As the primary mechanism of gas storage
in shale, sorption phenomena
of CH4 and other hydrocarbons in the micropores and mesopores
are critical to estimates of gas-in-place and of the long-term productivity
from a given shale play. Since C2H6 is another
important component of shale gas, besides CH4, knowledge
of CH4–C2H6 binary mixture
sorption on shale is of fundamental significance and plays a central
role in understanding the physical mechanisms that control fluid storage,
transport, and subsequent shale-gas production. In this work, measurements
of pure component sorption isotherms for CH4 and C2H6 for pressures up to 114 and 35 bar, respectively,
have been performed using a thermogravimetric method in the temperature
range (40–60 °C), typical of storage formation conditions.
Sorption experiments of binary (CH4–C2H6) gas mixtures containing up to 10% (mole fraction)
of C2H6, typical of shale-gas compositions,
for pressures up to 125 bar under the aforementioned temperature conditions
have also been conducted. To the best of our knowledge, this is the
first time that systematic measurements of CH4 and C2H6, both pure and in binary mixtures, sorption
on the Marcellus shale have been conducted, thus providing a comprehensive
set of CH4–C2H6 competitive
sorption data, which can help to improve the fundamental understanding
of shale-gas storage mechanisms and its subsequent production. In
the study, the multicomponent potential theory of adsorption (MPTA)
approach is utilized to model the sorption data. The MPTA model is
shown capable in representing the pure component sorption data, and
also provides reasonable predictive capability when applied to predict
the total sorption for CH4–C2H6 binary mixtures in shale over a range of compositions and temperatures.