Spontaneous Imbibition and Drainage of Water in a Thin Porous Layer: Experiments and Modeling

The typical characteristic of a thin porous layer is that its thickness is much smaller than its in-plane dimensions. This often leads to physical behaviors that are different from three-dimensional porous media. The classical Richards equation is insufficient to simulate many flow conditions in thin porous media. Here, we have provided an alternative approach by accounting for the dynamic capillarity effect. In this study, we have presented a set of one-dimensional in-plane imbibition and subsequent drainage experiments in a thin fibrous layer. The X-ray transmission method was used to measure saturation distributions along the fibrous sample. We simulated the experimental results using Richards equation either with classical capillary equation or with a so-called dynamic capillarity term. We have found that the standard Richards equation was not able to simulate the experimental results, and the dynamic capillarity effect should be taken into account in order to model the spontaneous imbibition. The experimental data presented here may also be used by other researchers to validate their models. Article Highlights We have presented a set of one-dimensional in-plane imbibition and subsequent drainage experiments in a thin fibrous layer. The experimental data were simulated using the Richards equation either with classical capillary equation or with a so-call dynamic capillarity term. The dynamic capillarity effect should be taken into account in order to model the spontaneous imbibition.