Results of the experiments on passing air and gas CO2 through samples of me
tamorphic rocks at atmospheric pressure and room temperature are plotted. I
t has been established that the flow of CO2, in contrast to other gases, is
governed by sorption-desorption processes, which have pulse behavior in th
e presence of water vapor, rather than by pressure difference. Generation a
nd development of gas sorption-desorption on dried samples are considered.
The flow of CO2 has both continuous and discrete components. The discrete c
omponent has pseudoharmonic behavior and causes spasmodic changes of the co
ntinuous one.
The data obtained agree with known laws of fluid flow on filtration of the
system gas-water through natural porous media.