TY - JOUR
T1 - A three-dimensional reconstruction of coal microstructure using the Cryo-FIB-SEM technique
AU - Zakrzewski, Marcin
AU - Schertel, Andreas
AU - Brus, Grzegorz
AU - Wagner, Marian
AU - Sciazko, Anna
AU - Komatsu, Yosuke
AU - Kimijima, Shinji
AU - Kaneko, Shozo
AU - Szmyd, Janusz S.
N1 - Funding Information:
The present study was financially supported by the Japan Coal Energy Center ( JCOAL ), the Polish National Centre for Research and Development (NCBR Project: I_POL-JAP, SSD-4-LRC) and also partially supported by AGH University of Science and Technology (Grant AGH No. 16.16.210.476 ). We would like to thank Saskia Mimietz-Oeckler and Andreas Halladay, Leica Microsystems GmbH, Vienna, Austria for their technical support. The authors also greatly acknowledge Mr. Wojciech Szczuraszek, ZEISS Group, Microscopy Division Poznań, Poland for making the arrangements of this cooperative work.
Funding Information:
The present study was financially supported by the Japan Coal Energy Center (JCOAL), the Polish National Centre for Research and Development (NCBR Project: I_POL-JAP, SSD-4-LRC) and also partially supported by AGH University of Science and Technology (Grant AGH No. 16.16.210.476). We would like to thank Saskia Mimietz-Oeckler and Andreas Halladay, Leica Microsystems GmbH, Vienna, Austria for their technical support. The authors also greatly acknowledge Mr. Wojciech Szczuraszek, ZEISS Group, Microscopy Division Pozna?, Poland for making the arrangements of this cooperative work.
Publisher Copyright:
© 2020 The Authors
PY - 2020/9/1
Y1 - 2020/9/1
N2 - Two basic homogeneous lithotypes, defined as elementary coal layers, within the seam of lignite can be distinguished: xylitic and detritic coal. As each of them exhibits various features, including structure, mechanical, technological properties, and chemical ash composition, the share of lithotypes within a lignite deposit provides important information regarding the applicability of this fuel. This study describes a unique three-dimensional reconstruction of a lignite microstructure using scanning electron microscopy (SEM) to acquire images of subsequent coal cross-sections which are exposed by focused ion beam (FIB) milling at cryogenic temperatures. Because of the organic origin and high moisture content, the fully hydrated lignite sample was frozen in nitrogen slush for the SEM observation in its frozen native state in order to avoid dehydration and other sample modifications. The acquired data cube contained distinguished petrographic phases, identified with coaly macerals of xylitic and detritic coal along with the fragment of the gelified leaf tissue, typical for ortho-lignite structure. The 3D reconstruction and phase segmentation process was performed using the Avizo software to constitute a cuboid model with an edge length of ca. 10 µm. Lignite exhibits low local uniformity, therefore to draw generally valid conclusions, a statistical relevant number of similar three dimensional reconstructions at representative locations for the different lithotypical and petrographic coal compositions within the analysed fragment would be demanded.
AB - Two basic homogeneous lithotypes, defined as elementary coal layers, within the seam of lignite can be distinguished: xylitic and detritic coal. As each of them exhibits various features, including structure, mechanical, technological properties, and chemical ash composition, the share of lithotypes within a lignite deposit provides important information regarding the applicability of this fuel. This study describes a unique three-dimensional reconstruction of a lignite microstructure using scanning electron microscopy (SEM) to acquire images of subsequent coal cross-sections which are exposed by focused ion beam (FIB) milling at cryogenic temperatures. Because of the organic origin and high moisture content, the fully hydrated lignite sample was frozen in nitrogen slush for the SEM observation in its frozen native state in order to avoid dehydration and other sample modifications. The acquired data cube contained distinguished petrographic phases, identified with coaly macerals of xylitic and detritic coal along with the fragment of the gelified leaf tissue, typical for ortho-lignite structure. The 3D reconstruction and phase segmentation process was performed using the Avizo software to constitute a cuboid model with an edge length of ca. 10 µm. Lignite exhibits low local uniformity, therefore to draw generally valid conclusions, a statistical relevant number of similar three dimensional reconstructions at representative locations for the different lithotypical and petrographic coal compositions within the analysed fragment would be demanded.
KW - 3D coal microstructure reconstruction
KW - Brown coal
KW - Detritic coal
KW - Focused ion beam
KW - Lignite
KW - Low-rank coal
KW - Xylitic coal
KW - cryo-FIB-SEM tomography
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U2 - 10.1016/j.fuel.2020.117919
DO - 10.1016/j.fuel.2020.117919
M3 - Article
AN - SCOPUS:85084232562
SN - 0016-2361
VL - 275
JO - Fuel
JF - Fuel
M1 - 117919
ER -