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|title=Hindered Calcification Process | |title=Hindered Calcification Process | ||
}} | }} | ||
== Explanation == | == Explanation == | ||
The formation of limestone (calcification) follows the chemical reaction Ca<sup>++</sup> + 2HCO<sub>3</sub><sup>-</sup> ⇔ CaCO<sub>3</sub> + H<sub>2</sub>O + CO<sub>2</sub> | The formation of limestone (calcification) follows the chemical reaction Ca<sup>++</sup> + 2HCO<sub>3</sub><sup>-</sup> ⇔ CaCO<sub>3</sub> + H<sub>2</sub>O + CO<sub>2</sub> | ||
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The addition of an acid shifts the equilibrium towards the left of the equation. In other words, if the pH drops, there are fewer bicarbonate ions, making it more difficult for organisms to build their shells. | The addition of an acid shifts the equilibrium towards the left of the equation. In other words, if the pH drops, there are fewer bicarbonate ions, making it more difficult for organisms to build their shells. | ||
== Correction== | |||
===Causes=== | |||
* [[En-en_adult_card_24_ocean_acidification|Ocean Acidification]] | |||
=== Consequences === | |||
* [[En-en_adult_card_29_pteropods_and_coccolithophores|Pteropods and Coccolithophores]] | |||
[[fr:Fr-fr_adulte_carte_23_problèmes_de_calcification]] | [[fr:Fr-fr_adulte_carte_23_problèmes_de_calcification]] |
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