ACTA

Preliminary Investigations of Elemental Content, Microporosity, and Specific Surface Area of Porous Rocks Using PIXE and X-ray Microtomography Techniques

J. Bielecki^a, S. Bożek^{a, b}, E. Dutkiewicz^a, R. Hajduk^a, J. Jarzyna^c, J. Lekki^a, T. Pieprzyca^a, Z. Stachura^a, Z. Szklarz^a and W.M. Kwiatek^a
^aThe Henryk Niewodniczański Institute of Nuclear Physics, Polish Academy of Sciences, E. Radzikowskiego 152, 31-342 Kraków, Poland
^bMedical College, Department of Pharmacokinetics and Physical Pharmacy, The Jagiellonian University, Medyczna 9, 30-688 Kraków, Poland
^cFaculty of Geology, Geophysics and Environment Protection, AGH University of Science and Technology, al. A. Mickiewicza 30, 30-059 Kraków, Poland

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Determination of physical properties of porous geological materials is of great importance for oil industry. The knowledge of rocks properties is usually obtained from porosity studies such as pore size distribution, specific surface area determination, and hydrodynamic permeability calculations. This study describes determination of elemental composition and measurements of the particular physical properties of geological samples (porous sandstone rocks) by means of the nuclear and X-ray microprobes at the Institute of Nuclear Physics, Polish Academy of Sciences in Kraków, Poland. The special emphasis has been put on the computed microtomography method. Measurements have been carried out in close cooperation with Department of Geophysics, FGGEP AGH in Kraków, Poland. Chemical composition of the Rotliegend sandstone rock samples (few millimeters diameter), extracted from a borehole at 2679.6 m, 2741.4 m and 2742.4 m depth have been investigated using the 2.2 MeV proton beam (proton induced X-ray emission technique). Next, measurements of the porosity and the specific surface area of the pore space have been carried out using the X-ray microtomography technique. Basing on microtomographic data obtained with the high spatial resolution, simulations of the fluid dynamic in the void space of porous media have been carried out. Lattice Boltzmann method in the 3DQ19 geometrical model has been used in order to predict the hydraulic permeability of the media. In order to avoid viscosity-permeability dependence the multiple-relaxation-time model with half-way bounce back boundary conditions has been used. Computing power-consuming processing has been performed with the use of modern grid infrastructure.

DOI: 10.12693/APhysPolA.121.474
PACS numbers: 81.70.Tx, 91.65.-n, 47.56.+r