Start Date/Time: Wednesday, February 11, 2009, 9:00 AM
Location: Health Sciences Building, Room T-239
'Carbon sequestration: Modeling CO2 migration and fluid-rock
interactions'
Speaker Mike Bickle, University of Cambridge
Abstract:
Geological carbon storage in which carbon dioxide is separated from power
station fuels or waste gases and pumped into storage in geological
formations will play a critical role in moderating anthropogenic CO2
emissions while society develops carbon-free energy sources. The carbon
dioxide needs to remain underground for at least 10,000 years. Although
geological evidence shows that natural CO2 fields have existed for
millions of years with minimal leakage, there is considerable interest in
the fate of CO2 in the anthropogenic storage sites. A number of processes
may affect stored CO2. Many of these act to retain CO2 in the reservoir.
Some of the CO2 will dissolve in formation brines, some will be trapped
in the porosity and some will react with silicate minerals and
precipitate solid carbonate minerals. However the CO2 is lighter than the
brines and will tend to rise. It is possible, although unlikely, that the
CO2 or acidic CO2-saturated brines will corrode cap rocks and escape into
the overlying formations. Modeling such processes is subject to
significant uncertainties. However by making observations on existing CO2
storage sites and older natural CO2 reservoirs we can learn a lot about
the processes which will occur in the reservoirs. I will discuss
observations on the Sleipner field in the North Sea into which Statoil is
pumping 1 million tons of CO2 a year and on natural CO2 field in the
Colorado plateau which allow us to infer the rate at which CO2-saturated
brines react with minerals in their host formations.
2008/09 WUN Earth Systems Virtual Seminar Theme: Geoengineering and Geohazards
Website: http://www.wun.ac.uk/horizons/earthsystems/