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Lithological and Petrophysical Core-Log Interpretation in CO_2SINK, the European CO_2 Onshore Research Storage and Verification Project

机译:欧洲CO_2陆上研究存储和验证项目CO_2SINK中的岩性和岩石物理岩心测井解释

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The storage of carbon dioxide (CO_2) in saline aquifers is one of the most promising options for Europe to reduce emissions of greenhouse gases from power plants to the atmosphere and to mitigate global climate change. The CO_2SINK (CO_2 Storage by Injection into a saline aquifer at Ketzin) project is a research and development (R&D) project, mainly supported by the European Commission, the German Federal Ministry of Education and Research, and the German Federal Ministry of Economics and Technology, targeted at developing an in-situ laboratory for CO_2 storage.rnThe preparatory phase of the project involved a baseline geological-site exploration and the drilling of one injection and two observation wells, as well as the acquisition of a geophysical baseline and geochemical monitoring, in Ketzin, located near Berlin. The target saline aquifer is the lithologically heterogeneous Triassic Stuttgart formation, situated at approximately 630- to 710-m (2,070- to 2,330-ft) depth. A comprehensive borehole-logging program was performed consisting of routine well logging complemented with an enhanced logging program for one well that recorded nuclear-magnetic-resonance (NMR) and borehole-resistivity images, to characterize the storage formation better. A core analysis program carried out on reservoir rock and caprock included measurements of helium porosity, nitrogen permeability, and brine permeability at different pressure conditions.rnThe saline aquifer at Ketzin shows a variable porosity/permeability distribution, which is related to grain size, facies variation, and rock cementation with values in the range from 5 to > 35% and 0.02 to > 5,000 md for porosity and permeability, respectively. On the basis of core analysis and logging data, an elemental log-analysis model for the target formation was established for all three wells. In addition, permeability was estimated using the Coates equation and compared with core data and NMR log-derived permeability, which seems to provide meaningful permeability estimates for the Ketzin reservoir. On the basis of the good core control that guided the petrophysical well-log interpretation in the first two CO_2SINK wells, a porosity and permeability prediction by analogy for the third well is appropriate and applicable. The availability of cores was crucial for a sophisticated formation evaluation at borehole scale that characterizes the real subsurface conditions.
机译:在欧洲,减少发电厂向大气排放的温室气体并减轻全球气候变化是最有希望的选择之一,在盐水层中储存二氧化碳(CO_2)是最有希望的选择之一。 CO_2SINK(通过注入Ketzin的盐水层中的CO_2来储存)项目是一项研究与开发(R&D)项目,主要由欧洲委员会,德国联邦教育与研究部以及德国联邦经济技术部支持,目的是建立一个用于CO_2储存的现场实验室。该项目的准备阶段包括基线地质现场勘探,一口注入和两口观察井的钻探,以及获取地球物理基线和地球化学监测,位于柏林附近的Ketzin。目标盐水层是岩性非均质的三叠纪斯图加特地层,位于约630至710 m(2,070至2,330 ft)的深度。进行了全面的井眼测井程序,该程序包括常规测井,以及针对一个井的增强测井程序,该程序记录了核磁共振(NMR)和井眼电阻率图像,以更好地表征储层特征。在储层岩石和盖层上进行的岩心分析程序包括测量不同压力条件下的氦气孔隙度,氮渗透率和盐水渗透率。rnKetzin的盐水层显示出可变的孔隙度/渗透率分布,这与粒度,相变有关。孔隙度和渗透率分别为5到> 35%和0.02到> 5,000 md。在岩心分析和测井数据的基础上,为所有三口井建立了用于目标形成的元素测井分析模型。此外,使用Coates方程估算了渗透率,并将其与岩心数据和NMR对数衍生的渗透率进行了比较,这似乎为Ketzin油藏提供了有意义的渗透率估算。在指导前两个CO_2SINK井进行岩石物理测井解释的良好岩心控制的基础上,第三类井的类比孔隙度和渗透率预测是适当和适用的。岩心的可用性对于表征真实地下条件的井下规模的复杂地层评估至关重要。

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