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Pore space relevant for gas permeability in Opalinus clay: Statistical analysis of homogeneity, percolation, and representative volume element
Author(s) -
Keller Lukas M.,
Holzer Lorenz,
Schuetz Philipp,
Gasser Philippe
Publication year - 2013
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.983
H-Index - 232
eISSN - 2169-9356
pISSN - 2169-9313
DOI - 10.1002/jgrb.50228
Subject(s) - porosity , percolation threshold , materials science , microstructure , homogeneity (statistics) , facies , mineralogy , anisotropy , percolation theory , representative elementary volume , composite material , geology , electrical resistivity and conductivity , optics , chemistry , conductivity , physics , mathematics , geomorphology , statistics , quantum mechanics , structural basin
Local porosity theory in combination with percolation theory was applied to shale microstructures that were reconstructed on the basis of focused ion beam nanotomography and scanning transmission electron microscopy. This allowed characterizing pore microstructures in Opalinus clay with length scales on the order of tens of microns. In a sample from the sandy facies (with low clay content), the fraction of “larger” pores ϕ (radii~ > 15 nm) = 0.076 is substantially higher than that in the shaley facies (with a higher clay content), where ϕ (radii~ > 15 nm) = 0.015. The resolved porosity possesses a certain degree of homogeneity, and the representative volume element (RVE) of porosity can be determined in terms of a given relative error on porosity. For example, if we accept a relative error of 10%, the RVE is on the scale of a few hundreds of microns. Both pore microstructures from sandy and shaley facies show anisotropic characteristics with respect to connectivity and percolation threshold. Using finite scaling, we found percolation thresholds with critical porosities ϕ c,b = 0.04–0.12 parallel to bedding and ϕ c ,perp = 0.11–0.19 perpendicular to bedding. The resolved porosity of the sandy facies (low clay content) is close to the percolation threshold, whereas the porosity of the shaley facies (high clay content) is below the percolation threshold. The porosity in carbonate layers is around ϕ = 0.027, and the pore size is substantially larger when compared to the pores in the clay matrix. In the analyzed sample, pores in carbonate layers are poorly connected.