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Effervescence in mineralogy refers to the bubbling that occurs when a mineral reacts with an acid, releasing carbon dioxide gas. This reaction is a key test for identifying carbonate minerals.12

For example, when dilute hydrochloric acid is applied to minerals like calcite or aragonite, they bubble vigorously, producing a "fizz" due to the release of carbon dioxide. Other carbonate minerals, such as dolomite, may show a slower effervescence, especially if the mineral is powdered or the acid is warmed. This difference in reaction helps distinguish between minerals like calcite and dolomite in the field. The term effervescence can also describe a lively quality, like the "effervescence of youth".134

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