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Gas–Liquid–Solid Migration Characteristicsof Gas Hydrate Sediments in Depressurization Combined with ThermalStimulation Dissociation

机译:气液固迁移特性热结合降压过程中天然气水合物沉积物的变化刺激解离

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摘要

The exploitation of natural gas hydrate is always hindered by the migration of water and sands due to gas production. Depressurization combined with thermal stimulation is an effective method for hydrate dissociation. This paper reported the influence of gas–liquid–solid migration on morphological change of hydrate sediments in natural gas production using visualization method. Different backpressures combined with thermal stimulation methods were applied to simulate natural gas hydrate exploitation. Pressure compensation was first employed to study sediment recovery features. The expansion rate of a porous medium layer under combined dissociation and different backpressure (4.5, 3.5, 2.5, 1.5, and 0.1 MPa) was discussed. A 176% hydrate sediment expansion rate was found after the combined dissociation at 0.1 MPa. In addition, it was observed that the height of the water layer above the porous media after pressure compensation was gradually reduced with a decrease in backpressure and eventually disappeared at 0.1 MPa. It was also found that the disappearing water layer caused ananomalous memory effect phenomenon. Expansion and subsidence of sedimentsprovide a better reference for hydrate exploitation and geologicalsafety.
机译:天然气水合物的开采总是受到由于天然气生产而引起的水和砂子迁移的阻碍。减压与热刺激相结合是水合物分解的有效方法。本文使用可视化方法报告了气液固迁移对天然气生产中水合物沉积物形态变化的影响。应用不同的背压结合热刺激方法模拟天然气水合物的开采。首先采用压力补偿来研究沉积物的回收特征。讨论了组合解离和不同背压(4.5、3.5、2.5、1.5和0.1 MPa)下多孔介质层的膨胀率。在0.1 MPa的条件下合并解离后,发现了176%的水合物沉积物膨胀率。此外,观察到压力补偿后多孔介质上方的水层高度随着背压的降低而逐渐减小,并最终在0.1MPa时消失。还发现消失的水层引起了异常记忆效应现象。沉积物的膨胀和沉降为水合物开发和地质提供更好的参考安全。

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