延长探区山西组陆相页岩储层孔隙结构及孔隙发育主要影响因素

    Pore structure and its influence factors of lacustrine facies shale reservoirs inShanxi formation of Yanchang exploration area

    • 摘要: 储层的孔隙特征对页岩气含气性和产能评价具有重要作用,为研究延长探区山西组页岩气储层孔隙特征,通过应用氩离子抛光-场发射扫描电子显微镜、岩芯观察、薄片鉴定、全岩X射线衍射和压汞实验等测试方法,对孔隙类型和孔隙结构进行了详细探究。结果表明山西组页岩气储层矿物组成以黏土矿物和石英为主,黏土矿物含量较高,且变化范围较大,在43.5%~98%之间。储层发育大量的微裂隙和微孔隙,孔径主要在0.5~20 μm之间,以微小孔隙为主,喉道较小且孔喉分选性较差,显微镜下观察发现储层泥页岩微裂缝极为发育,裂缝面密度达到108.8/m2,这些缝隙构成网状结构,既可以为页岩气提供储存空间,又是页岩气渗流的主要通道。有机碳含量高,有机质孔数量相应增加,碎屑含量降低, 减小了对有机质的挤压程度,有利于有机质孔的保存。热演化程度增高,有机质生烃转化和生气膨胀作用增加了有机质孔。进一步,黏土矿物在脱水转化过程中形成了微裂缝,对孔隙发育均具有促进作用。

       

      Abstract: The porosity characteristics of reservoir play an important role in the evaluation of gas-bearing and the production capacity of shale gas.In order to study the pore characteristics of shale gas reservoir in Shanxi formation of Yanchang exploration area, this paper integrates various technologies, such as observations of argon ion etching-polishing emission scanning electron microscopy, core observation, thin section, X-ray diffraction analysis, nuclear magnetic resonance and mercury injection to explore the pore types and pore structures detailed.The results show that the shale gas reservoir in Shanxi formation are dominated by clay mineraland quartz, it contain higher clay mineral and clay mineral content have larger variation from 43.5% to 98%.The reservoir develops a large number of micro-fractures and micro-pores.The pore size of reservoir ranging from 0.5 μm to 20 μm, pores are dominated by tiny pores, throat is small and unevenly distributed and pore throat sorting characteristic is poor.The micro-fracture of mud shale in the Shanxi formation is extremely developedobserved under the microscopeand the area density of crack can measure up 108.8/m, these pores and fracturesform a network structure are main channel for shale gas seepage and provides storage space for shale gas.Total organic carbon is higher, the number of organic pores will increase accordingly, and decrease in detritus content will reduce the degree of extrusion of organic matter, which propitious to the preservation of organic pores.Higher thermal evolution can increase organic pores under the effect of organic hydrocarbon generation and gas expansion, and clay minerals an form micro-fractures during dehydration conversion.All of them have a promoting effect on pore development.

       

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