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Limestone is a crystal that is formed by depositing Carabone mainly calcium and magnesium. The concentration of these substances is measured in French degrees (° F, 1 F = 1 cg / l calcium carbonate). Initially, the carbonate solution is in the state of carbonate acid or hydrogen carbonate due to carbon dioxide dissolved in water acidity that keeps below a certain value. When water is heated above 65 ° C, the carbon dioxide is removed from the water and the pH increases to the point that the hydrogen carbonate is transformed into carbonate, insoluble precipitates thus forming the limestone layer.
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There are many systems designed to solve the problem of scale, but between all that stands out for its efficiency and ion exchange. The ion exchange resins exploits the ability to attract to itself the ions responsible for hardness, highly soluble in water treated by releasing substances such as sodium chloride, salt with which the resins are regenerated once reached saturation. The process is then able to produce water at 0 ° F.
Other ways to reduce the problem of scale are the filters or silifosfati polyphosphates, or magnetic disruptors.
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