The numerical modelling of transport phenomena
in porous media often requires a compromise between grid
precision and the accuracy of simulation results. This study demonstrates
the impact of errors on the accuracy of the reproduction
of the actual pore space by the numerical grid on the estimated
values of the saturated water conductivity. Four types of computational
grids with varying levels of complexity were prepared for
each of the 12 tomographic images of the porous specimens. The
specific surfaces and total porosities were calculated for each of
the meshes and compared with those parameters calculated for
binarized tomographic images. Simulations of steady flow were
performed on the computational grids, and the saturated water
conductivity values were calculated. It has been shown that an
insufficiently accurate mesh only reproduces the largest pore
spaces in the analysed sample, which most often leads to an
underestimation of the water conductivity coefficient. The following
criterion for the optimal accuracy of the computational grid is
proposed, it is based on the voxel size of the tomographic images
of the porous media: the minimum size of the cell in the mesh
used for simulations has to be at most two times the size of the
voxel used in the tomographic scans of the porous medium.
Ta witryna wykorzystuje pliki cookies do przechowywania informacji na Twoim komputerze. Pliki cookies stosujemy w celu świadczenia usług na najwyższym poziomie, w tym w sposób dostosowany do indywidualnych potrzeb. Korzystanie z witryny bez zmiany ustawień dotyczących cookies oznacza, że będą one zamieszczane w Twoim komputerze. W każdym momencie możesz dokonać zmiany ustawień dotyczących cookies
Informacja
SZANOWNI CZYTELNICY!
UPRZEJMIE INFORMUJEMY, ŻE BIBLIOTEKA FUNKCJONUJE W NASTĘPUJĄCYCH GODZINACH:
Wypożyczalnia i Czytelnia Główna: poniedziałek – piątek od 9.00 do 19.00