 20(1): 165-168.

Citation:

加水热模拟中深湖与煤系泥岩地化特征比较

1 成都理工学院,成都,610059;
2 吉林石油勘探开发研究院,吉林松原,138001

详细信息

作者简介:
梁春秀男 1959年出生高级工程师石油地质

中图分类号: P593

计量

文章访问数: 394
HTML全文浏览量: 1
PDF下载量: 273
被引次数: 0

Comparison of Geochemistry Character between Mudstones from Deep Lacustrine Facies and Coal Measures by Hydrous Pyrolysis

1 Chengdu Science and Engeneering University,Chengdu 610059;
2 Jilin Petroleum Exploration and Development Institute, SongYuan, Jilin 138001

摘要

摘要: 通过深湖泥岩和煤系泥岩的加水热模拟研究认为,在热模拟实验过程中,深湖泥岩和煤系泥岩显示不同特征,并且其演化有差别。深湖泥岩利于液态原油的生成,并且转化率高于煤系泥岩。深湖泥岩残余可溶有机质饱和烃含量高于煤系泥岩,非烃含量则低于煤系泥岩。深湖泥岩胶质 /沥青质和饱芳比均随温度升高而降低,而煤系泥岩的胶质 /沥青质随温度升高有增加趋势,其饱芳比的变化则不大或有降低趋势。深湖泥岩的T_max难以指示演化阶段,其干酪根碳同位素值明显轻于煤系泥岩,它们的值均随温度的升高而变重。
- 加水热模拟 /
- 泥岩 /
- 可溶有机质 /
- 成熟度
Abstract: The geochemistry characters are discussed which between mudstones from deep lacustrine facies and coal measured by hydrous pyrolysis.Lots of differences of the two samples are pointed out by analysis.The mudstones from deep lacustrine facies and coal measure show difficult evolution features by hydrous pyrolysis. The mudstone from deep lacustrine facies has high hydrocarbon yield and is more profitable to liquid oil generation,so it will mainly generate liquid oil in the course of thermal evolution.The saturated hydrocarbon content is more and the nonhydrocarbon content is lower in the residual dissoluble organic matter in the mudstone from deep lacustrine facies than that in coal measures.The ratio of resin to asphalten and the ratio of saturated hydrocarbon to aromatics increase when the temperature rises in the mudstone from deep lacustrine facies.The ratio of resin to asphalten increases and the ratio of saturated hydrocarbon to aromatics varies little or decreases a little when the temperature rises in the mudstone from coal messures. T _max of the pyrolyzed(Rock-Eval) mudstones from deep lacustrine facies can not indicate evolution stage,but T _max of the pyrolyzed(Rock-Eval) mudstones from the mudstone from coal measures increases as the temperature rises.The carbon isotope of kerogen from the mudstone from deep lacustrine facies is lower distinctly than that of kerogen from mudstone of coal measures. The carbon isotope of kerogen from two samples becomes heavy as the temperature rises.It is obvious that the T _max of the mudstone from deep lacustrine facies should be considered carefully when it is used to rekon the maturity of organic matter,and that the variation of isotope carbon of kerogen should also be thought much when it is used to research the type of organic matter.
- hydroupyrolysis /
- mudstone /
- dissoluble organic matter /
- maturity

HTML全文

参考文献(8)

[1]	高岗,郝石生,柳广弟等.碳酸盐岩油气生成模拟方法[M].北京:石油工业出版社,2000
[2]	张文正,关德师著.液态烃分子系列碳同位素地球化学[M].北京:石油工业出版社,1997
[3]	高岗.富硫泥灰岩油气生成模拟研究[J].石油大学学报,2000,24(1):34～37
[4]	王新洲,宋一淘,王学军.石油成因与排油物理模拟-方法、机理即应用[M].山东东营:石油大学出版社,1996
[5]	Lewan M D.,Winters A,Williams J.Generation of oil-like pyrolyzates from organic-rich mudstones[J].Science,1979,203:897～899
[6]	Rowland S J.Hydrous pyrolysis of sediments composition and proportions of aromatic hydrocarbons in pyrolysates[J].Advances in Organic Geochemistry,1985,10:1 033～1 040
[7]	石卫,郭绍辉,秦匡宗.烃源岩在水介质下热压模拟的初步研究[A].第五届全国有机地球化学会议论文集[C].南京:江苏科学出版社,1994.381～386
[8]	夏新宇,张文正.热压模拟实验的动力学研究及意义[J].石油勘探与开发,2000,27(5):22～26

[1]	董济凯, 董春梅, 林承焰, 赵子茹. 湖相富有机质泥岩纹层组合类型及其储集意义——以济阳坳陷沙河街组泥页岩为例 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2023.131
[2]	朱志立, 李美俊, 李佳阳, 祁灵, 刘晓强, 韩秋雅, 路清华, 马媛媛, 冷筠滢. 沉积有机质中苯基菲成熟度参数及其化学机理 . 沉积学报, 2023, 41(2): 601-609. doi: 10.14027/j.issn.1000-0550.2021.107
[3]	杨江海, 王圆, 刘佳, 马睿, 杜远生, 刘超, 余文超. 南华北早二叠世泥岩沉积与深时陆地古温度重建 . 沉积学报, 2021, 39(3): 540-549. doi: 10.14027/j.issn.1000-0550.2020.092
[4]	. 吉木萨尔凹陷芦草沟组泥质岩类生烃潜力差异性分析 . 沉积学报, 2014, 32(2): 385-394.
[5]	. 成熟度对陆相烃源岩可溶有机质Pr/Ph比值的影响 . 沉积学报, 2014, 32(1): 182-188.
[6]	郑朝阳. 塔河油田奥陶系原油有机地球化学特征及其油藏成因 . 沉积学报, 2011, 29(3): 605-612.
[7]	陈祖林. 煤和泥岩不同温度条件下非烃中咔唑类化合物的演化特征 . 沉积学报, 2011, 29(3): 587-592.
[8]	陈致林. 利用双金刚烷指标研究济阳坳陷凝析油的成熟度和类型 . 沉积学报, 2008, 26(4): 705-708.
[9]	赵东升. 柴达木盆地西部地区古、新近系油源成熟度 . 沉积学报, 2007, 25(2): 319-324.
[10]	张沛, 郑建平, 张瑞生, 余淳梅. 塔里木盆地塔北隆起奥陶系——侏罗系泥岩稀土元素地球化学特征 . 沉积学报, 2005, 23(4): 740-746.
[11]	苗建宇, 祝总祺, 刘文荣, 卢焕勇. 泥岩有机质的赋存状态与油气初次运移的关系 . 沉积学报, 2004, 22(1): 169-175.
[12]	傅宁, 李友川. 估算天然气成熟度的新指标——金刚烷指标 . 沉积学报, 2001, 19(1): 145-149.
[13]	王万春, 徐永昌, Manfred Schidlowski, Eckhard Faber, Wolfgang Stahl. 不同沉积环境及成熟度干酪根的碳氢同位素地球化学特征 . 沉积学报, 1997, 15(S1): 132-137.
[14]	周士涛, 万光权, 刘永康. 碳酸盐岩有机质成熟度离子探针的判别 . 沉积学报, 1997, 15(2): 31-34.
[15]	沈忠民, 周光甲, 洪志华. 低成熟石油烃源岩的动力学研究 . 沉积学报, 1996, 14(3): 22-29.
[16]	段毅, 徐雁前, 马兰花, 申秀荣. 毕家山铅锌矿床有机地球化学研究（Ⅰ）：可溶有机质特征与矿床若干成因问题探讨 . 沉积学报, 1996, 14(S1): 198-205.
[17]	肖贤明, 吴治君, 刘德汉, 申家贵, 贾蓉芬, 赵林. 早古生代海相烃源岩成熟度的有机岩石学评价方法 . 沉积学报, 1995, 13(2): 112-119.
[18]	张柏生, 刘文汇, 徐永昌, 王兆云, 吴铁生. 辽河盆地过渡带有机地球化学（Ⅰ）──不同赋存状态的有机质与过渡带气的形成 . 沉积学报, 1994, 12(4): 58-65.
[19]	肖贤明, 刘德汉, 傅家谟. 沥青反射率作为烃源岩成熟度指标的意义 . 沉积学报, 1991, 9(S1): 138-146.
[20]	王铮. 干酪根的赋存状态与成熟度的关系 . 沉积学报, 1990, 8(4): 124-129.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 394
HTML全文浏览量: 1
PDF下载量: 273
被引次数: 0

加水热模拟中深湖与煤系泥岩地化特征比较

1 成都理工学院,成都,610059;

2 吉林石油勘探开发研究院,吉林松原,138001

作者简介:
梁春秀男 1959年出生高级工程师石油地质

收稿日期: 2001-02-13

中图分类号: P593

关键词:

加水热模拟 /

泥岩 /

可溶有机质 /

成熟度

摘要: 通过深湖泥岩和煤系泥岩的加水热模拟研究认为,在热模拟实验过程中,深湖泥岩和煤系泥岩显示不同特征,并且其演化有差别。深湖泥岩利于液态原油的生成,并且转化率高于煤系泥岩。深湖泥岩残余可溶有机质饱和烃含量高于煤系泥岩,非烃含量则低于煤系泥岩。深湖泥岩胶质 /沥青质和饱芳比均随温度升高而降低,而煤系泥岩的胶质 /沥青质随温度升高有增加趋势,其饱芳比的变化则不大或有降低趋势。深湖泥岩的T_max难以指示演化阶段,其干酪根碳同位素值明显轻于煤系泥岩,它们的值均随温度的升高而变重。

English Abstract

Comparison of Geochemistry Character between Mudstones from Deep Lacustrine Facies and Coal Measures by Hydrous Pyrolysis

1 Chengdu Science and Engeneering University,Chengdu 610059;

2 Jilin Petroleum Exploration and Development Institute, SongYuan, Jilin 138001

Received Date: 2001-02-13

Keywords:

Abstract: The geochemistry characters are discussed which between mudstones from deep lacustrine facies and coal measured by hydrous pyrolysis.Lots of differences of the two samples are pointed out by analysis.The mudstones from deep lacustrine facies and coal measure show difficult evolution features by hydrous pyrolysis. The mudstone from deep lacustrine facies has high hydrocarbon yield and is more profitable to liquid oil generation,so it will mainly generate liquid oil in the course of thermal evolution.The saturated hydrocarbon content is more and the nonhydrocarbon content is lower in the residual dissoluble organic matter in the mudstone from deep lacustrine facies than that in coal measures.The ratio of resin to asphalten and the ratio of saturated hydrocarbon to aromatics increase when the temperature rises in the mudstone from deep lacustrine facies.The ratio of resin to asphalten increases and the ratio of saturated hydrocarbon to aromatics varies little or decreases a little when the temperature rises in the mudstone from coal messures. T _max of the pyrolyzed(Rock-Eval) mudstones from deep lacustrine facies can not indicate evolution stage,but T _max of the pyrolyzed(Rock-Eval) mudstones from the mudstone from coal measures increases as the temperature rises.The carbon isotope of kerogen from the mudstone from deep lacustrine facies is lower distinctly than that of kerogen from mudstone of coal measures. The carbon isotope of kerogen from two samples becomes heavy as the temperature rises.It is obvious that the T _max of the mudstone from deep lacustrine facies should be considered carefully when it is used to rekon the maturity of organic matter,and that the variation of isotope carbon of kerogen should also be thought much when it is used to research the type of organic matter.

梁春秀, 魏志平, 毛超林, 李本才. 加水热模拟中深湖与煤系泥岩地化特征比较[J]. 沉积学报, 2002, 20(1): 165-168.

引用本文:

梁春秀, 魏志平, 毛超林, 李本才. 加水热模拟中深湖与煤系泥岩地化特征比较[J]. 沉积学报, 2002, 20(1): 165-168.

Citation:

全文HTML

参考文献 (8)

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

x 关闭永久关闭

2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）

留言板

加水热模拟中深湖与煤系泥岩地化特征比较

作者简介:
梁春秀男 1959年出生高级工程师石油地质

计量

Comparison of Geochemistry Character between Mudstones from Deep Lacustrine Facies and Coal Measures by Hydrous Pyrolysis

计量

目录

加水热模拟中深湖与煤系泥岩地化特征比较

1 成都理工学院,成都,610059;

2 吉林石油勘探开发研究院,吉林松原,138001

作者简介:
梁春秀男 1959年出生高级工程师石油地质

English Abstract

Comparison of Geochemistry Character between Mudstones from Deep Lacustrine Facies and Coal Measures by Hydrous Pyrolysis

1 Chengdu Science and Engeneering University,Chengdu 610059;

2 Jilin Petroleum Exploration and Development Institute, SongYuan, Jilin 138001

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

加水热模拟中深湖与煤系泥岩地化特征比较

作者简介: 梁春秀 男 1959年出生 高级工程师 石油地质

计量

出版历程

Comparison of Geochemistry Character between Mudstones from Deep Lacustrine Facies and Coal Measures by Hydrous Pyrolysis

计量

出版历程

目录

加水热模拟中深湖与煤系泥岩地化特征比较

1 成都理工学院,成都,610059; 2 吉林石油勘探开发研究院,吉林松原,138001

作者简介: 梁春秀 男 1959年出生 高级工程师 石油地质

English Abstract

Comparison of Geochemistry Character between Mudstones from Deep Lacustrine Facies and Coal Measures by Hydrous Pyrolysis

1 Chengdu Science and Engeneering University,Chengdu 610059; 2 Jilin Petroleum Exploration and Development Institute, SongYuan, Jilin 138001

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
梁春秀男 1959年出生高级工程师石油地质

1 成都理工学院,成都,610059;

2 吉林石油勘探开发研究院,吉林松原,138001

作者简介:
梁春秀男 1959年出生高级工程师石油地质

1 Chengdu Science and Engeneering University,Chengdu 610059;

2 Jilin Petroleum Exploration and Development Institute, SongYuan, Jilin 138001