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Effect of pore structure on the seepage characteristics of tight sandstone reservoirs: A case study of Upper Jurassic Penglaizhen Fm reservoirs in the western Sichuan Basin

机译:孔隙结构对致密砂岩储层渗流特征的影响-以川西盆地上侏罗统蓬莱镇组储层为例

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Tight sandstone reservoirs are characterized by complex pore structures and strong heterogeneity, and their seepage characteristics are much different from those of conventional sandstone reservoirs. In this paper, the tight sandstone reservoirs of Upper Jurassic Penglaizhen Fm in western Sichuan Basin were analyzed in terms of their pore structures by using the data about physical property, mercury injection and nuclear magnetic resonance (NMR) tests. Then, the seepage characteristics and the gas–water two-phase migration mechanisms and distribution of tight sandstone reservoirs with different types of pore structures in the process of hydrocarbon accumulation and development were simulated by combining the relative permeability experiment with the visual microscopic displacement model. It is shown that crotch-like viscous fingering occurs in the process of gas front advancing in reservoirs with different pore structures. The better the pore structure is, the lower the irreducible water saturation is; the higher the gas-phase relative permeability of irreducible water is, the more easily the gas reservoir can be developed. At the late stage of development, the residual gas is sealed in reservoirs in the forms of bypass, cutoff and dead end. In various reservoirs, the interference between gas and water is stronger, so gas and water tends to be produced simultaneously. The sealed gas may reduce the production rate of gas wells significantly, and the existence of water phase may reduce the gas permeability greatly; consequently, the water-bearing low-permeability tight sandstone gas reservoirs reveal serious water production, highly-difficult development and low-recovery percentage at the late stage, which have adverse impacts on the effective production and development of gas wells.
机译:致密砂岩储层的孔隙结构复杂,非均质性强,其渗流特征与常规砂岩储层有很大不同。本文利用物性,注汞和核磁共振试验数据,对川西上侏罗统蓬莱镇组致密砂岩储层进行了孔隙结构分析。然后,通过相对渗透率实验与可视化微观位移模型相结合,模拟了不同孔隙结构的致密砂岩油藏在油气成藏过程中的渗流特征,气水两相运移机理和分布。结果表明,在具有不同孔隙结构的储层中,瓦斯前移过程中出现c状粘性指状。孔隙结构越好,不可还原的水饱和度越低;不可还原水的气相相对渗透率越高,储气库越容易开发。在开发的后期,残余气体以旁路,截止和死角的形式被密封在储层中。在各种储层中,气与水之间的干扰更强,因此倾向于同时生产气和水。封闭的气体会大大降低气井的生产率,而水相的存在会大大降低气体的渗透率。因此,含水低渗致密砂岩气藏后期出水严重,开发难度大,采收率低,对气井的有效开发产生不利影响。

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