Karboksyreutvekslingen
Karboksyreutvekslingen, also known as the carbonic acid cycle, is a fundamental process in the Earth's carbon cycle. It involves the exchange of carbon dioxide (CO2) between the atmosphere, oceans, and land biosphere. This cycle is driven by the dissolution of CO2 in water, forming carbonic acid (H2CO3), which can then dissociate into bicarbonate (HCO3-) and carbonate (CO3^2-) ions. These ions can be taken up by marine organisms and plants, or they can be released back into the atmosphere through respiration and decomposition.
The carbonic acid cycle plays a crucial role in regulating the Earth's climate. By absorbing CO2 from
The carbonic acid cycle is also influenced by geological processes, such as volcanic activity and weathering