In the north Atlantic Ocean near Bermuda, surface seawater pH is decreasing AG-014699 supplier by 0.0017 ± 0.0001 units yr−1 (Bates

and Peters, 2007) whilst measurements from the European Time Series in the Canary Islands (0.0017 ± 0.0004 pH units yr−1) provides very similar results for the east Atlantic Ocean (Santana-Casiano et al., 2007). The Pacific ALOHA station, near Hawaii, has shown surface pH values to be decreasing by 0.0019 ± 0.0002 yr−1 (Dore et al., 2009). So as the threat of global warming and acidification become ever more real the political, social and environmental pressure to reduce CO2 emissions continues to grow. Indeed, the Intergovernmental Panel on Climate Change (IPCC) stated that if global average temperature increases are to be prevented from exceeding pre-industrial levels by more than 2 °C, then global CO2 emissions must be reduced by between 50% and 85% by 2050. However, with the International Energy Agency (IEA) predicting that global energy demand could increase by as much as 45% by 2030, a reduction in emissions on this scale is extremely challenging. This realisation has prompted the exploration

of a number of engineering-based mitigation strategies. One of these proposed mitigation techniques is CO2 capture and storage (CCS), which involves the capturing of waste CO2 from large industries such as coal and Olopatadine natural gas fired power plants, transporting it to a storage site and depositing it in

deep geological formations such as depleted oil buy Omipalisib and gas fields, unmineable coal seams or deep saline aquifers (Holloway, 2007). By significantly reducing CO2 emissions from fossil fuel power stations it is estimated that CCS could have a significant affect in a relatively short period of time; potentially reducing total emissions by 21–45% before 2050 (Metz et al., 2005). With many nations heavily reliant and economically locked into fossil fuel based power generation such an emissions reduction strategy is extremely attractive. The technology required to inject CO2 into geological formations is not new. It has been employed at industrial scales for decades as part of the Enhanced Oil Recovery (EOR) process. However, injecting CO2 solely for the purposes of permanent storage is in its infancy. Whilst the technology to transport and place CO2 under the ground is well advanced a number of key areas still need to be more fully explored. One major issue for CCS, as with the introduction of many new technologies, is the need to secure scientific and public acceptance of CCS activities. Whilst it can be argued that the likelihood of leakage is extremely small, the possibility of leaks cannot be ruled out.