This
study explores imbibition dynamics and flowback of fracturing
fluids in Penglaizhen sandstones by imbibition experiment and nuclear
magnetic resonance analysis. A gas–water system was considered
and samples were subjected to different boundary conditions and fully
immersed in the wetting phase for imbibition. A close range of the
pore radius was observed between 0.1 nm and 9.3 μm for all samples.
Basic features of the imbibition phases were represented by the imbibition
profile, and imbibition parameters were quantified in terms of gas
recovery, imbibition capacity, imbibition index and pore connectivity,
diffusion ability, and imbibition potential under the respective boundary
conditions. The study reveals that capillary imbibition (mainly in
all-face-open (AFO) and two-end-closed (TEC)) and diffusion imbibition
(mainly in two-end-open (TEO) and one-end-open (OEO)) are the major
mechanisms by which fracture fluids flow into the formation matrix.
There is high gas recovery in all samples (>79%), which can be
attributed
to the high water-wet nature of the samples, while the residual gas
saturation is very low with the highest value in OEO at 0.17 and the
lowest in AFO at 0.01. The strong capillary force in AFO and TEC boundary
conditions is the key factor for higher gas recovery than TEO and
OEO samples. However, the low diffusion ability of AFO and TEC samples
depict a low gas displacement effect. On the other hand, TEO and OEO
boundary conditions show an increased gas displacement effect through
increased diffusion ability. The imbibition index (which represents
pore connection) and imbibition potential from the highest to the
lowest also correspond to the diffusion ability from the highest to
the lowest.