北海北部Johansen组潜在CO2储层特征

M. Fawad, N. Mondol
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引用次数: 2

摘要

为了评价地下储层的CO2封存能力,粒度性质和成岩作用对注入能力和随后的动员作用至关重要。本文以北海北部巨魔气田附近侏罗系约翰森组为研究对象。约翰森组为含盐含水层,迄今尚未发现油气。利用岩石物理和岩石物理技术对24口井进行了分析,获得了净储层、净总比、有效孔隙度、页岩体积和胶结程度,并试图将这些参数与影响这些参数的因素联系起来。发现储层性质大约在小于2000m(低于海底,BSF)的深度附近是最佳的。即使是最浅的砂岩也表现出胶结作用,表明在沉积物沉积过程中方解石沉淀。然而,页岩的存在抑制了石英胶结作用,可能保留了孔隙度。这些发现将有助于了解Johansen砂岩储层的复杂性以及非均质性对CO2迁移的影响。
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Reservoir Characterisation Of Johansen Formation As Potential CO2 Storage Reservoir In The Northern North Sea
To evaluate subsurface reservoirs for CO2 sequestration, the grain scale properties and role of diagenesis is important for the injectivity and the subsequent mobilization. This study focuses on Johansen Formation of Jurassic age in the vicinity of Troll field within the northern North Sea. Johansen Formation is a saline aquifer and no hydrocarbon discovery has been reported in this reservoir so far. We analysed 24 wells using petrophysics and rock physics techniques to obtain net reservoir, net to gross ratio, effective porosity, volume of shale and level of cementation, and attempted to relate these parameters with the factors influencing them. The reservoir properties were found to be optimal approximately around depths shallower than 2000m (below sea floor, BSF). Even the shallowest sandstones exhibited cementation indicating calcite precipitation while the sediments deposited. Presence of shale however found to inhibit the quartz cementation possibly preserving the porosity. These findings will help understanding the complexity of the Johansen Sandstone as storage reservoir and the influence of heterogeneity on CO2 migration.
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