strange-steve
Quantum Brewer
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What is alkalinity?
Essentially, alkalinity is a measurement of a solution's pH buffering capacity, its ability to resist change in pH. The higher the alkalinity, the more resistant the water is to a change in pH because the ions responsible for alkalinity neutralise acids by absorbing H⁺ ions. In other words, more acid would be required to lower the pH of high alkalinity water compared to low alkalinity. This seems to be a common source of confusion, because alkalinity often gets conflated or confused with pH, hardness, or basicity, which are related but not the same thing.
Now the water coming from our taps contains various dissolved minerals and ions, some of which contribute to alkalinity. The three main sources of alkalinity are carbonate, bicarbonate, and hydroxide [1]. The carbonate (CO₃⁻²) and bicarbonate (HCO₃⁻) ions typically find their way into water from CO₂ absorption (forming carbonic acid initially) and from geological sources when precipitation runs over or through soil and rock. The hydroxide ions (OH⁻) on the other hand are a natural part of water due to the self-ionisation reaction mentioned earlier.
The alkalinity equation
So the total alkalinity is a sum of these negatively charged ions minus the positively charged hydrogen ions:
Alkalinity = (carbonate x 2) + bicarbonate + hydroxide - hydrogen ion
(Note: carbonate is multiplied by 2 because it has a -2 charge meaning it can react with 2 H⁺ ions)
To help get a more intuitive understanding of this and how it applies, let's look at some simplified examples. Pure water, with no carbonate or bicarbonate, and equal amounts of hydrogen and hydroxide ions (ie pH neutral) will have an alkalinity of 0:
Alkalinity = (0 x 2) + 0 + 1 - 1 = 0
This also helps us see the relationship between alkalinity and pH. Typically as the pH gets lower (ie H⁺ increases) the alkalinity will reduce and as pH increases, so does alkalinity. Look at the following two sums, the first one is a basic solution (more hydroxide than H⁺) and the second one is acidic:
Alk = (4 x 2) + 4 + 8 - 6 = 14
Alk = (4 x 2) + 4 + 6 - 8 = 10
Notice that when the carbonate and bicarbonate remain the same, but the pH is reduced it results in lower alkalinity. Now these aren't real world examples, these numbers don't mean anything, but hopefully they help you to get a more intuitive understanding of how alkalinity and pH are linked but are not the same.
Essentially, alkalinity is a measurement of a solution's pH buffering capacity, its ability to resist change in pH. The higher the alkalinity, the more resistant the water is to a change in pH because the ions responsible for alkalinity neutralise acids by absorbing H⁺ ions. In other words, more acid would be required to lower the pH of high alkalinity water compared to low alkalinity. This seems to be a common source of confusion, because alkalinity often gets conflated or confused with pH, hardness, or basicity, which are related but not the same thing.
Now the water coming from our taps contains various dissolved minerals and ions, some of which contribute to alkalinity. The three main sources of alkalinity are carbonate, bicarbonate, and hydroxide [1]. The carbonate (CO₃⁻²) and bicarbonate (HCO₃⁻) ions typically find their way into water from CO₂ absorption (forming carbonic acid initially) and from geological sources when precipitation runs over or through soil and rock. The hydroxide ions (OH⁻) on the other hand are a natural part of water due to the self-ionisation reaction mentioned earlier.
The alkalinity equation
So the total alkalinity is a sum of these negatively charged ions minus the positively charged hydrogen ions:
Alkalinity = (carbonate x 2) + bicarbonate + hydroxide - hydrogen ion
(Note: carbonate is multiplied by 2 because it has a -2 charge meaning it can react with 2 H⁺ ions)
To help get a more intuitive understanding of this and how it applies, let's look at some simplified examples. Pure water, with no carbonate or bicarbonate, and equal amounts of hydrogen and hydroxide ions (ie pH neutral) will have an alkalinity of 0:
Alkalinity = (0 x 2) + 0 + 1 - 1 = 0
This also helps us see the relationship between alkalinity and pH. Typically as the pH gets lower (ie H⁺ increases) the alkalinity will reduce and as pH increases, so does alkalinity. Look at the following two sums, the first one is a basic solution (more hydroxide than H⁺) and the second one is acidic:
Alk = (4 x 2) + 4 + 8 - 6 = 14
Alk = (4 x 2) + 4 + 6 - 8 = 10
Notice that when the carbonate and bicarbonate remain the same, but the pH is reduced it results in lower alkalinity. Now these aren't real world examples, these numbers don't mean anything, but hopefully they help you to get a more intuitive understanding of how alkalinity and pH are linked but are not the same.