Visualization and quantification of capillary drainage in the pore space of laminated sandstone by a porous plate method using differential imaging X‐ray microtomography

The experimental determination of capillary pressure drainage curves at the pore scale is of vital importance for the mapping of reservoir fluid distribution. To fully characterize capillary drainage in a complex pore space, we design a differential imaging‐based porous plate (DIPP) method using X‐ray microtomography. For an exemplar mm‐scale laminated sandstone microcore with a porous plate, we quantify the displacement from resolvable macropores and subresolution micropores. Nitrogen (N2) was injected as the nonwetting phase at a constant pressure while the porous plate prevented its escape. The measured porosity and capillary pressure at the imaged saturations agree well with helium measurements and experiments on larger core samples, while providing a pore‐scale explanation of the fluid distribution. We observed that the majority of the brine was displaced by N2in macropores at low capillary pressures, followed by a further brine displacement in micropores when capillary pressure increases. Furthermore, we were able to discern that brine predominantly remained within the subresolution micropores, such as regions of fine lamination. The capillary pressure curve for pressures ranging from 0 to 1151 kPa is provided from the image analysis compares well with the conventional porous plate method for a cm‐scale core but was conducted over a period of 10 days rather than up to few months with the conventional porous plate method. Overall, we demonstrate the capability of our method to provide quantitative information on two‐phase saturation in heterogeneous core samples for a wide range of capillary pressures even at scales smaller than the micro‐CT resolution. A differential imaging‐based porous plate method is devised to visualize brine distribution during capillary drainage with micro‐CTThe sequence of capillary‐controlled pore filling in a laminated sandstone is determined with a pore‐scale interpretation of displacementThe capillary pressure measurements agree with porous plate experiments on a larger core but with much shorter experimental time