An evaluation is made of the imbibition potential of two different cha
lk facies from outcrops in England and Denmark. Both chalk facies have
low permeability, moderate to high porosity, and comparable low insol
uble residues (< 5%), but different texture, depositional origin and d
iagenetic history. Spontaneous imbibition experiments were carried out
on plugs with low initial water saturation and North Sea dead oil. Di
stinctly different production rates and production plateaus were obser
ved for the two chalk facies. Careful investigations of the rock frame
work and pore system of the sample material form the basis for a theor
etical description of wettability alteration and possible imbibition p
rocesses in the two chalks. The theoretical descriptions are used to r
ationalize the results from the spontaneous imbibition experiments. Th
e results suggest that by knowing lithology, depositional history and
degree of diagenetic alteration a relative potential of spontaneous im
bibition in different chalk facies may be elucidated.