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Nanometer Pore Structure Characterization of Chang 7 Member Continental Shale in Northern Shaanxi Area, Ordos Basin Based on the Nitrogen Adsorption Experiment

机译:鄂尔多斯盆地陕西州北部昌7成员大陆位数的纳米孔结构特征,鄂尔多斯盆地基于氮吸附实验

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摘要

The Northern Shaanxi Area, Ordos Basin is an important continental shale gas exploration area in China. The Chang 7 Member of Upper Triassic Yanchang Formation is a main exploration interval for this area. In order to strengthen research on nanometer pore structures of Chang 7 Member shale reservoirs in the Northern Shaanxi Area, the microscopic pore structure characteristics are studied through the nitrogen adsorption experiment. The main controlling factors of pore development are discussed and the significance of pore structure for shale gas storage is analyzed. Results show that the pores of shale reservoirs of Chang 7 Member are dominated by nanoscale ones and the average pore size of shale samples is between 5.7 and 7.9 nm. According to IUPAC classification, shale pores of Chang 7 Member are dominated by mesopores, accounting for 90.8%-95.5% of the total pore volume. The nanometer pore structure is relatively uniform and the adsorption/desorption curves are dominated by Type B in the De Boer classification. The micropore volume and the macropore volume have similar proportions, and they account for 4.5%-9.2% of the total volume, averaging at 7.2%. Characteristics of Type E indicate that most pores are open type ones, and slit-like pores and 'ink bottle' shaped pores are irregularly configured. Total organic carbon (TOC) has a weak negative correlation with specific surface area of the shale, and has a weak positive correlation with total pore volume. Maturity (Ro) has a weak negative correlation with both specific surface area and total pore volume. The content of brittle minerals and content of clay minerals have no clear correlation with the specific surface area and the pore volume.
机译:鄂尔多斯盆地北陕西地区是中国重要的大陆物流煤气勘探区。高三叠纪延长地层的常7成员是该地区的主要探索间隔。为了加强陕北昌7成员页岩储层纳米孔结构的研究,通过氮吸附实验研究了微观孔隙结构特性。讨论了孔隙发育的主要控制因素,分析了页岩气体储存孔隙结构的重要性。结果表明,常7成员的页岩储层毛孔由纳米级载体主导,页岩样品的平均孔径为5.7和7.9nm。根据IUPAC分类,常7会员的页岩毛孔由中孔占主导地位,占总孔隙体积的90.8%-95.5%。纳米孔结构相对均匀,吸附/解吸曲线在DE BOER分类中由B型主导。微孔体积和大孔体积具有相似的比例,它们占总量的4.5%-9.2%,平均为7.2%。 E型特性表明大多数孔隙是开放式的,并且狭缝状孔和“墨水瓶”形孔不规则地配置。总有机碳(TOC)具有与页岩的比表面积弱的负相关性,并且具有与全孔体积的弱阳性相关性。成熟(RO)与比表面积和全孔总量的弱负相关性。脆性矿物质的含量和粘土矿物的含量与比表面积和孔体积没有明显的相关性。

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