When dissolves in seawater, it reacts with water () to form carbonic acid ():
Carbonic acid is unstable and quickly dissociates into hydrogen ions () and bicarbonate ions ():
The increase in ions directly lowers the pH of the water, making it more acidic. Furthermore, these ions react with existing carbonate ions () to form more bicarbonate, which depletes the carbonate available for marine life.
Fossil Fuel Combustion: The burning of coal, oil, and natural gas for energy and transportation is the primary source of excess atmospheric .
Deforestation: Removing forests reduces the planet's capacity to sequester carbon through photosynthesis, leaving more in the atmosphere to be absorbed by oceans.
Industrial Processes: Activities such as cement production release significant amounts of when calcium carbonate is chemically converted into lime.
Calcification Inhibition: Marine organisms like corals, mollusks, and some plankton use carbonate ions to build calcium carbonate () shells and skeletons. As carbonate availability drops, these structures become harder to build and may even begin to dissolve.
Coral Reef Degradation: Slower calcification rates lead to weaker reef structures that are more susceptible to erosion and storm damage, threatening the biodiversity they support.
Food Web Disruption: Small shelled organisms like pteropods (sea butterflies) are highly sensitive to pH changes. Their decline removes a foundational food source for fish, which eventually impacts apex predators and human food security.
| Feature | Ocean Acidification | Global Warming |
|---|---|---|
| Primary Cause | Absorption of gas | Greenhouse effect trapping heat |
| Direct Effect | Chemical change (lower pH) | Physical change (higher temperature) |
| Biological Impact | Difficulty building shells/skeletons | Thermal stress and bleaching |
| Relationship | Shared cause (), but NOT a result of warming | Shared cause (), but NOT a result of acidification |
The pH Scale is Logarithmic: Remember that a small numerical drop in pH represents a large change in acidity. A drop from 8.2 to 8.1 is a ~30% increase in concentration.
Identify the Ions: Be precise about which ions are increasing (, ) and which are decreasing (). Exams often test this specific inverse relationship.
Avoid the 'Acid' Trap: The ocean is not becoming 'an acid' (pH < 7); it is becoming more acidic (moving toward 7). It currently remains slightly basic.
Causality Check: Always state that reacts with water to form an acid. Do not skip the chemical intermediate (carbonic acid) when explaining the process.