CH4–CO2 swapping has been
viewed as
a win–win situation for gas hydrate exploitation and geological
storage of CO2. This method would form CH4 and
CO2 coexist in the hydrate phase after reaction, and the
stability condition of (CH4 + CO2) hydrates
in the geological environment is significant for better understanding
the CH4 recovery and CO2 sequestration. The
dissociation points of (CH4 + CO2) hydrates
in the (quartz sands + NaCl solution) system were measured with the
isochoric pressure-search method in this work. The results indicated
that the measured dissociation points shift left compared to the equilibrium
curves of bulk hydrate. The equilibrium pressure of (CH4 + CO2) hydrates present a decreasing trend with the increasing
of CO2 concentration in the gas phase at a given temperature.
The effect of pore water salinity and sediment particle size on the
hydrate equilibrium condition was investigated. It was found that
the hydrate dissociation condition shifted to a lower temperature
with the increase of NaCl concentration. The temperature shifts showed
an increasing trend as the sediment particle size decreases. The maximum
temperature shift was 1.2 K for the quartz sand system with an average
particle size of 8.85 μm. The hydrate dissociation enthalpies
were calculated with the Clausius–Clapeyron equation. The dissociation
enthalpies of (CH4 + CO2) hydrates are between
those of pure CH4 and CO2 hydrate, having an
increasing trend with the increase of CO2 content in the
gas phase.