Not exact matches
Acidification refers to a lowering of the pH of
seawater when it
absorbs carbon dioxide, pushing it closer to the acidic end of the scale, although it is still slightly alkaline.
This is the drop in
seawater pH as the oceans
absorb an estimated 22 million tons of
carbon dioxide from the 80 million tons emitted each day by human activities.
just a small example: rain washes CO2 from the air into the sea - > water turns CO2 into carbonic acid - > coral
absorbs that compound — > keeps the
carbon for itself - > releases the oxygen from the CO2 molecule, to replenish the
seawater with oxygen.
When atmospheric
carbon dioxide is
absorbed into the ocean, it reacts to produce carbonic acid, increasing the acidity of
seawater and diminishing the amount of a key building block (carbonate) used by marine species like shellfish and corals to make their shells and skeletons.
Although the CO2 that is taken up by the ocean does not contribute to greenhouse warming, ocean warming reduces the solubility of
carbon dioxide in
seawater; and thus reduces the amount of CO2 the oceans can
absorb from the atmosphere.
Fish are known to
absorb calcium from
seawater, binding it to
carbon and excreting it as a carbonate molecule that can form a weak base capable of neutralizing ocean acidity.
It does this by shifting the series of equilibria (below) to the right, thereby increasing the capacity of
seawater to
absorb carbon dioxide from the atmosphere and by decreasing the propensity for
seawater to desorb
carbon dioxide into the atmosphere.»
But also, over time, most of the
carbon dioxide in the atmosphere is
absorbed by the ocean, where it reacts with
seawater to form an acid that is corrosive to coral reefs, shellfish, and other marine life.
For example, as temperatures warm,
seawater absorbs less
carbon dioxide, and as precipitation patterns change and plants grow (or die), they take up more (or less)
carbon.
«Ocean pH tells us about the amount of
carbon absorbed by ancient
seawater, but we can get even more information by also considering changes in the isotopes of
carbon, as these provide an indication of its source,» says Andy Ridgwell, co-author of the study.
The oceans
absorb carbon dioxide, causing
seawater to be 30 % more acidic than it was in pre-industrial times.