| What is Hard Water? As water passes through soil and rock,
it dissolves and retains tiny amounts of
minerals in solution. Calcium and
magnesium
dissolved
in water are the two most common minerals that
make water "hard." The degree of hardness
becomes greater as calcium and magnesium concentrations
increase. Hard water is not a health risk; it simply contains
a higher concentration of natural minerals. However,
it is a nuisance to equipment and taps, as it
will more likely lead to scale buildup
and generate premature damages. The Water Quality Association has developed a
water hardness table (shown below).
|
|
 |
| |
Water
Hardness Table |
|
|
|
|
Grain per gallon |
PPM |
| |
Soft |
Less
than
1 |
Less than 17.1 |
| |
Slightly Hard |
1 to 3.5 |
17.1 to 60 |
| |
Moderately Hard |
3.5 to 7 |
60 to 120 |
| |
Hard |
7 to 10.5 |
120 to 180 |
| |
Very Hard |
10.5 and up |
180 and up |
|
 |
 |
|
| |
Source: Water Quality Association |
|
Hard water is a common natural
phenomenon. For example, over half of the
United States territory is supplied with water
that is qualified as hard to very hard (see map). How Does
Scale Form? As
mentioned above, the harder the water, the greater
the formation of scale. Scale is the result of the
crystallization of minerals found in water. This
crystallization process is
even more intense in warm water. As water temperature rises,
water minerals such as calcium and magnesium tend
to crystallize,
clump together, and form deposits on the inside
walls
of pipes or any other surface they touch. |