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  2. Ocean acidification - Wikipedia

    en.wikipedia.org/wiki/Ocean_acidification

    Ocean acidification is the ongoing decrease in the pH of the Earth's ocean. Between 1950 and 2020, the average pH of the ocean surface fell from approximately 8.15 to 8.05. [ 2 ] Carbon dioxide emissions from human activities are the primary cause of ocean acidification, with atmospheric carbon dioxide (CO 2) levels exceeding 422 ppm (as of ...

  3. Carbonated water - Wikipedia

    en.wikipedia.org/wiki/Carbonated_water

    Carbonated water is a diluent mixed with alcoholic beverages where it is used to top-off the drink and provides a degree of 'fizz'. Adding soda water to "short" drinks such as spirits dilutes them and makes them "long" (not to be confused with long drinks such as those made with vermouth).

  4. Carbonic acid - Wikipedia

    en.wikipedia.org/wiki/Carbonic_acid

    Carbonic acid is a chemical compound with the chemical formula H 2 C O 3. The molecule rapidly converts to water and carbon dioxide in the presence of water. However, in the absence of water, it is quite stable at room temperature. [ 5 ][ 6 ] The interconversion of carbon dioxide and carbonic acid is related to the breathing cycle of animals ...

  5. Biological pump - Wikipedia

    en.wikipedia.org/wiki/Biological_pump

    The equilibrium between carbonic acid and carbonate determines the pH of the seawater. Carbon dioxide dissolves easily in water and its solubility is inversely related to temperature. Dissolved CO 2 is taken up in the process of photosynthesis, and can reduce the partial pressure of CO 2 in the seawater, favouring drawdown from the atmosphere.

  6. Bjerrum plot - Wikipedia

    en.wikipedia.org/wiki/Bjerrum_plot

    Example Bjerrum plot: Change in carbonate system of seawater from ocean acidification.. A Bjerrum plot (named after Niels Bjerrum), sometimes also known as a Sillén diagram (after Lars Gunnar Sillén), or a Hägg diagram (after Gunnar Hägg) [1] is a graph of the concentrations of the different species of a polyprotic acid in a solution, as a function of pH, [2] when the solution is at ...

  7. Marine biogenic calcification - Wikipedia

    en.wikipedia.org/wiki/Marine_biogenic_calcification

    Calcifying organisms are particularly at risk due to changes in the chemical composition of ocean water associated with ocean acidification. As pH decreases due to ocean acidification, the availability of carbonate ions (CO 3 2-) in seawater also decreases. Therefore, calcifying organisms experience difficulty building and maintaining their ...

  8. Alkalinity - Wikipedia

    en.wikipedia.org/wiki/Alkalinity

    In the carbonate system the bicarbonate ions [HCO − 3] and the carbonate ions [CO 2− 3] have become converted to carbonic acid [H 2 CO 3] at this pH. This pH is also called the CO 2 equivalence point where the major component in water is dissolved CO 2 which is converted to H 2 CO 3 in an aqueous solution. There are no strong acids or bases ...

  9. Ocean acidification in the Arctic Ocean - Wikipedia

    en.wikipedia.org/wiki/Ocean_acidification_in_the...

    Process. Ocean acidification is caused by the equilibration of the atmosphere with the ocean, a process that occurs worldwide. Carbon dioxide in the atmosphere equilibrates and dissolves into the ocean. During this reaction, carbon dioxide reacts with water to form carbonic acid. The carbonic acid then dissociates into bicarbonate ions and ...