Learn about Water and Filtration
Contaminants and Health Effects
Water quality problems and solutions
Sources of our drinking water
Standards for drinking water
Hard and soft water
pH value of water
Filtration OR Purification?
Myth on minerals and water
Popular filtration methods explained
General water treatment
Water quality defined
Hydrologic cycle of water
Meteoric water and cycle
Environmental factors of water
Age of ground water
Temperature of ground water
Water quality of surface water
Cistern water quality
Summary of water quality and the environment
Hard water explained
Hard water problems
Softened water energy savings
Hard water analysis
Hard water and soap curd
Ion exchange principles
More on water softening
Home water softener basics
Water deionization
Lime soda ash water treatment
3 Types of basic water
TDS-Total dissolved solids
Reverse osmosis treatment
Alkalinity of water
Reverse osmosis and pH
Carbon dioxide in water
Chloride and sulfate
Fluoride in drinking water
Hydrogen sulfide in water
Nitrate/ nitrogen in water
Oxygen in drinking water
Silica in drinking water
Sodium/methane/ phenol Disease-causing organisms
Micro-organism in water1
Micro-organism in water2
Viruses in drinking water
Bacteria in drinking water
Water disinfect methods1
Water disinfect methods2
Water disinfect-chlorine
Dechlorinating filters Q&A
Palatability of water
Turbidity of drinking water
Mechanical filtration
Multi-media (depth filters)
Color of drinking water

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SOFTENED WATER ENERGY SAVINGS STUDY

In a recent University study energy consumption of gas and electric water heaters operated and tested on hard water supplies was measured and compared to measured energy consumption of gas and electric water heaters operated and tested on softened water supplies.

The gas heaters operated and tested on hard water consumed 29.57% more Btu's of energy than the gas heaters operated and tested on softened water for the same amount of energy delivered.

The electric heaters operated and tested on hard water consumed 21.68% more Btu's of energy than the electric water heaters operated and tested on softened water for the same amount of energy delivered.

It is not necessary to heat water to a high temperature to produce scale. Any increase above the original temperature of the water can cause lime scaling to occur.

Although no chemical reaction occurs which causes calcium sulfate to deposit when the water is heated, this hardness mineral is unusual as it is less soluble in hot water than in cold.

Hard water can also be troublesome in industry. In many industrial applications, however, not only must hardness be removed from the water, but all mineral content must be eliminated. Mineral deposits can cause serious difficulties in boilers, air conditioning systems, gasoline and diesel engine cooling systems.

Water is an excellent solvent. Our previous articles outlines how water collects the various contaminants found in it.

As moisture falls through the atmosphere, it absorbs amounts of carbon dioxide (CO2).It also collects amounts of this gas on and in the ground from decaying vegetation. Since carbon dioxide is a product of both combustion and decay it is present in practically all water supplies.

When carbon dioxide dissolves in water, some of it forms a weak acid called carbonic acid.

H20 + C02 --> H2C03

This acid is responsible for dissolving limestone or carbonate deposits in the earth. It also produces certain types of corrosion in water and steam lines. The natural solvent action of water is enhanced by carbonic acid making it even more effective in dissolving hardness minerals.

Hardness minerals-calcium and magnesium­ are in plentiful supply. While they are not found in their elemental form in the earth, they occur in combination with other elements in an abundance of forms. Common calcium minerals include chalk, limestone and marble. These substances are chiefly calcium carbonate (CaC03) or mixtures of calcium and magnesium carbonates and other impurities. Gypsum is calcium sulfate (CaSO4). In this compound calcium is combined with sulfur and oxygen.

Epsom salt is magnesium sulfate (MgS04).

Ions of the following calcium and magnesium compounds are found in water:

The amounts of these various chemical compounds present in water supplies depend on two factors:

1. The minerals present in the earth; and

2. Their solubility in water related to carbon dioxide (CO2) concentration.

On a decreasing scale of solubility, calcium chloride, magnesium chloride and magnesium sulfate are extremely soluble. They may be found in water in almost unlimited amounts. Calcium sulfate is less soluble. At the other end of the solubility scale are the calcium and magnesium carbonates which are very slightly soluble in pure water. The amounts of these last two compounds in water rarely exceeds two and five grains respectively. Calcium and magnesium carbonates are seldom found in natural water supplies because of their very low solubility.

While "insoluble" carbonates are rarely found, they are found in their extremely soluble form in hard water as calcium and magnesium bicarbonates. When water containing carbon dioxide comes into contact with calcium and magnesium carbonates in the ground, a chemical reaction takes place. The "insoluble" carbonate forms of magnesium and calcium are transformed into highly soluble bicarbonates. These are the principal hardness compounds found in water. It is interesting to note that these bicarbonate forms exist only in solution. If heat is applied to water, the bicarbonates can release carbon dioxide and revert to their carbonate or "insoluble" state. For this reason, bicarbonate hardness is often referred to as temporary hardness.

Hardness caused by the presence of the soluble chlorides and sulfates of calcium and magnesium are classified as "permanent" because these compounds cannot be removed from water through simple heating.

When these chemical compounds are dissolved in water, their ions are released.

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