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A Case Study of Detailed Computational Fluid Dynamic Modelling of Coupled Wellbore and Subsurface Multiphase Reactive Flow

机译:耦合井筒和地下多相反应流动的详细计算流体动力学模型的案例研究

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A novel concept of circulating molten salt (CMS) through a subsurface formation has been developed for the purpose of in- situ upgrading (IUP) of heavy oils into lighter transportation fuels, in pursuit of its potential to substantially reduce power expenditures and CO2 emissions during the IUP process. The CMS system can utilize molten nitrate salt to transfer heat from a surface heat source down to the hydrocarbon (HC) bearing reservoir via a system of underground pipes, essentially creating a subsurface heat exchanger. Nitrate salts are known to be strong oxidizers and can react exothermally with various hydrocarbon constituents in the subsurface under certain conditions. Detailed Computational Fluid Dynamics (CFD) simulations were carried out to evaluate the consequences of an accidental release of molten nitrate salt from a failed pipe and into the surrounding formation rock. Modeling results have been used to assess: (1) the temperature and pressure build up in the near wellbore region; and (2) the propagation of a reaction front in the formation and its impact on neighboring heater/producer wells. Extensive sensitivity analyses on salt temperature, reaction rate constants, and time of occurrence were performed. The simulation results indicate that the reaction progress is likely to be mass-transfer controlled rather than kinetically controlled under subsurface conditions. Both pressure and temperature build up are likely to be moderate in the event of a large release of molten salt. The damage that a moving burning front in the formation may cause to neighboring heater pipes appears to be manageable as long as sufficient flow rate is maintained in these pipes.
机译:通过地下地层循环熔融盐(CMS)的新颖概念是为了原位升级(IUP)的重油进入较轻的运输燃料,旨在显着降低电力支出和二氧化碳排放IUP过程。 CMS系统可以利用熔融的硝酸盐盐通过地下管系统从表面热源从表面热源转移到烃(HC)轴承储存器,基本上产生了地下热交换器。已知硝酸盐是强氧化剂,并且可以在某些条件下与地下的各种烃成分进行热反应。进行了详细的计算流体动力学(CFD)模拟,以评估熔融硝酸盐从失效管道和周围地层岩石中释放熔融硝酸盐的后果。建模结果已被用于评估:(1)在井筒区附近的温度和压力累积; (2)反应前沿在地层中的繁殖及其对邻近加热器/生产者井的影响。进行盐温,反应速率常数和发生时间的广泛敏感性分析。仿真结果表明,反应进展可能是在地下条件下的传质控制而不是动力学控制。在大释放熔盐的情况下,压力和温度增强可能是中等的。由于在这些管道中保持足够的流速,因此在地层中移动燃烧前部的损坏可能导致相邻的加热器管道似乎是可控的。

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