Most flooding experiments in sandstone cores are carried out either in
almost homogeneous samples or in core samples of uncertain heterogene
ity. As a result, the interaction of small-scale sedimentary heterogen
eity with the fluid mechanics of water-oil displacement cannot be adeq
uately understood or quantified. Because most elastic sediments show s
ome degree of lamination, this might be expected to have a significant
influence on both oil displacement efficiency and residual/remaining
oil saturation. This paper reports results from low-rate, drainage/imb
ibition floods in a 20 x 10 x 1-cm water-wet slab of cross-laminated h
eterogeneous eolian sandstone. The distribution of porosity, permeabil
ity, initial water saturation and residual oil saturation were monitor
ed with computerized-tomography (CT) scanning techniques. The low-rate
imbibition floods show that between 30% and 55% of original oil may b
e trapped in isolated high-permeability lamina. This work shows the im
portance of recognizing the role of core-scale heterogeneity in the la
boratory measurement of waterflood behavior (i.e., the interaction of
capillary forces with rock structure, particularly lamination). The pr
actice of performing high-rate floods on rock samples assumed to be ho
mogeneous is unwise and can lead to erroneous conclusions. The results
of this work have major implications for (1) two-phase petrophysical
measurements; (2) assessment of residual/ remaining oil, and (3) multi
phase-flow scaleup.