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AAPG Bulletin· 2012Q1

Microstructural investigation of gas shales in two and three dimensions using nanometer-scale resolution imaging

Mark E. Curtis, Carl Sondergeld, Raymond Ambrose, Chandra Rai

Short summary

Gas shales exhibit highly variable microstructures, with kerogen volumes ranging from 0-90% and pore volumes from 0.2-2.3%, revealed by 3D nanometer-scale imaging.

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Key points

  • Gas shale microstructures are complex and vary significantly across different formations.
  • Key components identified include clay, carbonate, quartz, pyrite, and kerogen.
  • 3D reconstructions from FIB-SEM imaging quantified kerogen volumes (0-90%) and pore volumes (0.2-2.3%).
  • Pore-size distributions show that smaller pores (approx. 3 nm radii) are most numerous but not necessarily the largest volumetric contributors.

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Abstract

Abstract The microstructure of gas shale samples from nine different formations has been investigated using a combination of focused ion beam (FIB) milling and scanning electron microscopy (SEM). Backscattered electron (BSE) images of FIB cross sectioned shale surfaces show a complex microstructure with variations observed among the formations. Energy dispersive spectroscopy of the shale cross sections indicates that clay, carbonate, quartz, pyrite, and kerogen are the most prevalent components. In the BSE images, areas of kerogen are observed interspersed with the inorganic grains. Pores are observed in both the kerogen and inorganic matrix with the size, shape, and number of pores varying among the shale samples. By using FIB milling and SEM imaging sequentially and repetitively, three-dimensional (3-D) data sets of SEM images have been generated for each of the shale samples. Three-dimensional volumes of the shales are reconstructed from these images. By setting thresholds on the gray scale, the kerogen and pore networks are segmented out and visualized in the reconstructed shale volumes. Estimates of kerogen and pore volume percentages of the reconstructed shale volumes have been made and range from 0 to 90.0% for the kerogen and 0.2 to 2.3% for pores. Estimates of pore-size distributions suggest that although pores with radii of approximately 3 nm dominate in number, they do not necessarily dominate in total volumetric contribution. Scanning electron microscopy images and 3-D reconstructions reinforce the facts that shales are quite different and that their microstructures are highly variable and complex.

The authors' abstract, as published at the source. AAPG Bulletin, 2012 · DOI ↗

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Field: Mechanics of Materials

Mechanics of MaterialsEngineering