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纳米多孔介质中凝聚态碳氢化合物的亚连续介质质量输运

Subcontinuum mass transport of condensed hydrocarbons in nanoporous media.

作者信息

Falk Kerstin, Coasne Benoit, Pellenq Roland, Ulm Franz-Josef, Bocquet Lydéric

机构信息

Department of Civil and Environmental Engineering and MultiScale Material Science for Energy and Environment UMI 3466 CNRS-MIT, Massachusetts Institute of Technology, 77 Massachusetts Avenue, Cambridge, Massachusetts 02139, USA.

出版信息

Nat Commun. 2015 Apr 22;6:6949. doi: 10.1038/ncomms7949.

DOI:10.1038/ncomms7949
PMID:25901931
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC4421809/
Abstract

Although hydrocarbon production from unconventional reservoirs, the so-called shale gas, has exploded recently, reliable predictions of resource availability and extraction are missing because conventional tools fail to account for their ultra-low permeability and complexity. Here, we use molecular simulation and statistical mechanics to show that continuum description--Darcy's law--fails to predict transport in shales nanoporous matrix (kerogen). The non-Darcy behaviour arises from strong adsorption in kerogen and the breakdown of hydrodynamics at the nanoscale, which contradict the assumption of viscous flow. Despite this complexity, all permeances collapse on a master curve with an unexpected dependence on alkane length. We rationalize this non-hydrodynamic behaviour using a molecular description capturing the scaling of permeance with alkane length and density. These results, which stress the need for a change of paradigm from classical descriptions to nanofluidic transport, have implications for shale gas but more generally for transport in nanoporous media.

摘要

尽管来自非常规储层的烃类生产,即所谓的页岩气,近年来呈爆发式增长,但由于传统工具无法考虑其超低渗透率和复杂性,因此缺乏对资源可用性和开采的可靠预测。在此,我们使用分子模拟和统计力学表明,连续介质描述——达西定律——无法预测页岩纳米多孔基质(干酪根)中的输运。非达西行为源于干酪根中的强吸附以及纳米尺度流体动力学的失效,这与粘性流动的假设相矛盾。尽管存在这种复杂性,但所有渗透率都汇聚在一条主曲线上,且对烷烃长度有意外的依赖性。我们使用一种分子描述来解释这种非流体动力学行为,该描述捕捉了渗透率与烷烃长度和密度的标度关系。这些结果强调了从经典描述向纳米流体输运转变范式的必要性,对页岩气有影响,但更普遍地对纳米多孔介质中的输运也有影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/f3d3e084f98a/ncomms7949-f6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/4eb210930546/ncomms7949-f1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/f555c8107cb3/ncomms7949-f2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/91e3c7446a72/ncomms7949-f3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/f3180795547b/ncomms7949-f4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/b8e153ddb3fd/ncomms7949-f5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/f3d3e084f98a/ncomms7949-f6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/4eb210930546/ncomms7949-f1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/f555c8107cb3/ncomms7949-f2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/91e3c7446a72/ncomms7949-f3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/f3180795547b/ncomms7949-f4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/b8e153ddb3fd/ncomms7949-f5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be26/4421809/f3d3e084f98a/ncomms7949-f6.jpg

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