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Effects of Aquifer Parameters on Long-Term Storage of Carbon Dioxide in Saline Aquifers

机译:含水层参数对盐水含水层中二氧化碳长期储存的影响

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Geological storage of carbon dioxide has been recognized as one of the most effective options for mitigation of industrial emissions. Deep saline formations, otherwise called saline aquifers, are among the potential sequestration targets. To enhance the confidence regarding some of the key issues, such as site selection, planning, injection itself and long term monitoring of sequestration site, management of uncertainties is an essential step. This paper consists of two main parts. In the first part, CO2 storage in Mt. Simon sandstone in Ohio State, USA, is modeled using two compositional simulators – TOUGH2-ECO2N and CMG-GEM, which results provide an initial assessment for storage capacity of this site and discuss possible safety issues. In the second part, objective is reached using combination of experimental design and response surface methodology. Experimental Design (DOE) is an unbiased, rapid approach for obtaining probabilistic results. The purpose of Response Surface Methodology (RSM) is to fit simulation results to a response surface using analytical or numerical functions. In this study, DOE and RS methodologies were jointly applied to investigate the effect of uncertainties of key saline aquifer parameters on long-term CO2 storage in the form of solubility trapping and on the total storage capacity. The selected parameters in this study are: absolute permeability, global porosity, end point saturations, irreducible liquid saturation, temperature, aqueous phase salinity, vertical to horizontal permeability ratio, diffusion coefficient of CO2 in brine and relative depth of perforation interval. Mt. Simon is expected to be a safe, secure CO2 storage formation within selected site due to several factors such as regionally extensive caprock and seals including Eau Claire Formation (Cambrian) and Knox Dolomite (Cambo-Ordovician) and high CO2 storage capacity with favorable reservoir properties. This conclusion is supported by the results of modeling performed using both TOUGH2 and CMG GEM simulators. It is expected that 15-17 Mt of CO2 could be safely injected into Mt. Simon formation during 25 years via one vertical injection well while staying below fracturing pressure. It was demonstrated that combination of DOE and RSM techniques could be successfully applied for research into CO2 sequestration.
机译:二氧化碳的地质储存已被确认为对工业排放的缓解最有效的选择之一。深部咸水层,否则所谓的盐水层,是潜在的封存目标之一。为了增强对于一些关键问题,如选址,规划,注射本身和长期监测封存地点的信心,不确定性的管理是一个重要的步骤。本文包括两个主要零件。 TOUGH2-ECO2N和CMG-创业板,其结果对本网站的存储容量,提供了一个初步评估,并讨论可能的安全问题 - 在第一部分中,二氧化碳储存在俄亥俄州,美国西蒙山砂岩,使用两个组分模拟器模拟。在第二部分中,目标是用实验设计和响应面分析法的组合达到。实验设计(DOE)对获得的概率结果的公正,快速的方法。响应面分析法(RSM)的目的是为了配合仿真结果使用分析或数字功能的响应面。在这项研究中,DOE和RS进行的方法联合应用到调查键盐水的不确定性的含水层参数对长期储存二氧化碳的溶解度俘获的形式,并且在总存储容量的效果。在本研究中所选择的参数是:绝对渗透率,孔隙度全球,结束点的饱和度,束缚液体饱和度,温度,水相含盐量,垂直到水平的渗透率比,在盐水和穿孔间隔的相对深度的二氧化碳扩散系数。山西蒙预计将选定的站点内的一个安全的,安全的二氧化碳封存形成由于几个因素,如区域广泛盖层和密封件包括欧克莱尔组(寒武纪)和诺克斯白云石(金宝-奥)和高CO 2的存储容量具有良好储层性质。这个结论是通过同时使用TOUGH2和CMG创业板仿真建模设计执行结果的支持。据预计,二氧化碳的15-17万吨可以安全25年来,通过一个垂直注入井,同时保持低于破裂压力注入到山西蒙形成。这证明DOE的该组合和RSM技术可以成功地用于研究CO2封存。

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