氢抑制条件下的有机质热演化动力学模型——以三塘湖盆地芦草沟组为例

张磊; 孟元林; 崔存萧; 李新宁; 陶士振; 吴晨亮; 胡安文; 许丞

doi:10.11743/ogg20170504

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氢抑制条件下的有机质热演化动力学模型——以三塘湖盆地芦草沟组为例
A new kinetic model of organic thermal evolution under the condition of hydrogen suppression:A case study from the Lucaogou Formation in the Santanghu Basin
2017年38卷第5期页码：862-868
网络首发：2017-10-28，

纸质出版：2017
DOI： 10.11743/ogg20170504
稿件说明：

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张磊, 孟元林, 崔存萧, 等. 氢抑制条件下的有机质热演化动力学模型——以三塘湖盆地芦草沟组为例[J]. 石油与天然气地质, 2017,38(5):862-868. DOI： 10.11743/ogg20170504.

Zhang Lei, Meng Yuanlin, Cui Cunxiao, et al. A new kinetic model of organic thermal evolution under the condition of hydrogen suppression:A case study from the Lucaogou Formation in the Santanghu Basin[J]. 2017, 38(5): 862-868. DOI： 10.11743/ogg20170504.

摘要

三塘湖盆地马朗凹陷芦草沟组烃源岩含有较多的富氢组分，有机质的热演化受到氢抑制。为了模拟氢抑制背景下的有机质热演化史，在经典的Sweeny和Burham Easy%R

时-温双控化学动力学模型基础上，本文考虑氢抑制对有机质热演化的影响，根据氢指数调节反应活化能，建立了描述有机质热演化的时-温-氢抑制多控化学动力学模型。研究结果表明，芦草沟组氢抑制对R

的贡献值为0.2%左右；由于氢抑制的影响，芦草沟组烃源岩进入生烃门限和开始大量生烃的时间均被延迟。文中新建立的化学动力学模型可以应用于各种类型干酪根的有机质热演化史模拟，其精度更高、应用范围更广。

Abstract

Organic matters of the source rocks in the Lucaogou Formation of the Malang Sag

Santanghu Basin are rich in hydrogen components

which suppresses the thermal evolution of organic matters.To simulate thermal evolution of organic matters

a new kinetic model of organic thermal evolution under the condition of hydrogen suppression was established integrating time

temperature

and hydrogen retardation based on Sweeny and Burham Easy %R

time and temperature controlling kinetic model.In the new kinetic model

activity energies are adjusted by hydrogen index.The results show that hydrogen suppression contributes to 0.2% of R

value in the Lucaogou Formation.Hydrogen suppression also resulted in delays of both initial generation of hydrocarbons and peak generation of hydrocarbons.This new established model is widely applicable to thermal histories for different kerogen types with higher accuracy.