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Nondestructive natural gas hydrate recovery driven by air and carbon dioxide

机译:由空气和二氧化碳驱动的无损天然气水合物回收

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摘要

Current technologies for production of natural gas hydrates (NGH), which include thermal stimulation, depressurization and inhibitor injection, have raised concerns over unintended consequences. The possibility of catastrophic slope failure and marine ecosystem damage remain serious challenges to safe NGH production. As a potential approach, this paper presents air-driven NGH recovery from permeable marine sediments induced by simultaneous mechanisms for methane liberation (NGH decomposition) and CH4-air or CH4-CO2/air replacement. Air is diffused into and penetrates NGH and, on its surface, forms a boundary between the gas and solid phases. Then spontaneous melting proceeds until the chemical potentials become equal in both phases as NGH depletion continues and self-regulated CH4-air replacement occurs over an arbitrary point. We observed the existence of critical methane concentration forming the boundary between decomposition and replacement mechanisms in the NGH reservoirs. Furthermore, when CO2 was added, we observed a very strong, stable, self-regulating process of exchange (CH4 replaced by CO2/air; hereafter CH4-CO2/air) occurring in the NGH. The proposed process will work well for most global gas hydrate reservoirs, regardless of the injection conditions or geothermal gradient.
机译:用于生产天然气水合物(NGH)的当前技术,包括热增产,降压和抑制剂注入,引起了人们对意想不到的后果的担忧。灾难性的边坡破坏和海洋生态系统破坏的可能性仍然是安全NGH生产的严峻挑战。作为一种可能的方法,本文介绍了甲烷释放(NGH分解)和CH4-空气或CH4-CO2 /空气置换的同时机理,从可渗透的海洋沉积物中进行空气驱动的NGH回收。空气扩散并渗透到NGH中,并在其表面上形成气相和固相之间的边界。然后进行自发熔化,直到随着NGH耗尽继续在两相中的化学势变得相等,并且在任意点进行自调节的CH4空气置换。我们观察到了NGH储层中形成分解和置换机制之间边界的临界甲烷浓度。此外,当添加二氧化碳时,我们观察到NGH中发生了非常强烈,稳定,自我调节的交换过程(CH4替换为CO2 /空气;此后称为CH4-CO2 /空气)。无论注入条件或地热梯度如何,所提出的方法对于大多数全球天然气水合物储层都将很好地工作。

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