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ENTROPY PRODUCTION OF HYDRATE TRANSPORT IN SUBSEA MULTIPHASE PIPELINE FLOWS

机译:水下多相管道中水合物的熵产

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A numerical model is developed to examine the flow conditions of multiphase heat transfer and entropy production during hydrate formation in subsea pipelines. The temperature and pressure gradients of the oil and gas flow in subsea pipelines lead to entropy generation. This paper examines the impacts and effects of thermodynamic irreversibilities on the nucleation and growth processes of hydrate crystals in the pipeline flows. The effects of heat transfer ratio, internal diameter of the pipe, molar gas density, and environment temperature on entropy production in subsea pipelines are predicted and discussed in this paper. The numerical model accounts for the temperature distribution along the axial length of the pipe, reaction kinetics, and mass transfer between the solid and fluid layer. The kinetic energy of the hydrate particles during the coagulation process is analyzed in the numerical model. The results indicate that entropy production is highest at the beginning of the nucleation process. Pipelines with smaller internal radii have a lower rate of hydrate formation in subsea pipelines. The results from the numerical model are verified by comparison with experimental results for structure type Ⅱ natural gas hydrates.
机译:建立了一个数值模型,以检查海底管道中水合物形成过程中多相传热和熵产生的流动条件。海底管道中的油气流动的温度和压力梯度会导致产生熵。本文研究了热力学不可逆性对管道流中水合物晶体成核和生长过程的影响和影响。预测并讨论了传热比,管道内径,摩尔气体密度和环境温度对海底管道熵产的影响。数值模型考虑了沿管道轴向长度的温度分布,反应动力学以及固体和流体层之间的传质。在数值模型中分析了凝结过程中水合物颗粒的动能。结果表明,在成核过程开始时,熵产生最高。内部半径较小的管道在海底管道中形成水合物的速率较低。通过与结构Ⅱ型天然气水合物的实验结果进行比较,验证了数值模型的结果。

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