4.7 Article

Nanopore structure characterization for organic-rich shale using the non-local-density functional theory by a combination of N2 and CO2 adsorption

Journal

MICROPOROUS AND MESOPOROUS MATERIALS
Volume 227, Issue -, Pages 88-94

Publisher

ELSEVIER
DOI: 10.1016/j.micromeso.2016.02.050

Keywords

Nanopore structure; Characterization; Organic-rich shale; Low-pressure gas adsorption; NLDFT method

Funding

  1. Special Fund for Strategic Priority Research Program of the Chinese Academy of Sciences (Class B) [XDB10010500]
  2. Chinese Ministry of Land and Resources [Zi[2014]03-030-003]

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Low-pressure gas adsorption is widely used for pore size analysis of porous materials, and has been employed to characterize pore systems in shale. However, the complexity of shale pore structures means that different methods and models may lead to distinct interprets for adsorption data. Non-local-density functional theory (NLDFT) analysis based on N-2 and CO2 composited adsorption isotherms is used here to investigate the pore structure of nanopores in marine organic-rich shale and compare with the results from some conventional methods in this paper. The results indicate that (1) The N-2 adsorption isotherms of organic-rich shale are a composite of Types I(b), II, and IV(a), according to the IUPAC (2015) classification of physisorption isotherms. The hysteresis loops show similar shapes to Type H2(a). Delayed capillary condensation is observed in the adsorption isotherms, and the desorption step is shifted to the lower relative pressure of similar to 0.45 characteristic of the cavitation mechanism, indicating ink-bottle pores with narrow necks. The CO2 adsorption isotherms are similar to Type I(b), but appear to increase without limit when p/p(0) = 0.03 because of the occurrence of meso-and macropores in the shales. (2) NLDFT method based on N-2 and CO2 composited adsorption isotherms is the most suitable and accurate method for using gas physisorption when considering the entire size distribution of nanopores, which allows a suitable range of critical pore sizes (similar to 033-100 nm) to be explored. (C) 2016 Elsevier Inc. All rights reserved.

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