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降压联合热刺激分解过程中天然气水合物沉积物的气-液-固迁移特性

Gas-Liquid-Solid Migration Characteristics of Gas Hydrate Sediments in Depressurization Combined with Thermal Stimulation Dissociation.

作者信息

Cheng Chuanxiao, Wang Fan, Zhang Jun, Qi Tian, Xu Peiyuan, Zheng Jili, Zhao Jiafei, Zhang Hanquan, Xiao Bo, Li Lun, Yang Penglin, Lv Shuai

机构信息

School of Energy and Power Engineering, Zhengzhou University of Light Industry, Zhengzhou 450002, China.

Key Laboratory of Ocean Energy Utilization and Energy Conservation of Ministry of Education, Dalian University of Technology, Dalian 116024, China.

出版信息

ACS Omega. 2019 Oct 10;4(17):17547-17555. doi: 10.1021/acsomega.9b02497. eCollection 2019 Oct 22.

Abstract

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 an anomalous memory effect phenomenon. Expansion and subsidence of sediments provide a better reference for hydrate exploitation and geological safety.

摘要

天然气水合物的开采总是因产气导致水和砂的运移而受到阻碍。降压与热刺激相结合是水合物分解的有效方法。本文采用可视化方法报道了气液固运移对天然气开采过程中水合物沉积物形态变化的影响。应用不同背压与热刺激方法相结合来模拟天然气水合物开采。首先采用压力补偿来研究沉积物恢复特征。讨论了在联合分解和不同背压(4.5、3.5、2.5、1.5和0.1MPa)下多孔介质层的膨胀率。在0.1MPa联合分解后,发现水合物沉积物膨胀率为176%。此外,观察到压力补偿后多孔介质上方水层的高度随着背压的降低而逐渐减小,最终在0.1MPa时消失。还发现水层的消失导致了异常记忆效应现象。沉积物的膨胀和沉降为水合物开采和地质安全提供了更好的参考。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dc7d/6812342/052fdfa82671/ao9b02497_0009.jpg

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