Fractal dimensionality of pore and grain volume of a siliciclastic marine sand
Physics and Astronomy
Three-dimensional (3D) spatial distributions of pore and grain volumes were determined from high-resolution computer tomography (CT) images of resin-impregnated marine sands. Using a linear gradient extrapolation method, cubic three-dimensional samples were constructed from two-dimensional CT images. Image porosity (0.37) was found to be consistent with the estimate of porosity by water weight loss technique (0.36). Scaling of the pore volume (V-p) with the linear size (L), V similar to L-D provides the fractal dimensionalities of the pore volume (D = 2.74 +/- 0.02) and grain volume (D = 2.90 +/- 0.02) typical for sedimentary materials.
INTERNATIONAL JOURNAL OF MODERN PHYSICS C
Pandey, R. B.,
(2000). Fractal dimensionality of pore and grain volume of a siliciclastic marine sand. INTERNATIONAL JOURNAL OF MODERN PHYSICS C, 11(8), 1555-1559.
Available at: http://aquila.usm.edu/fac_pubs/4037