摘要
Saline aquifer has the most sequestration potential among all the sites that can implement CO2 geological sequestration. Structual stratigraphic sequestration is the basic mechanism which can affect CO2 storage capacity in a saline aquifer. In this paper, an experimental method is used to measure the irreducible water saturation to a rock sample, a key parameter that affects structual stratigraphic storage capacity. The rock sample is taken from the Ordovician reef limestone in Tarim Basin, which is widely considered to be rich in oil and gas.