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_o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Ro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。
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 % Rotime 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 Ro 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.
出处
《石油与天然气地质》
EI
CAS
CSCD
北大核心
2017年第5期862-868,共7页
Oil & Gas Geology
基金
国家自然科学基金项目(41572135)
国家科技重大专项(2016ZX05046-001-006)
东北石油大学研究生创新科研项目(YJSCX2017-004NEPU)
黑龙江省科学基金项目(QC2016049)
黑龙江省普通本科高等学校青年创新人才培养计划项目(UNPYSCT-2016122)
关键词
氢抑制
化学动力学
页岩油
中二叠统
三塘湖盆地
hydrogen suppression, chemical kinetics, shale oil, Middle Permian, Santanghu Basin
