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首页> 外文期刊>Marine and Petroleum Geology >Effects of oil expulsion and pressure on nanopore development in highly mature shale: Evidence from a pyrolysis study of the Eocene Maoming oil shale, south China
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Effects of oil expulsion and pressure on nanopore development in highly mature shale: Evidence from a pyrolysis study of the Eocene Maoming oil shale, south China

机译:油气排出与压力对高度成熟页岩中纳米孔发育的影响:来自南方虫草石材石油页岩热解研究的证据

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摘要

The influence of oil-expulsion efficiency on nanopore development in highly mature shale was investigated by using anhydrous pyrolysis (425-600 degrees C) on solvent-extracted and non-extracted shales at a pressure of 50 MPa. Additional pyrolysis studies were conducted using non-extracted shales at pressures of 25 and 80 MPa to further characterize the impact of pressure on pore evolution at high maturity. The pore structures of the original shale and relevant artificially matured samples after pyrolysis were characterized by using low-pressure nitrogen and carbon-dioxide adsorption techniques, and gas yields during pyrolysis were measured. The results show that oil-expulsion efficiency can strongly influence gas generation and nanopore development in highly mature shales, as bitumen remained in shales with low oil expulsion efficiency significantly promotes gaseous hydrocarbon generation and nanopore (diameter < 10 nm) development. The evolution of micropores and fine mesopores at high maturity can be divided into two main stages: Stage I, corresponding to wet gas generation (EasyRo 1.2%-2.4%), and Stage II, corresponding to dry gas generation (EasyRo 2.4%-4.5%). For shales with low oil expulsion efficiency, nanopore (diameter < 10 nm) evolution increases rapidly in Stage I, whereas slowly in Stage II, and such difference between two stages may be attributed to the changes of the organic matter (OM)'s mechanical properties. Comparatively, for shales with high oil expulsion efficiency, the evolution grows slightly in Stage I, not as rapidly as shales with low efficiency, and decays in Stage II. The different pore evolution behaviors of these two types of shales are attributed to the contribution of bitumen. However, the evolution of medium coarse mesopores and macropores (diameter > 10 nm) remains flat at high maturation. In addition, high pressure can promote the development of micropores and fine mesopores in highly mature shales. (C) 2017 Elsevier Ltd. All rights reserved.
机译:通过在50MPa的压力下使用无水溶解和未提取的Haales对高度成熟的页岩纳米孔发育对纳米孔发育的影响。在25和80MPa的压力下使用未提取的Shales进行额外的热解性研究,以进一步表征压力对高成熟度的影响。通过使用低压氮和二氧化碳吸附技术,对原始页岩和相关人工成熟的样品的孔结构表征,测量热解期间的气体产率。结果表明,油排水效率可以强烈影响气体产生和纳米孔发育在高度成熟的Shales中,因为沥青留在具有低油驱排水效率的Shales中,显着促进了气态碳氢化合物产生和纳米孔(直径<10nm)的发育。微孔和精细的中孔的演变可以分为两个主要阶段:阶段I,对应于湿气体产生(EasyRO 1.2%-2.4%),以及对应于干燥气体产生的阶段II(EasyRO 2.4%-4.5 %)。对于具有低油驱排水效率的Shales,纳米孔(直径<10nm)的进化在阶段I中迅速增加,而在阶段II中缓慢地增加,两个阶段之间的这种差异可能归因于有机物质(OM)机械的变化特性。相比之下,对于具有高油驱排水效率的Haales,演变在阶段I略微生长,而不是低效率的索拉斯,并且在阶段衰减。这两种神话的不同孔隙演化行为归因于沥青的贡献。然而,在高成熟度下,中等粗疏孔和大孔(直径> 10nm)的演变保持平坦。此外,高压可以促进高度成熟的Shales中微孔和细胞泡的发育。 (c)2017 Elsevier Ltd.保留所有权利。

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