The carbonic acid / bicarbonate / carbonate buffering system is very important in an aquarium and largely controls both the pH and the resistance to change of the pH in the water.  These three carbonate-based species can all interconvert in a connected equilibrium reaction:

(1)  H2CO3 (carbonic acid) ⇌ H+ + HCO3 (bicarbonate) ⇌ 2H+ + CO3-2 (carbonate)

H+ is shorthand for the hydronium H3O+ ion.  The concentration of H+ (notated as [H+]) is what determines pH.  pH is calculated as:

(2)  pH = -log10[H+]

So when [H+] = 1e-7M the pH is -log10(1e-7) = 7.0 which is considered ‘neutral pH’.

Collectively, the amount of HCO3 (bicarbonate) and CO3-2 (carbonate) set the water’s ‘alkalinity‘ which is sometimes reported as the ‘dKH’ value.

Equilibrium concentrations of carbonic acid, bicarbonate and carbonate

The relative fraction of carbonic acid vs. bicarbonate vs. carbonate is entirely determined by the pH of the water.  At lower pH (more acidic) the equilibrium shifts away from carbonate through bicarbonate and winds up as carbonic acid.  The reverse is true at high pH.  As the “middle ground” bicarbonate represents the majority of the species over a range of pH near neutral, including most of the typical pH values an aquarium might have.

The equilibrium for each of the carbonate-based species is the concentration(s) at which the relative amounts of each species are stable and unchanging, because under equilibrium conditions the rate of forward and reverse reactions are the same.   This includes H3O+ so at equilibrium the pH is also stable.  These equilibrium concentrations can be described as follows:

(3)  [H+] x [HCO3] / H2CO3 = Ka1

(4′)  [H+] x [H+] x [CO3-2] / [H+] / [HCO3] = Ka2   which simplifies to…

(4)  [H+] x [CO3-2] / [HCO3] = Ka2

Ka1 and Ka2 are the equilibrium constants for these reactions.  You will often see these equilibrium constants expressed as pKa1 and pKa2 where by exact analogy to how pH relates to [H+] by pH = -log10[H+], pKa1 = -log10[Ka1] and pKa2 = -log10[Ka2].  Whilst pKa2 is well-known to be 10.3, the value for pKa1 is still being debated, with a recent determination of 3.49.  Part of the challenge with measuring pKa1 is that H2CO3 can also spontaneously react with water along this scheme:

(5)  H2CO3 (carbonic acid) ⇌ H2O + CO2

This last reaction has an equilibrium that very heavily favors CO2 over H2CO3, which is important in a planted aquarium since dissolved CO2 gas is the major source of carbon for submersed plants.  If we assume the concentration of water in this reaction is constant, then the equilibrium constant for conversion of carbonic acid to carbon dioxide is around 667 so carbonic acid at equilibrium is about 0.15% of the carbon dioxide concentration.  This rapid conversion of carbonic acid to something other than bicarbonate is part of what makes determining Ka1 so challenging.

Relative amounts of carbonic acid, bicarbonate and carbonate

If the pH changes, the relative amounts of the three carbonate-based species will also change, establishing new equilibrium concentrations one relative to the other at the new pH.  The reverse is also true, so if for example growing plants consume dissolved carbon dioxide, that will lower the concentration of carbonic acid which will in turn affect (raise) the pH, again rebalancing the relative distribution of the three carbonate-based species to a new equilibrium.

Knowing the pH and the two equilibrium constants Ka1 and Ka2 the relative fraction carbonic acid, bicarbonate and carbonate can be calculated.  After some algebra (left as an exercise for the reader) this works out to:

(6)  fraction of  H2CO3 (carbonic acid) = [H+] / ([H+] + Ka1 + Ka1 x Ka2 / [H+])

(7)  fraction of HCO3 (bicarbonate) = Ka1 / ([H+] + Ka1 + Ka1 x Ka2 / [H+])

(8)  fraction of CO3-2 (carbonate) = Ka2 / ([H+] + Ka2 + [H+] x [H+] / Ka1)

Of course, these three relative amounts add up to exactly 1.0 and are dependent on pH and the two equilibrium constants.  There is also a dependence on both temperature and the amount of salt in the water to a certain extent which can be modeled by adjusting the Ka1 and Ka2 values suitably if needed.

Bjerrum plot of carbonate equilibria

Bjerrum plot of carbonate equilibria
relative fraction of carbonic acid, bicarbonate and carbonate vs. pH

Plotting these relative fractions vs. pH gives an interesting graph.  Shown here is the result for pKa1 = 3.49 and pKa2 = 10.3 over a range of pH values, remembering to convert the pKa values to their respective Ka values when using the equations.  You can see from the graph that between pH 5 and 9 the bicarbonate will represent over 95% of the three different carbonate species.  Note that here we show carbonic acid and not carbon dioxide.  The interconversions between carbonic acid, bicarbonate and carbonate are all protonations and reach equilibrium very quickly, but the interconversion between carbonic acid and carbon dioxide is a legitimate chemical reaction which under some circumstances can take a long time to reach equilibrium.

Carbon dioxide vs. bicarbonate vs. carbonate

Bjerrum plot of carbonate equilibria
relative fraction of dissolved carbon dioxide, bicarbonate and carbonate vs. pH

Of perhaps more general relevance is a plot of dissolved CO2 vs. other carbonate species.  This uses a pKa1 = 6.35 which accounts for the linked equilibria between dissolved CO2 and carbonic acid.  Bicarbonate is still the dominant species at most aquarium-relevant pH values.

The absolute amount of dissolved CO2 gas in aquarium water is a constant value

Note that the graphs show the relative levels of the species, not the absolute levels.  Under conditions where the aquarium is open to atmosphere (doesn’t have a lid) the absolute level of dissolved CO2 gas is set by the level of atmospheric CO2 and temperature and not by pH.  It might seem from the graph like you could boost levels of dissolved CO2 gas in the water by keeping the pH (and necessarily also the alkalinity) low, but this doesn’t actually work.  Instead what happens is CO2 levels equilibrate to a constant value and is it the total amount of both bicarbonate and carbonate that is affected by changing the pH.  As pH is increased exponentially more bicarbonate and carbonate are produced from the unchanging amount of carbonic acid (and thereby dissolved CO2) present.

Exact solution for CO2, H2CO3, HCO3, CO3-2

log transformed fractional carbonate species graph
log10 transformed fractional carbonate species equilibria by pH

For the sake of completeness, it is straightforward to find exact solutions to the relative fraction of all four species, however, since the relationship between CO2 and H2CO3 is not dependent on pH, and H2CO3 is always a small fraction of CO2, the graph of the four species with respect to pH is nearly identical to the one above for three species using pKa1 = 6.35, with the amount of H2CO3 remaining small over all pH.  If the hydration of CO2 has an equilibrium:

(9)  [H2CO3] / [CO2] / [H2O] = Khyd ≈ 1.5e-3 (with water assumed constant at 55.56M)

Then the relative fractions of CO2, H2CO3, HCO3 and CO3-2 are:

(10)  CO2 fx = 1 / (1 + Khyd + Khyd x Ka1 / [H+] + Khyd x Ka1 x Ka2 / [H+] / [H+])

(11)  H2CO3 fx = 1 / (1 + 1 / Khyd + Ka1 / [H+] + Ka1 x Ka2 / [H+] / [H+])

(12)  HCO3 fx = 1 / (1 + [H+] / Ka1 + [H+] / Khyd / Ka1 + Ka2 / [H+])

(13)  CO3-2 fx = 1 / (1 + [H+] / Ka2 + [H+] x [H+] / Ka1 / Ka2 + [H+] x [H+] / Khyd / Ka1 / Ka2

Shown here is the fractional equilibrium concentrations of the four different carbonate-based species at a given pH, using Ka1 = 3.24e-4 and Ka2 = 5.01e-11.  This graph is log10 transformed to better illustrate the minor components.  To find the actual concentrations, raise 10 to the indicated power shown on the Y-axis, so 0 → 100 = 1.0 = 100%; -1 → 10-1 = 0.1 = 10%; -2 → 10-2 = 0.01 = 1% etc.

One more reaction path for CO2

Not discussed above and not influencing the equilibrium values or how they are calculated, there is a second reaction path available by which bicarbonate can interconvert to carbon dioxide:

(14)  CO2 + OH ⇌ HCO3

In this hydroxylation reaction, dissolved carbon dioxide reacts with the hydroxyl ion to form the bicarbonate ion.  The equilibrium for this reaction is:

(15)  [HCO3 ] / [CO2] / [OH] = Koh ≈ 3.02e7

Unlike the hydration of carbon dioxide to carbonic acid, which is independent of pH, the hydroxylation reaction is pH dependent.  The very well known self-ionisation of water follows this scheme:

(16)  [H+] x [OH] = Kw = 1e-14

such that:

(17)  [HCO3 ] x [H+] / [CO2]  = Kw x Koh ≈ 1e-14 x 3.02e7 ≈ 3.02e-7

It doesn’t matter which equilibrium pathway you use to calculate the amount of CO2 as the amounts will work out to be the same either way – at least to within an approximation of how accurately the various equilibrium constants have been determined.

Leave a Reply

Your email address will not be published. Required fields are marked *

You may use these HTML tags and attributes:

<a href="" title=""> <abbr title=""> <acronym title=""> <b> <blockquote cite=""> <cite> <code> <del datetime=""> <em> <i> <q cite=""> <s> <strike> <strong>