Abstract
Structural trapping, the most important CO2 geostorage mechanism during the first decades of a sequestration project, hinges on the traditional assumption that the caprock is strongly water wet. However, this assumption has not yet been verified; and it is indeed not generally true as we demonstrate here. Instead, caprock can be weakly water wet or intermediate wet at typical storage conditions; and water wettability decreases with increasing pressure or temperature. Consequently, a lower storage capacity can be inferred for structural trapping in such cases.
| Original language | English |
|---|---|
| Pages (from-to) | 9279-9284 |
| Number of pages | 6 |
| Journal | Geophysical Research Letters |
| Volume | 42 |
| Issue number | 21 |
| DOIs | |
| Publication status | Published - 16 Nov 2015 |
| Externally published | Yes |
Keywords
- CO geosequestration
- storage capacity
- structural trapping
- wettability