
Hard water poses challenges for both industrial and domestic use due to its elevated levels of calcium (Ca) and magnesium (Mg) ions compared to regular water. Temporary hardness, known as carbonate hardness, arises from the presence of carbonates and bicarbonates of calcium and magnesium, while permanent hardness results from other dissolved minerals.
The hardness of water increases with higher concentrations of calcium and magnesium ions, which originate from limestone sediments and carbon dioxide present in atmospheric and groundwater sources. Softening hard water is commonly achieved through ion exchange processes, which involve the removal of calcium and magnesium ions and their replacement with sodium ions.

Ca (HCO3)2 + Na2 R = RCa + NaHCO3
CaSO4 + Na2 R = RCa + Na2SO4MgCl2 + Na2
R = RMg + NaCl
RCa + NaCl = RNa + CaCl2
RMg + NaCl = RNa + MgCl2
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