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X-ray Microtomography to Quantify Morphological Sandstones Properties
Laboratory of Physics Applied to Soils and Environmental SciencesPires, Luiz Fernando; Melo, Mário Sérgio de; Laboratory of Physics Applied to Soils and Environmental SciencesBorges, Jaqueline Aparecida Ribaski; Heck, Richard John; Laboratory of Physics Applied to Soils and Environmental SciencesFacin, Paulo Cesar.
  • Laboratory of Physics Applied to Soils and Environmental SciencesPires, Luiz Fernando; State University of Ponta Grossa. Department of Physics. Laboratory of Physics Applied to Soils and Environmental SciencesPires, Luiz Fernando. Ponta Grossa. BR
  • Melo, Mário Sérgio de; State University of Ponta Grossa. Department of Geosciences. Ponta Grossa. BR
  • Laboratory of Physics Applied to Soils and Environmental SciencesBorges, Jaqueline Aparecida Ribaski; State University of Ponta Grossa. Department of Physics. Laboratory of Physics Applied to Soils and Environmental SciencesBorges, Jaqueline Aparecida Ribaski. Ponta Grossa. BR
  • Heck, Richard John; University of Guelph. School of Environmental Sciences. Guelph. CA
  • Laboratory of Physics Applied to Soils and Environmental SciencesFacin, Paulo Cesar; State University of Ponta Grossa. Department of Physics. Laboratory of Physics Applied to Soils and Environmental SciencesFacin, Paulo Cesar. Ponta Grossa. BR
Braz. arch. biol. technol ; 62: e19180125, 2019. tab, graf
Article in English | LILACS | ID: biblio-1011526
ABSTRACT
Abstract The sandstones of the Furnas Formation in the State of Paraná, south of Brazil, are located in regions with great importance due to the natural heritage found in the rocky forms and associated flora and fauna. This paper presents a detailed analysis of the internal structure of diverse sandstones of the Furnas Formation. X-ray microtomography allowed 3D characterization of the number, pore size and shape distributions of the sandstones. Images with voxel size of 603 µm3 were utilized to evaluate the sandstone's macroporosity. The main results obtained indicate that higher macroporosities were observed in coarser and some types of silicified sandstones. In general, fine sandstones were characterized by the largest number of pores. As a general conclusion the size and shape distribution of pores seem to have a variable relation with genetic factors as grain size and cement (siliceous and/or ferruginous).
Subject(s)


Full text: Available Index: LILACS (Americas) Main subject: Image Processing, Computer-Assisted / X-Ray Microtomography / Sand Language: English Journal: Braz. arch. biol. technol Journal subject: Biology Year: 2019 Type: Article Affiliation country: Brazil / Canada Institution/Affiliation country: State University of Ponta Grossa/BR / University of Guelph/CA

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Full text: Available Index: LILACS (Americas) Main subject: Image Processing, Computer-Assisted / X-Ray Microtomography / Sand Language: English Journal: Braz. arch. biol. technol Journal subject: Biology Year: 2019 Type: Article Affiliation country: Brazil / Canada Institution/Affiliation country: State University of Ponta Grossa/BR / University of Guelph/CA