A significant amount of foreign fluid is kept in the
marine shale
reservoirs after hydraulic fracturing. The water distribution characteristics
in the pore space are quite complex because of the shale’s
significant inhomogeneity. The change in reservoir water status brings
new challenges to studying the adsorption and flow capacity of shale
gas, which also brings difficulties to assessing the geological reserves
of shale reservoirs and capacity prediction and development. In this
study, based on a two-dimensional nuclear magnetic resonance technique
and low-temperature nitrogen adsorption technique, clay minerals,
organic matter, and marine shale were used as the study objects to
get the distribution characteristics of water in shale pores. The
results show that after entering the shale reservoir, most of the
water is adsorbed on the surface of inorganic pores, mostly clay pores,
to create a bound water film with a thickness of around 0.96 nm. Shale
pores’ diameter, volume, and surface area are all smaller in
the wet state compared to the dry, falling by 10.11, 47.02, and 71.00%,
respectively. Small-scale pores (D < 10 nm) are
better at absorbing water, and the water in these pores fills the
spaces between them to create capillary water besides being adsorbed
on the pore surface. Bound water can aid in the development of gas
reservoirs and the desorption of adsorbed gas, but the capillary water
column obstructs the flow of gas and restricts the flow of shale gas
in microscopic pores. This study will lay a theoretical foundation
for evaluating the water-bearing characteristics of marine shale reservoirs,
which will help analyze the modification effect of fracturing fluid
retention on reservoir water-bearing characteristics and then guide
gas well development.