Showing
a maximum followed by a “decline” in the
CH4/CO2 high-pressure sorption isotherms measured
on shale and coal is often considered abnormal, and it also fails
to form a consistent view on the reason resulting in this abnormity.
Thus far, various factors affecting this phenomenon were proposed,
such as the error produced during the void volume calibration, the
sorption-induced swelling effect, the physical properties of the measured
gas, the difference between the excess and absolute adsorbed amount,
etc. In this study, a systematic classification for these factors
is first provided on the basis of the relevant theoretical and technical
backgrounds, including three categories: (1) measurement procedure,
(2) data processing procedure, and (3) other factors. Then, high-quality
CH4 and CO2 high-pressure sorption isotherms
are obtained in our laboratory and published literature. On this basis,
the effects of these factors on the isotherm are compared by quantitative
or qualitative analysis. The results show that, as a result of the
technical limitation during processing sorption data, the deviation
at 20 MPa would exceed 28% for the CH4 isotherm and 142%
for the CO2 isotherm within the measured temperature range,
which is considered as the main reason resulting in the “decline”
in the high-pressure sorption isotherms on shale and coal. Some additional
evidence, such as the temperature dependence of the “decline”
phenomenon, may also indicate the rationality of this conclusion.
In comparison to the effect of the data processing procedure, the
effect of the measurement procedure is expected to be relatively low,
and the third category of factors only indirectly controls the “display”
of the “decline” in the sorption isotherm. In addition,
our analyses further support the necessity of the correction of the
high-pressure sorption isotherm via blank measurement, especially
for a low-sorption sample.