Ocean acidification in a geoengineering context
Fundamental changes to marine chemistry are occurring because of increasing carbon dioxide (CO2) in the atmosphere. Ocean acidity (H+ concentration) and bicarbonate ion concentrations are increasing, whereas carbonate ion concentrations are decreasing. There has already been an average pH decrease o...
| Main Authors: | , |
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| Format: | Online |
| Language: | English |
| Published: |
The Royal Society Publishing
2012
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| Online Access: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3405667/ |