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Sequential storage and in-situ tracking of gas in geological formations by a systematic and cyclic foam injection- A useful application for mitigating leakage risk during gas injection

机译:系统和循环泡沫注入通过系统和循环泡沫注射在地质构造中的顺序储存及地原位跟踪 - 一种有用的应用气体注射过程中泄漏风险的应用

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Geological storage of Carbon Dioxide (CO2) can safely and permanently store a huge amount of anthropogenic greenhouse gases. However, the possible leakage of mobile gases through the cap rock that confines them within the reservoir is a cause of safety concerns. Residual and solubility trapping of the injected gas in the pores of the rock can reduce the amount of mobile gas lying below the cap rock. These trapping mechanisms will only begin at the end of several decades of gas injection, which implies that there is an imminent risk of discharge of large amount of gas in the event of a leak. This paper presents a method to fast-track and enhance residual and solubility trapping process while gas injection is in progress, such that only a fraction of the injected gas will migrate and be trapped beneath the cap rock after injection ceases. The method involves cyclic injection of gas and water (containing small amount of foaming agent). Foams are known to have gas trapping characteristics during flow in porous medium. A series of laboratory experiments was conducted on representative rock samples at different reservoir conditions. The results show a sequential and cumulative growth in trapped gas during cyclic injection of gas and foam based on in-situ and real time measurements of gas saturation in the samples using electrical resistivity tool. The amount of trapped (residual) gas depends on the type of gas (N-2 or CO2), water salinity, concentration of the foaming agent, and temperature. The highest residual gas saturations (50%-70% of reservoir pore volume) occurred at a temperature and water salinity typical of a deep saline aquifer (45 degrees C and 58,000 ppm water). At a high water salinity of 242,000 ppm, the residual gas saturation was significantly lower (27%-30%). Similarly, at a high temperature of 90 degrees C, the residual gas saturation reduced to 27%. Residual gas could not be sustained when CO2 is injected compared to N-2 because of the low interfacial tension between CO2 and water, which reduces the foam quantity and strength. The importance of foam stabilizing agents (e.g. polymers and nanoparticles) in addressing the observed shortcomings in CO2 foam and for foam injection in high salinity - high temperature reservoirs is discussed. A field scale application of this method is also highlighted.
机译:二氧化碳(CO2)的地质储存可以安全地储存大量的人为温室气体。然而,移动气体通过盖岩岩石泄漏,这些岩石将它们限制在水库内是安全问题的原因。岩石孔中注入气体的残余和溶解度诱捕可以减少盖帽下方的移动气体量。这些捕获机制只会在几十年的气体注入结束时开始,这意味着在泄漏时存在迫在眉睫的气体排出大量气体。本文介绍了一种方法来快速跟踪和增强残留和溶解性捕获过程,同时进入气体注射,使得只有注射气体的一部分将在注射停止后迁移并被捕获在盖岩下方。该方法涉及循环注入气体和水(含有少量发泡剂)。已知泡沫在多孔介质的流动期间具有气体捕获特性。在不同储层条件下的代表性岩石样品上进行了一系列实验室实验。结果显示了使用电阻率工具在样品中的原位和实时测量样品中的气体饱和期间在循环注入气体和泡沫过程中捕获气体的顺序和累积生长。被捕获的(残留)气体的量取决于气体(N-2或CO 2),水盐度,发泡剂浓度和温度的类型。最高的残余气体饱和(50%-70%的储层孔体积)发生在典型的盐水含水层(45摄氏度和58,000ppm)的温度和水盐度下发生。在高242,000ppm的高水盐度下,残留的气体饱和度明显较低(27%-30%)。类似地,在90℃的高温下,残留的气体饱和度降低至27%。当CO 2与N-2相比,由于CO 2和水之间的界面张力低而注入CO 2时,残留气体不能持续,这降低了泡沫量和强度。讨论了泡沫稳定剂(例如聚合物和纳米颗粒)在寻址CO 2泡沫中观察到的缺点和高盐度 - 高温储层中观察到的缺点的重要性。还突出了该方法的现场规模应用。

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