To reveal the feasibility of the Polanyi potential theory
toward
methane (CH4) adsorption equilibrium on marine gas-bearing
shale matrices, a quantitative analysis method was proposed to elaborate
adsorption mechanisms on CH4–shale systems based
on CH4 adsorption data. Additionally, the potential theory
was employed to generate CH4 adsorption isotherms on shale
matrices at a given temperature and further distinguish organic matter
and clay mineral dependences of CH4 adsorption. Ultimately,
the potential theory was used to plot the curves of CH4 adsorption capacity versus various burial depths of shale reservoirs.
Results indicate that CH4 adsorption on marine gas-bearing
shale matrices typically follows micropore filling. Hence, the supercritical
Dubinin–Astakhov (D–A) model derived from the potential
theory is capable of describing CH4 adsorption equilibrium
on shale matrices. The adsorption characteristic curve via combining
the Polanyi potential theory and the supercritical D–A model
well coincides within the entire adsorption temperature range. Therefore,
the adsorption characteristic curve is competent to predict CH4 adsorption isotherms at a given temperature. Moreover, the
Polanyi potential theory approach suggests that the organic matter
content of shale matrices shows a slightly positive correlation with
its adsorption capability for CH4. The clay minerals exert
a minor impact on the CH4 adsorption capability of the
shale matrices with high organic matter contents. Instead, the contribution
of clay minerals to the shale matrices with low TOC cannot be neglected.
Finally, the potential theory is capable of plotting the variation
curves of the CH4 adsorption capacity versus burial depth.
The Polanyi potential theory can well estimate the CH4 adsorption
capability of shale matrices with various burial depths, thereby benefiting
shale gas assessment and production.