Hardness in water is defined as the presence of cations.
Hardness in water can cause water to form scales and a resistance to
soap. It can also be defined as water that does not produce lather with
soap solutions, but produces white precipitate. Hardness Test Kits are used to determine the amount of hardness in the water
Hard water minerals primarily consist of magnesium and calcium metal cations, and sometimes other dissolved compounds such as bicarbonates and sulfates. Calcium usually enters the water as either calcium carbonate,, in the form of limestone and chalk, or calcium sulfate, in the form of other mineral deposits. The predominant source of magnesium is dolomite. Hard water is generally not harmful to one's health.
Hardness of water may also be defined as the soap-consuming capacity of water, or the capacity of precipitation of soap as a characteristic property of water that prevents the lathering of soap. Hardness test kits are used to verify hardness.
Permanent hardness is hardness is considered mineral content. This cannot be removed by boiling. It is usually caused by the presence in the water of magnesium and calcium and/or chlorides which become more soluble as the temperature rises. Despite the name, permanent hardness can be removed using a water softener or ion exchange column, where the calcium and magnesium ions are exchanged with the sodium ions in the column.
Hard water can cause scaling. The left-over mineral deposits that are formed after the hard water had evaporated. This is also known as limescale. Scale can clog pipes, ruin water heaters, coat the insides of tea and coffee pots, and decrease the life of toilet flushing units.
In industrial settings, water hardness must be constantly monitored to avoid costly breakdowns in boilers, cooling towers, and other equipment that comes in contact with water. Hardness is controlled by the addition of chemicals and by large-scale softening with zeolite and ion exchange resins. Hardness test kits can be used to determine the amount of hardness in the water.
Measurement
Because it is the precise mixture of minerals dissolved in the water, together with the water's pH and temperature, that determines the behavior of the hardness, a single-number scale does not adequately describe hardness. Descriptions of hardness correspond roughly with ranges of mineral concentrations:
-
Soft: 0-60 mg/L
- Moderately hard: 61-120 mg/L
- Hard: 121-180 mg/L
- Very hard: >181 mg/L
It is possible to measure the level of total hardness in water by obtaining a total hardness water testing kit. These kits measure the level of calcium and magnesium in the water. Temporary hardness test kits do not normally measure calcium and magnesium levels but normally use an approximation based on some form of alkalinity test. Measuring temporary hardness accurately would involve a series of tests to work out how much bicarbonates and carbonates are present and how much calcium and magnesium is present and what percentage combination there is. In most cases, the temporary hardness kit is a good approximation, but anions such as hydroxides, borates, phosphates can have quite an effect on temporary hardness test kits.
There are several different scales used to describe the hardness of water in different contexts.
- Parts per million (ppm)
- Usually defined as one milligram of calcium carbonate (CaCO3) per litre of water
- Grains per Gallon (gpg)
- Defined as 1 grain (64.8 mg) of calcium carbonate per U.S. gallon (3.79 litres), or 17.118 ppm
- Degrees of General Hardness (dGH)
- One degree American is defined as one milligram of calcium carbonate per litre of water, equivalent to 1 ppm.
Softening Process
The most economical way to soften household water is with an ion
exchange water softener. This unit uses sodium chloride (table salt) to
recharge beads made of the ion exchange resins that exchange hardness
mineral ions for sodium ions. Artificial or natural zeolites can also be
used. As the hard water passes through and around the beads, the
hardness mineral ions are preferentially absorbed, displacing the sodium
ions. This process is called ion exchange. When the bead or sodium
zeolite has a low concentration of sodium ions left, it is exhausted,
and can no longer soften water. The resin is recharged by flushing
(often back-flushing) with saltwater. The high excess concentration of
sodium ions alter the equilibrium between the ions in solution and the
ions held on the surface of the resin, resulting in replacement of the
hardness mineral ions on the resin or zeolite with sodium ions. The
resulting saltwater and mineral ion solution is then rinsed away, and
the resin is ready to start the process all over again. This cycle can
be repeated many times.
A water softener works on the principle of cation or ion exchange in which ions of the hardness minerals (mainly calcium and magnesium ions) are exchanged for sodium or potassium ions, effectively reducing the concentration of hardness minerals to tolerable levels and thus making the water softer and giving it a smoother feeling.