There are different types of water hardness:
|● TH||–||Total Hardness|
|● CH||–||Carbonate Hardness||(Temporary Hardness)|
|● NCH||–||Non-carbonate Hardness||(Permanent Hardness)|
|● PsH||–||Pseudo Hardness|
Total Hardness TH
Total hardness is defined as the molar concentrations of all multi-valent cations in water (i.e. all but the monovalent cations):
|(1)||Total Hardness TH = Σ multivalent cations|
In practice, it is often used as the sum of the two most important freshwater cations, calcium and magnesium:
|(1a)||TH ≈ [Ca] + [Mg]|
But this is only an approximation, albeit a good one.1 The correct formula is (according to its definition in 1):
|(1b)||TH = [Ca] + [Mg] + [Sr] + [Ba] + [Fe] + [Mn] + [Al] + …|
There are several water hardness scales in use. For example, it can be expressed in meq/L (SI units), or in ppm CaCO3, or in German hardness degrees:
|(2a)||TH in meq/L||=||2 × ( [Ca in mM] + [Mg in mM] )|
|(2b)||TH in ppm||=||100.1 × ( [Ca in mM] + [Mg in mM] )|
|(2c)||TH in °d||=||0.1339 × [Ca in mg/L] + 0.2307 × [Mg in mg/L]|
Note: If the concentrations of Ca and Mg ions are expressed as “ppm CaCO3”, 1a is also represented in the form:
|(3)||Total Hardness TH = Calcium Hardness + Magnesium Hardness|
Carbonate Hardness CH
While the total hardness in 1 is defined by the cationic content, there is also the opposite viewpoint taken from the anionic content, which divides the total hardness into carbonate hardness CH (temporary hardness) and non-carbonate hardness NCH (permanent hardness):
|(4)||Total Hardness TH = CH + NCH|
Carbonate hardness is directly related to alkalinity:
|(5a)||CH in meq/L||=||[Alk in meq/L]|
|(5b)||CH in °dH||=||2.809 × [Alk in meq/L]|
This means that in water chemistry the terms carbonate hardness and alkalinity (i.e. M alkalinity or total alkalinity) are synonyms:
|(6)||Carbonate Hardness CH = Alkalinity|
The program calculates TH and CH, and displays both quantities in the output tables – as shown here.
Non-Carbonate Hardness NCH
Both total hardness and alkalinity (i.e. carbonate hardness) are common water analysis parameters. The non-carbonate hardness is – according to 4 – the difference of both quantities:
|(7)||NCH = TH – CH|
Carbonate hardness is named temporary hardness because Ca and Mg carbonates precipitate as minerals upon heating, whereas Ca and Mg associated with sulfates, chlorides, or nitrates do not precipitate upon heating (therefore NCH is called permanent hardness).
Alternative Interpretation. The non-carbonate hardness is a measure of the excess of strong acids over strong bases:
|(8)||NCH = strong acids – strong bases|
Given a water analysis, strong acids manifest themselves in the presence of non-carbonate anions such like sulfate, chloride, nitrate. On the other hand, strong bases are indicated by monovalent cations (e.g. Na, K, ammonium). In this way, 8 converts to
|(9)||NCH [meq/L] ≈ (2×sulfate + chloride + nitrate) – (Na + K + ammonium)|
where the measured concentrations should be entered in units of mmol/L.
Pseudo Hardness PsH
The three quantities, TH, CH and NCH form the standard vocabulary of water hardness in almost all textbooks. However, a problem appears if the measured alkalinity (i.e. CH) exceeds the total hardness: CH > TH. In this special case 4 becomes senseless.
To solve the problem, the hardness terminology should be extended by an additional quantity – the pseudo hardness PsH (or “apparent hardness”). It is defined as the “negative NCH” and expressed by the reverse of 8:
|(10)||PsH = strong bases – strong acids = – NCH|
|(11)||PsH [meq/L] ≈ (Na + K + Ammonium) – (2×sulfate + chloride + nitrate)|
In other words, PsH is the portion of the carbonate hardness that belongs to the monovalent cations (Na, K, ammonium).
Extension of the Common Hardness Relation
Due to the additional quantity PsH we are able to extend the “standard hardness equation” (4):
|(12)||Water Hardness: TH + PsH = CH + NCH|
It is important to note that PsH and NCH are mutually exclusive in the above formula: either the strong bases outweigh the strong acids (then NCH=0) or vice versa (then PsH=0). Thus, 12 becomes:
|(13a)||TH ≥ CH:||TH = CH + NCH||PsH = 0|
|(13b)||TH < CH:||TH + PsH = CH||NCH = 0|
where 13a represents the “standard” hardness relation of common textbooks.
Example: TH ≥ CH
The case TH ≥ CH is typical for almost all natural waters. For illustration we take the example water C1.sol (button Open) with the following parameters:
Run the water sample by click on button Start. The program complains about a non-zero CBE, and we establish exact charge balance by adjustment of DIC (which decreases alkalinity from 2.50 to 2.45 meq/L). The obtained hardness values are (as shown in table column Output 1):
|TH = 2.45 meq/L|
|CH = 3.26 meq/L|
From the difference we get: NCH = 0.81 meq/L. There is no pseudo hardness (PsH=0). The total hardness is determined by the sum of Ca and Mg: TH = (2×1.40 + 2×0.23) meq/L = 3.26 meq/L – as presented in the diagram above.
Example: TH < CH
We use the same example water C1.sol and add 2 mM NaOH (with button Reac)2.
Due to the addition of 2 meq/L of a strong base the alkalinity and, hence, CH increase by 2 meq/L while the total hardness remains unchanged:
|CH = 4.45 meq/L|
|TH = 3.26 meq/L|
Here the difference is given by the pseudo hardness: PsH = 1.19 meq/L. There is no NCH.
The value of PsH can also be calculated by inserting the molar concentrations of the input water into 11:
|(14)||PsH = (2.30 + 0.05) – (2×0.38 + 0.25 + 0.15) = 1.19 meq/L|
Note that Na also incorporates the addition of 2 mM NaOH: Na = (2.0 + 0.3) meq/L. The calculated value of 14 is explicitly shown as ‘Diff’ in the above diagram.
Calcite Precipitation. Due to the addition of 2 mM NaOH the water becomes super-saturated with respect to calcite. The bottom diagram shows the results when 1.37 mM calcite precipitates (table column Output 2):
|CH||=||(4.45 – 2×1.37) meq/L||=||1.71 meq/L|
|TH||=||(3.26 – 2×1.37) meq/L||=||0.52 meq/L|
|PsH||=||CH – TH||=||1.19 meq/L (unchanged)|
In the following we add one or two reactants with an amount of 1 mM to pure water (H2O).3 The results of about 20 calculations are listed in the table below; each row referring to one calculation. The values of TH, CH, NCH, and PsH are given in the last columns.
Note: In cases where CaCO3 (calcite) becomes super-saturated (SI > 0), an extra row has been added to show the results after calcite precipitation.4
Water hardness is expressed in different units:
|(15a)||German Degrees:||1 °d||=||10 mg/L CaO|
|(15b)||French Degrees:||1 °f||=||10 mg/L CaCO3|
|(15c)||English Degrees:||1 °e||=||10 mg CaCO3 in 0.7 L|
|(15d)||1 ppm CaCO3 (US norm):||1 °a||=||1 mg/L CaCO3 5|
These units are interrelated by simple conversion rules:
|1 ppm CaCO3||1||0.06||0.10||0.07||0.02||0.01|
The conversion factors in this table follow directly from the molar weights of calcium carbonate and calcium oxide:
|(16a)||CaCO3:||100.09 g/mol||or||1 mg/L CaCO3||=||0.010 mM|
|(16b)||CaO:||56.08 g/mol||or||10 mg/L CaO||=||0.178 mM|
Remarks & Footnotes
Other alkaline-earth metals like strontium (Sr) and barium (Ba) have no significant contribution to TH because they are found in trace amounts in natural waters. The same applies for all other metals (such like Fe, Mn, Al) in pH neutral waters. ↩
To establish exact charge balance click on Setup in the reaction module. ↩
To add reactants to a given water click on Reac. ↩
The reaction 1 mM CaCO3 + 1 mM MgCO3 generates a water which is super-saturated with respect to both calcite and brucite. In the present example, we consider the precipitation of calcite, but we ignore the precipitation of brucite, i.e. Mg(OH)2. ↩
ppm (parts per million) is defined as 1 ppm = 1 mg / 1 kg = 10-6. For diluted solutions with density ≈ 1 kg/L the numerical value of both concentration units, ppm and mg/L, are practically equal. ↩