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滑溜水压裂液与页岩储层化学反应及其对孔隙结构的影响 被引量:3
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作者 孙则朋 王永莉 +4 位作者 吴保祥 卓胜广 魏志福 汪亘 徐亮 《中国科学院大学学报(中英文)》 CSCD 北大核心 2018年第5期712-719,共8页
为探究页岩气井压裂作业过程中,滑溜水压裂液对不同沉积环境(海相、陆相、海陆过渡相)页岩储层孔隙结构的影响,利用盆地深层流体-岩石相互作用模拟仪,模拟地层条件(100℃,50 MPa)下滑溜水压裂液注入过程中与不同沉积环境页岩的相互作用... 为探究页岩气井压裂作业过程中,滑溜水压裂液对不同沉积环境(海相、陆相、海陆过渡相)页岩储层孔隙结构的影响,利用盆地深层流体-岩石相互作用模拟仪,模拟地层条件(100℃,50 MPa)下滑溜水压裂液注入过程中与不同沉积环境页岩的相互作用实验。通过对比反应前与反应72 h后3套页岩样品矿物组成、孔体积和比表面积的变化,对不同类型页岩孔隙结构的变化进行剖析。结果表明,滑溜水压裂液处理后的不同沉积环境页岩矿物组成和孔隙结构都发生了变化。海相页岩反应之后,碳酸盐矿物发生溶蚀,形成大量直径为2~8μm左右的溶蚀孔,导致纳米孔孔体积和比表面积减小。因含有较多的伊/蒙混层矿物,陆相和海陆过渡相页岩遇压裂液容易发生膨胀、分散作用,导致其孔体积及比表面积减小。该实验结果为研究滑溜水压裂液对不同沉积环境页岩储层的物理、化学作用,以及为压裂液的改造提供了一定的科学依据。 展开更多
关键词 不同沉积环境页岩 滑溜水压裂液 高温高压模拟 水岩相互作用
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Serpentinization, abiogenic organic compounds, and deep life 被引量:12
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作者 WANG XianBin OUYANG ZiYuan +3 位作者 zhuo shengguang ZHANG MingFeng ZHENG GuoDong WANG YongLi 《Science China Earth Sciences》 SCIE EI CAS 2014年第5期878-887,共10页
The hydrocarbons and other organic compounds generated through abiogenic or inorganic processes are closely related to two science subjects, i.e., energy resources and life's origin and evolution. "The earth's prim... The hydrocarbons and other organic compounds generated through abiogenic or inorganic processes are closely related to two science subjects, i.e., energy resources and life's origin and evolution. "The earth's primordial abiogenic hydrocarbon theory" and "the serpentinization of abiogenic hydrocarbon theory" are the two mainstream theories in the field of related studies. Ser- pentinizafion generally occurs in slow expanding mid-ocean ridges and continental ophiolites tectonic environment, etc. The abiogenic hydrocarbons and other organic compounds formed through the serpentinization of ultramafic rocks provide energy and raw materials to support chemosynthetic microbial communities, which probably was the most important hydration reac- tion for the origin and early evolution of life. The superposition of biological and abiological processes creates big challenge to the identification of the abiogenic organic materials in serpentinite-hosted ecosystem. Whether abiotic (inorganic) process can form oil and gas resource is a difficult question that has been explored continuously by scientific community for more than a century but has not yet been solved. However, some important progress has been made. The prospecting practice of abiogenic hydrocarbons in commercial gases from the Songliao Basin, China, provides an important example for exploring abiogenic natural gas resources. 展开更多
关键词 ultramafic rocks scrpentinization abiogenic origin organic compound origin of life
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Abiogenic hydrocarbons in commercial gases from the Songliao Basin,China 被引量:6
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作者 WANG XianBin GUO ZhanQian +14 位作者 TUO JinCai GUO HongYan LI ZhenXi zhuo shengguang JIANG HongLiang ZENG LongWei ZHANG MingJie WANG LianSheng LIU ChunXue YAN Hong LI LiWu ZHOU XiaoFeng WANG YongLi YANG Hui WANG Guang 《Science China Earth Sciences》 SCIE EI CAS 2009年第2期213-226,共14页
This paper discusses the kinetic fractionation, composition and distribution characteristics of carbon and hydrogen isotopes for various alkane gases formed in different environments, by different mechanisms and from ... This paper discusses the kinetic fractionation, composition and distribution characteristics of carbon and hydrogen isotopes for various alkane gases formed in different environments, by different mechanisms and from different sources in nature. It is demonstrated that the biodegradation or thermodegradation of complex high-molecule sedimentary organic material can form microbial gas or thermogenic gas. The δ13C1 value ranges from ?110% to ?50% for microbial gases but from ?50% to ?35% (even heavier) for thermogenic gases. Controlled by the kinetic isotope fractionation, both microbial and thermogenic gases have δ13C and δ D values characterized by normal distribution, i.e. δ13C1< δ 13C2< δ 13C3< δ 13C4 and $ \delta D_{CH_4 } < \delta D_{C_2 H_6 } < \delta D_{C_3 H_8 } < \delta D_{C_4 H_{10} } $ , and by a positive correlation between the δ 13C and δ D values. Simple carbon-bearing molecules (CH4, CO and CO2) can form abiogenic alkane gases via polymerization in the abiological chemical process in nature, with δ13C1 heavier than ?30‰ Moreover, controlled by the kinetic isotope fractionation, abiogenic alkane gases are characterized by a reverse distribution of δ 13C values and a normal trend of δ D values, namely δ13C1> δ 13C2> δ 13C3> δ 13C4 and $ \delta D_{CH_4 } < \delta D_{C_2 H_6 } < \delta D_{C_3 H_8 } < \delta D_{C_4 H_{10} } $ . The δ 13C values and δ D values are negatively correlated. Natural gases from 26 commercial gas wells distributed in the Xujiaweizi and Yingshan-Miaotaizi faulted depressions in the Songliao Basin, China, show δ13C1 values ranging from ?30.5% to ?16.7% with a very narrow δ D range between ?203‰?196‰ These gases are characterized by a reverse distribution of δ 13C values but a normal distribution of δ C values, and a negative correlation between their δ 13C and δ C values, indicating an abiological origin. The present study has revealed that abiogenic hydrocarbons not only exist in nature but also can make significant contribution to commercial gas reserviors. It is estimated that the reserve volume of alkane gases with abiogenic characteristics in these 26 gas wells in the Songliao Basin is over 500×108 m3. The prospecting practice in the Songliao Basin has demonstrated that abiogenic alkane gases are of a promising resource, and it provides an example for the investigation of and search for abiogenic commercial natural gases worldwide. 展开更多
关键词 generation mechanism of natural GASES kinetic ISOTOPE FRACTIONATION the Songliao Basin of China COMMERCIAL abiogenic HYDROCARBON gaspool
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