The chemical dissolution of soluble rock, chiefly limestone, dolomite and gypsum, by slightly acidic water, gradually removing rock mass without leaving solid debris behind. It is the fundamental process behind karst landscapes, from surface fluting and grikes to underground cave systems.
Facts
Process Type Connections
Sources
1. Chemical weathering, Wikipedia
Carbonation sectionQuote, Carbonation section
It takes place when rainwater combines with carbon dioxide to form carbonic acid, a weak acid, which dissolves calcium carbonate (limestone) and forms soluble calcium bicarbonate.
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