1. #"CaCO"_3# causes most of the hardness
Water passing over limestone deposits dissolves some of the minerals.
The concentrations of #"Ca"^"2+", "Mg"^"2+"#, and #"HCO"_3^"-"# ions present in the water increase greatly and cause the water to become "hard."
#"Ca"# and #"Mg"# often occur together, so it is convenient to have a single number that represents the total concentration of both ions.
2. The calculation is easy
We measure the concentrations of individual ions #"Ca"^"2+"# and #"Mg"^"2+"#.
We usually express the hardness of water in "ppm" (parts per million or milligrams per kilogram of water or milligrams per litre).
The molar mass of #"CaCO"_3"# is 100 g/mol, so it is easy to manipulate the numbers.
Thus,
#M_text(CaCO₃)/M_text(Ca) = 100/40 = 2.5#
#M_text(CaCO₃)/M_text(Mg) = 100/24.3 = 4.1#
Thus we can express the total hardness of water as
#["CaCO"_3] = 2.5["Ca"^"2+"] + 4.1["Mg"^"2+"]#
Example
If #["Ca"^"2+"] = "30 mg/L"# and #["Mg"^"2+"] = "3 mg/L"#,
The total hardness expressed as #"CaCO"_3# is
#["CaCO"_3] = "2.5 × 30 mg/mL+ 4.1 × 3 mg/L = 75 mg/L + 12 mg/L"#
# "= 87 mg/L"#