Fast mass transport of oil and supercritical carbon dioxide through organic nanopores in shale

被引:126
|
作者
Wang, Sen [1 ,2 ]
Javadpour, Farzam [2 ]
Feng, Qihong [1 ]
机构
[1] China Univ Petr East China, Sch Petr Engn, Qingdao, Peoples R China
[2] Univ Texas Austin, Bur Econ Geol, Jackson Sch Geosci, Austin, TX 78713 USA
基金
中国国家自然科学基金;
关键词
Shale; Organic matter; Supercritical; Carbon dioxide; Nanopore; Slip length; MOLECULAR-DYNAMICS SIMULATIONS; GAS-FLOW; METHANE ADSORPTION; FLUID TRANSPORT; PERMEABILITY; NETWORK; ALKANE; CO2; HYDRODYNAMICS; WETTABILITY;
D O I
10.1016/j.fuel.2016.05.057
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Hydrocarbon production from shale has grown dramatically in North America, and has the potential to do so globally. Nanoporous organic matter is probably the dominant mode of porosity occurrence in productive shale systems, but the physics of liquid transport through organic-hosted pores is still ambiguous. In the present work, molecular dynamics simulations were conducted to study the static properties and pressure-driven flow behavior of pure liquid hydrocarbons (octane) and supercritical carbon dioxide (scCO(2)) confined in slit-shaped organic nanopores. Carbonaceous slits having apertures ranging from 1.5 to 11.2 nm were explored. A range of thermodynamic conditions, corresponding to the sedimentary reservoirs, were examined. Equilibrium molecular dynamics (EMD) enabled us to determine the density profile, from which we observed the layering structure of confined fluid and the preferential adsorption of scCO(2) relative to C8H18 and CH4. As the pore size increases, the structure of the adsorbed phase transforms from a single-file chain to four and three dense monolayers for C8H18 and scCO(2), respectively. Then we calculated, using nonequilibrium molecular dynamics (NEMD), their velocity profiles and studied the hydrodynamics under a pressure gradient. We found that the velocity profiles in an organic slit tend to be pluglike, which deviates significantly from the parabolic profile in inorganic nanopores, and the flow exceeds predictions of the no-slip Poiseuille equation by 1-3 orders of magnitude. We proposed two models to characterize the flow behavior, each of which can be integrated into a bottom-up framework to mimic fluid transport in shale and estimate the apparent liquid permeability. The parameters in our models, slip length and apparent viscosity, are exponentially dependent on driving force, pore size, and temperature. Our results, which highlight the need for taking into account the different nature of organic matter and inorganic minerals in flow modeling, will shed light on the development of shale resources and, more generally, mass transfer in nanoporous materials. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:741 / 758
页数:18
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