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由空气和二氧化碳驱动的天然气水合物无损开采

Nondestructive natural gas hydrate recovery driven by air and carbon dioxide.

作者信息

Kang Hyery, Koh Dong-Yeun, Lee Huen

机构信息

Department of Chemical and Biomolecular Engineering, Korea Advanced Institute of Science and Technology, 291 Daehak-ro, Guseong-dong, Yuseong-gu, Daejeon 305-701, South Korea.

1] Department of Chemical and Biomolecular Engineering, Korea Advanced Institute of Science and Technology, 291 Daehak-ro, Guseong-dong, Yuseong-gu, Daejeon 305-701, South Korea [2] Graduate School of EEWS, Korea Advanced Institute of Science and Technology, 291 Daehak-ro, Guseong-dong, Yuseong-gu, Daejeon 305-701, South Korea.

出版信息

Sci Rep. 2014 Oct 14;4:6616. doi: 10.1038/srep06616.

Abstract

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.

摘要

当前用于生产天然气水合物(NGH)的技术,包括热刺激、减压和注入抑制剂,引发了人们对意外后果的担忧。灾难性边坡失稳和海洋生态系统破坏的可能性仍然是安全开采NGH的严峻挑战。作为一种潜在方法,本文提出了通过甲烷释放(NGH分解)和CH₄-空气或CH₄-CO₂/空气置换的同步机制,从渗透性海洋沉积物中空气驱动回收NGH。空气扩散进入并穿透NGH,并在其表面形成气固两相之间的边界。然后自发熔化继续进行,直到随着NGH消耗的持续,两相中的化学势变得相等,并且在任意点发生自我调节的CH4-空气置换。我们观察到在NGH储层中存在形成分解和置换机制边界的临界甲烷浓度。此外,当添加CO₂时,我们观察到在NGH中发生了非常强烈、稳定的自我调节交换过程(CH₄被CO₂/空气取代;以下简称CH₄-CO₂/空气)。无论注入条件或地热梯度如何,所提出的过程对大多数全球天然气水合物储层都将有效。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e9a9/4196106/a4cc63944d1f/srep06616-f1.jpg

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