TY - JOUR
T1 - Resolution dependence of petrophysical parameters derived from X-ray tomography of chalk
AU - Müter, Dirk
AU - Sørensen, Henning Osholm
AU - Jha, Diwaker
AU - Harti, Ralph Patrick
AU - Dalby, Kim Nicole
AU - Suhonen, H.
AU - Feidenhans'l, Robert Krarup
AU - Engstrøm, F.
AU - Stipp, Susan Louise Svane
PY - 2014/7/28
Y1 - 2014/7/28
N2 - X-ray computed tomography data from chalk drill cuttings were taken over a series of voxel dimensions, ranging from 320 to 25 nm. From these data sets, standard petrophysical parameters (porosity, surface area, and permeability) were derived and we examined the effect of the voxel dimension (i.e., image resolution) on these properties. We found that for the higher voxel dimensions, they are severely over or underestimated, whereas for 50 and 25 nm voxel dimension, the resulting values (5%-30% porosity, 0.2-2 m2/g specific surface area, and 0.06-0.34 mD permeability) are within the expected range for this type of rock. We compared our results to macroscopic measurements and in the case of surface area, also to measurements using the Brunauer-Emmett-Teller (BET) method and found that independent of the degree of compaction, the results from tomography amount to about 30% of the BET method. Finally, we concluded that at 25 nm voxel dimension, the essential features of the nanoscopic pore network in chalk are captured but better resolution is still needed to derive surface area.
AB - X-ray computed tomography data from chalk drill cuttings were taken over a series of voxel dimensions, ranging from 320 to 25 nm. From these data sets, standard petrophysical parameters (porosity, surface area, and permeability) were derived and we examined the effect of the voxel dimension (i.e., image resolution) on these properties. We found that for the higher voxel dimensions, they are severely over or underestimated, whereas for 50 and 25 nm voxel dimension, the resulting values (5%-30% porosity, 0.2-2 m2/g specific surface area, and 0.06-0.34 mD permeability) are within the expected range for this type of rock. We compared our results to macroscopic measurements and in the case of surface area, also to measurements using the Brunauer-Emmett-Teller (BET) method and found that independent of the degree of compaction, the results from tomography amount to about 30% of the BET method. Finally, we concluded that at 25 nm voxel dimension, the essential features of the nanoscopic pore network in chalk are captured but better resolution is still needed to derive surface area.
U2 - 10.1063/1.4891965
DO - 10.1063/1.4891965
M3 - Journal article
SN - 0003-6951
VL - 105
JO - Applied Physics Letters
JF - Applied Physics Letters
M1 - 043108
ER -