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Using pressure recovery at a depleted gas field to understand saline aquifer connectivity

机译:在耗尽的气体场上使用压力恢复以了解盐水含水层的连接

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A key uncertainty facing Carbon dioxide Capture and Storage (CCS) in saline aquifers is long term injectivity, which is primarily a function of the connected aquifer pore-volume within which formation brine can be displaced as the CO2 is injected. Protracted injection testing to interrogate and prove the far-field connected pore-volume would increase the lead-in times for commissioning of storage sites and would significantly increase appraisal costs. Here we use natural gas production and subsequent reservoir recharge legacy data from the Esmond gas field in the UK sector of the southern North Sea to gain an understanding of the dynamic behaviour of the Bunter Sandstone, a major saline aquifer. Results suggest that Esmond has a connected pore volume of 1.83xl010 m3, suitable for injecting CO2 at a rate of up to 2 million tonnes per year for at least 55 years. 3D seismic data suggest that Esmond reservoir properties are likely to be replicated across the wider Bunter Sandstone aquifer, notably around the Endurance structure which was, until recently, proposed for a full-chain CCS project.
机译:在盐水层面临二氧化碳捕获和储存(CCS)的一个关键不确定性是长期注入性,这主要是所连接的含水层的孔隙体积内哪个作为CO2被注入地层盐水可以移动的功能。旷日持久的注入测试查询和证明远场连接孔容积会增加导入时间储存点的调试,并会显著增加鉴定成本。在这里,我们使用天然气的生产和后续水库补给旧数据从李建英气场在英国部门北海南部的获得对Bunter砂岩,主要的盐水层的动态行为的理解。结果表明,李建英具有1.83xl010 M3的连接孔容积,适合在高达的速度每年200万吨,至少55年CO2注入。三维地震数据表明,李建英储层物性有可能在更广泛的Bunter砂岩含水层被复制,特别是周围的耐力结构是,直到最近,提出了一个完整的链CCS项目。

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