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Preinjection reservoir fluid characterization at a CCS demonstration site: Illinois Basin – Decatur Project, USA

机译:在CCS示范现场的预注解储层液体特性:伊利诺伊州盆地 - 美国衰老项目

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The Midwest Geological Sequestration Consortium is conducting the Illinois Basin – Decatur Project (IBDP), a large-scale carbon capture and storage (CCS) project in Decatur, Illinois, USA. An extensive Monitoring, Verification, and Accounting (MVA) program has been implemented, and a deep monitoring well, VW#1, was drilled to a depth of 2,201 m (7,264 ft). The well was perforated in eleven zones ranging in depth from 1,499 to 2,153 m (4917 to 7061 ft.). Fluid samples were collected during three sampling events using two different sampling methods. This paper describes the well construction, well completion, sample collection procedures, and selected preinjection sampling results from VW#1. Prior to sampling, particular care was taken to remove non-native fluids from each of the sampling zones. Density, specific conductance, bromide concentrations, and bromide-chloride ratios have been used as indicators of sample representativeness. Fluid compositional data and formation pressure data have been collected from VW#1. These high-quality, fieldbased data are essential to establish hydrochemical conditions in and above the storage reservoir prior to CO_2 injection, indicate the response of the reservoir to injection, provide detailed geochemical model inputs, and provide insights for on-going work at the Illinois State Geological Survey about the origin of Illinois Basin brines. Primary brine constituents are chloride, sodium, and calcium with average total dissolved solids concentrations of 190,000 mg/L in the Mt. Simon Sandstone and 65,600 mg/L in Ironton-Galesville Formation (above the injection reservoir).
机译:中西部地质封存财团正在美国伊利诺伊州的伊利诺伊州山地山地衰老项目(IBDP),大型碳捕获和储存(CCS)项目。已经实施了广泛的监测,验证和会计(MVA)计划,深度监测井VW#1被钻到了2,201米(7,264英尺)的深度。井在119℃的11个区域中穿孔,从1,499到2,153米(4917至7061英尺)。使用两种不同的采样方法在三种采样事件中收集流体样品。本文介绍了井的结构,完井,样品收集程序,以及VW#1的选定预注油采样结果。在取样之前,采取特别小心去除来自每个采样区的非天然流体。密度,特异性电导,溴化物浓度和溴 - 氯化物比已被用作样品代表性的指标。已经从VW#1收集了流体组成数据和形成压力数据。这些高质量的现场比较数据对于在CO_2注射之前建立储存储存器中的水质条件,表明储存器对注射的响应,提供详细的地球化学模型输入,并为伊利诺伊州的持续工作提供了洞察力伊利诺伊州盆地盐水起源的国家地质调查。原发性盐水成分是氯化物,钠和钙,平均总溶解固体浓度为190,000mg / L的MT.Simon砂岩和65,600 mg / L在Ironton-Galesville Mablation(注射储存器上方)。

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