Lubjakivi tekib kas vees lahustunud leelismuldmetallide soolade soojusmuundamise teel (karbonaadi karedus) või lahustuvuspiiri ületamise teel, mis sõltub ka temperatuurist.
The limescale either by heat conversion of the alkaline earth salts dissolved in the water (carbonate hardness) or by overstepping the point of solubility which is also temperature-dependent.
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