When CO2 (in liquid or gas phase) is pumped into the underpermafrost collectors, it is possible that some CO2 migrates towards the hydrate stability zone and hydrate-saturated horizons can be formed. This can increase the effective capacity of the collector and increase the isolating properties of cap rock. The possibility of CO2 sequestration in the permafrost area and the processes of hydrate formation that occur were studied. Air-con.
|Number of pages||1|
|Publication status||Published - 1 Jan 2015|