Knowledge of a shale pore structure is essential and
critical to
estimating gas storage and predicting gas production. Shale is a heterogeneous
rock in terms of its composition and consists of organic matter (OM)
and inorganic matter (IOM). Due to their difference in surface wettability
and affinity to methane, the quantitative determination of apparent
pore size distributions (APSDs) of OM and IOM as well as their contributions
to the Barrett–Joyner–Halenda (BJH) pore volume is a
very important task, but it is still a puzzling issue, especially
considering the occurrence of water under the in situ condition. In
this work, combining the water adsorption and low-pressure N2 adsorption–desorption experiments, we obtained the APSDs
of dry and moist shale and clay samples, where the latter is assumed
to the representative of IOM. Then, given the water distribution related
to the surface wettability, a novel approach is proposed to quantitatively
determine the APSDs of OM and IOM as well as their contributions to
the BJH pore volume of shale under dry and in situ conditions. Our
experimental results demonstrated that small nanopores (<5 nm)
presented under a dry condition may be absent on the clay APSD curves
under a moist condition due to the capillary condensation effect but
are still shown on the shale APSD curves due to the existence of hydrophobic
OM nanopores. Under a dry condition, the APSDs of OM and IOM for our
samples show that OM is rich in small nanopores (i.e., 3–50
nm) while IOM pores show a wider range of size (i.e., 3–200
nm), and the contribution of OM-hosted volume to BJH pore volume is
26.7% and 20%. While under a moist condition (RH = 98%), IOM pore
volumes of 26% and 20% are occupied by water molecules, and the OM-hosted
proportion increases to 36% and 26%, respectively. This study proposed
a significant approach to deeply characterize shale pore structure,
which provides a more solid and reliable foundation for the shale
gas storage estimation and well performance prediction.