This article is from the Water for coffee FAQ, by Jim Schulman with numerous contributions by others.
There are two items that need to be noted prior to doing
calculations from published or test data.
Most tests measure hardness and alkalinity. They do not
measure total dissolved solids (this requires a conductivity test).
But, since calcium, magnesium, and carbonates form the preponderance
of dissolved solids in most natural drinking water, and since total
dissolved solids plays only a small role in the calculations, the
higher of the hardness or alkalinity measures (in CaCO3 equivalent
units) can serve as the total dissolved solids measure with only a
minimal loss of accuracy (The LI will come out about 0.1 to 0.2 too
high for water with lots of other minerals).
Second, acidity in natural water comes from dissolved CO2
(fizz), which can vary quickly. A recent improvement on the Langelier
index, called the Puckorius index, replaces the water's current pH
with its equilibrium pH (pHeq), which derives from the alkalinity
value. When water is exposed to air or heated, this works better as a
long term pH estimate than any current pH reading. The formula is:
pHeq = 1.465*log(A) + 4.54
The following table shows the alkalinity value that is equivalent to
the medium pH levels in drinking water:
EQUILIBRIUM WATER pH VERSUS BICARBONATE ALKALINITY IN mg/L CaCO3
----------------------------------------------------------
pHeq 6. .2 .4 .6 .8 7. .2 .4 .6 .8 8.
Alkalinity 10 14 19 26 35 48 65 90 123 168 230
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