4.3 Article

Extraction of organic compounds from representative shales and the effect on porosity

Journal

JOURNAL OF NATURAL GAS SCIENCE AND ENGINEERING
Volume 35, Issue -, Pages 646-660

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.jngse.2016.08.064

Keywords

Small angle neutron scattering; Solvent extraction from shales; Eagle Ford shale; Marcellus shale; Pore size distribution

Funding

  1. US Department of Energy through the program Research Partnership to Secure Energy for America
  2. US Department of Energy through the program Office of Science, Scientific User Facilities Program
  3. US Department of Energy through the program Laboratory Directed Research and Development of Oak Ridge National Laboratory
  4. University of Tennessee through the Bredesen Center
  5. Chesapeake Energy

Ask authors/readers for more resources

As the location and accessibility of hydrocarbons is key to understanding and improving the extractability of hydrocarbons in hydraulic fracturing, this study is an attempt to understand how native organics are distributed with respect to pore size to determine the relationship between hydrocarbon chemistry and pore structure in shales. First, selected shale cores from the Eagle Ford and Marcellus formations were subjected to pyrolysis gas chromatography (GC), thermogravimetric analysis, and organic solvent extraction with the resulting effluent analyzed by GC-mass spectrometry (MS). Organics representing the oil and gas fraction (0.1-1 wt %) were observed by GC-MS. For most of the samples, the amount of native organic extracted directly related to the percentage of clay in the shale. The porosity and pore size distribution (0.95 nm-135 mu m) in the Eagle Ford and Marcellus shales was measured before and after solvent extraction using small angle neutron scattering (SANS). An unconventional method was used to quantify the background from incoherent scattering as the Porod transformation obscures the Bragg peak from the clay minerals. The change in porosity from SANS is indicative of the extraction or breakdown of higher molecular weight bitumen with high C/H ratios (asphaltenes and resins). This is mostly likely attributed to complete dissolution or migration of asphaltenes and resins. These longer carbon chain lengths, C30-C40, were observed by pyrolysis GC, but either were too heavy to be analyzed in the extracts by GC-MS or were not effectively leached into the organic solvents. Thus, experimental limitations meant that the amount of extractable material could not be directly correlated to the changes in porosity measured by SANS. However, the observable porosity generally increased with solvent extraction. A decrease in porosity after extraction as observed in a shale with high clay content and low maturity was attributed to swelling of pores with solvent uptake or migration of resins and asphaltenes. (C) 2016 Elsevier B.V. All rights reserved.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.3
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available