Application of low-pressure gas adsorption to nanopore structure characterisation of organic-rich lower Cambrian shale in the Upper Yangtze Platform, South China

被引:14
作者
Chen, L. [1 ,2 ,3 ]
Jiang, Z. [1 ,2 ]
Liu, K. [4 ]
Wang, P. [1 ,2 ]
Gao, F. [1 ,2 ]
Hu, T. [1 ,5 ]
机构
[1] China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
[2] China Univ Petr, Unconvent Nat Gas Inst, Beijing 102249, Peoples R China
[3] China Univ Petr, Unconvent Oil & Gas Cooperat Innovat Ctr, Beijing 102249, Peoples R China
[4] CSIRO Earth Sci & Resource Engn, Bentley, WA 6102, Australia
[5] China Univ Petr, Coll Geosci, Beijing 102249, Peoples R China
基金
中国国家自然科学基金;
关键词
shale gas; nanopore structure; low-pressure gas adsorption; pore-size distribution; lower Cambrian shale; Upper Yangtze Platform; MATURE POSIDONIA SHALE; PORE-SPACE MORPHOLOGY; THRUST-FOLD BELT; SICHUAN BASIN; METHANE ADSORPTION; BIB-SEM; THERMAL MATURITY; LACUSTRINE SHALE; PERMIAN SHALES; LONGMAXI SHALE;
D O I
10.1080/08120099.2017.1334705
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The pores in shales are mainly on a nanometer scale, and the pore-size distribution is vital with regard to the preservation and exploitation of shale gas. This study focuses on the organic-rich lower Cambrian black shale in the Upper Yangtze Platform, South China and investigates their TOC, mineralogical composition and nanopore structure. Low-pressure N-2 and CO2 adsorption experiments were conducted at 77.35K and 273.15K, respectively, and the nanopore structures were characterised by the modified Brunauer-Emmett-Teller, Dubinin-Radushkevich, t-plot, Barrett-Joyner-Halenda and density functional theory (DFT) methods. The results indicate the following. (1) The lower Cambrian shale has a high TOC content (1.77-7.23 wt%) and a high quartz content (27.7-51.6 vol%). The total specific surface area varies from 12.02 to 28.87 m(2)/g. Both the total specific surface area and quartz content are positively associated with the TOC content. (2) Shale samples with a higher TOC content have a greater number of micropores, resulting in more complicated nanopore structures. Micropore volumes/surface areas and non-micropore surface areas all increase with increasing TOC content, indicating that TOC is the key factor determining the nanopore structure of the lower Cambrian shale. (3) A combination of N-2 and CO2 adsorption provides the most suitable detection range (approximate to 0.3-60 nm) and is both highly reliable and accurate with regard to nanopore structure characterisation.
引用
收藏
页码:653 / 665
页数:13
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