Microwave irradiation is available
to produce shale gas. Practical
gas-bearing shale reservoirs often contain water (H2O).
Given the special physicochemical property of H2O and its
occurrence rule in the gas-bearing shale matrix, the presence of H2O has potential effect on electromagnetic energy penetration
and dielectric property of the shale matrix, therefore affecting application
of microwave irradiation to produce the chief component of shale gas,
that is, methane (CH4), from the shale reservoir. Hence,
to further explore shale gas production via microwave irradiation,
the impact of H2O of gas-bearing shale in its physicochemical
property response to microwave irradiation was mainly investigated.
The H2O dependence of CH4 adsorption capability
alteration due to microwave irradiation was also addressed. The results
indicate that microwave irradiation exerts minor impact on the micropore
of both dry and moist shales but a noticeable impact on their mesopore.
Specifically, both the mesoporous surface area and volume of dry and
moist shales decrease after microwave irradiation. The presence of
H2O further decreases the typical mesoporous parameters
including pore surface area and pore volume of shales in general.
Moreover, fractal analysis reveals that both the roughness of the
pore surface and complexity of pore structure decrease for all the
shales after microwave irradiation, and those of moist shale after
microwave irradiation decrease even further, thus facilitating shale
gas migration and diffusion within the shale matrix. As for the surface
chemical property of shale, the total amount of oxygenic groups consisting
of highly conjugated carbonyl, conjugated carbonyl, and carboxyl of
dry shales rises after microwave irradiation, but the aromaticity
drops. Also, the same changing rule in functional groups is also found
for moist shale after microwave irradiation; however, the change is
even more pronounced. Finally, the CH4 adsorption capacity
of both dry and moist shales decreases after microwave irradiation.
In comparison to dry shale, CH4 adsorption capacity of
moist shale containing low total organic carbon (TOC) and H2O decreases, but that of moist shale with high TOC content and H2O content increases. These alterations in CH4 adsorption
capability of various moist shales are relevant to their pore structure
and functional group response to microwave irradiation. Overall, the
presence of H2O is beneficial for further weakening the
adsorption affinity between CH4 and the shale matrix and
strengthening migration capability of CH4 under microwave
irradiation, thus making microwave irradiation become a competitive
technology regarding shale gas production.