Effect of Initial Water Saturation on Spontaneous Water Imbibition

Abstract

Abstract The effect of initial water saturation on gas recovery by cocurrent spontaneous water imbibition and imbibition rate was investigated both theoretically and experimentally. Equations correlating initial water saturation, gas recovery, imbibition rate, rock/fluid properties, and imbibition time were derived and used to conduct the theoretical analysis. These equations foresee that gas recovery and imbibition rate could increase, remain unchanged, or decrease with increase in initial water saturation, depending on rock properties, the quantity of residual gas saturation, the range of initial water saturation, and the units used in the definitions of gas recovery and imbibition rate. The theoretical predictions were verified experimentally by conducting spontaneous water imbibition at five different initial water saturations, ranging from 0 to about 50%. Water phase relative permeabilities and capillary pressures were calculated using the experimental data of spontaneous imbibition. The effects of initial water saturation on residual gas saturation, water phase relative permeability, and capillary pressure were also studied experimentally. The results in different rocks were compared. It was found that the residual gas saturation by spontaneous imbibition in a fired Berea sandstone sample (clay was removed by firing) was lower than in a natural Berea sandstone sample (clay was not removed). This demonstrates significant wettability alteration caused by firing. In other words, there may be significant wettability differences among different gas-liquid-rock systems.