Stepwise ionisation

Pour acid on your tongue and it feels like a single sour jolt — but if the acid carries more than one ionisable hydrogen, that jolt is really the sum of several separate handoffs of a proton, each easier or harder than the last. Carbonic acid, H2CO3\text{H}_2\text{CO}_3, the fizz in soda water and a key player in blood pH, does not fling off both its protons at once. It gives up the first quite readily and clings hard to the second. This staged release — stepwise ionisation — governs every polybasic acid and polyacidic base you will meet in Equilibrium, from carbonic and phosphoric acid to sulfide and carbonate ions acting as bases. Understanding why each step is harder than the one before, and knowing that this lets you often ignore every step but the first when calculating pH, is the practical payoff of this article.

The core insight

A polybasic acid or polyacidic base loses (or gains) its protons one at a time in successive equilibria, each with its own ionisation constant, and because the departing proton finds it progressively harder to leave an increasingly negative (or, for bases, increasingly less charged) species, the constants fall sharply at each step: Ka1≫Ka2≫Ka3K_{a1} \gg K_{a2} \gg K_{a3}.

The core idea

Why "stepwise" and not "all at once". A polybasic (polyprotic) acid such as H2AH_2A has more than one ionisable hydrogen, but chemically it cannot lose them simultaneously — each proton departs in its own distinct equilibrium, with its own equilibrium constant. Writing a single combined equation such as H2A⇌2H++A2−H_2A \rightleftharpoons 2H^+ + A^{2-} hides this staged structure and is not how the ionisation constants are defined or used. For a diprotic acid, the two steps and their constants are:

H2A⇌H++HA−Ka1=[H+][HA−][H2A]H_2A \rightleftharpoons H^+ + HA^- \qquad K_{a1} = \dfrac{[H^+][HA^-]}{[H_2A]}
HA−⇌H++A2−Ka2=[H+][A2−][HA−]HA^- \rightleftharpoons H^+ + A^{2-} \qquad K_{a2} = \dfrac{[H^+][A^{2-}]}{[HA^-]}

where: Ka1K_{a1} and Ka2K_{a2} are the first and second (stepwise) ionisation constants, and [ ][\ ] denotes equilibrium molar concentration. For a triprotic acid such as H3PO4\text{H}_3\text{PO}_4 a third analogous step follows, with constant Ka3K_{a3}.

The universal trend. For any polybasic acid, successive constants fall sharply — typically by a factor of 10410^4 to 10610^6 at each step:

Ka1≫Ka2≫Ka3K_{a1} \gg K_{a2} \gg K_{a3}

The same staged logic, and the same decreasing trend in successive KbK_b values, applies to polyacidic bases (species that accept more than one proton), though ISC problems most commonly work with polybasic acids.

Why each step is harder. Once the first proton leaves, the remaining species (HA−HA^-) is negatively charged, and this negative charge electrostatically attracts the departing proton more strongly than the neutral parent H2AH_2A did — so removing the second proton takes more energy and happens far less readily. Remove that proton too, and the species is even more negative, making the third departure (where relevant) harder still. The pattern is not an arbitrary numerical coincidence; it is charge bookkeeping.

The practical payoff. Because Ka1≫Ka2K_{a1} \gg K_{a2}, almost all of the H+H^+ in a polybasic acid solution comes from the first ionisation step alone — the second (and further) steps contribute a concentration of H+H^+ that is negligible by comparison. This is what lets pH calculations for polybasic acids be done, to excellent approximation, as if the acid were monoprotic using only Ka1K_{a1}. It is also why, when comparing acid strength across different acids, chemists compare Ka1K_{a1} (or the single KaK_a of a monobasic acid) — a larger KaK_a signals a more extensively ionised, stronger acid, and likewise a larger KbK_b signals a stronger base.

Figure
Bar chart comparing the first and second ionisation constants of carbonic acid on a logarithmic scale showing Ka1 far larger than Ka2
Successive ionisation constants of H2CO3 fall sharply ionisation step Ka (log scale) Ka1 = 4.3 x 10^-7 step 1: H2CO3 to H+ + HCO3- Ka2 = 4.8 x 10^-11 step 2: HCO3- to H+ + CO3(2-) the second bar is about 9000 times shorter than the first
Derivation ARatio and dominance of the first ionisation step

The goal is to show, using only the definitions of Ka1K_{a1} and Ka2K_{a2} and the algebra of an equilibrium approximation, that a polybasic acid's [H+][H^+] is fixed almost entirely by its first ionisation step whenever Ka1≫Ka2K_{a1} \gg K_{a2}, so that the second step can be dropped from a pH calculation without meaningful error — the same reasoning that justifies treating H2CO3\text{H}_2\text{CO}_3 as if it were a monoprotic acid of strength Ka1K_{a1}.

Step 1. Set up the first ionisation of a diprotic acid H2AH_2A at initial concentration CC, using an ICE table: [H2A]≈C−x[H_2A] \approx C - x, [H+]=x[H^+] = x, [HA−]=x[HA^-] = x, so Ka1=x2C−xK_{a1} = \dfrac{x^2}{C - x}. When Ka1K_{a1} is small compared with CC (true for weak acids), x≪Cx \ll C and Ka1≈x2/CK_{a1} \approx x^2/C, giving x=Ka1Cx = \sqrt{K_{a1}C} as the [H+][H^+] contributed by step one.

Step 2. Estimate the extra H+H^+ that the second step could add. Treating [HA−]≈x[HA^-] \approx x as the starting concentration for step two, and letting yy be the small additional ionisation, Ka2≈y2x  ⟹  y=Ka2 xK_{a2} \approx \dfrac{y^2}{x} \implies y = \sqrt{K_{a2}\,x}.

Step 3. Compare yy with xx using the ratio Ka2/Ka1K_{a2}/K_{a1}. Since y=Ka2xy = \sqrt{K_{a2}x} and x=Ka1Cx = \sqrt{K_{a1}C}, the ratio y/x=Ka2/Ka1×(a factor close to 1)y/x = \sqrt{K_{a2}/K_{a1}} \times (\text{a factor close to }1). Because Ka1≫Ka2K_{a1} \gg K_{a2} (typically by 10410^4–10610^6), the ratio Ka2/Ka1K_{a2}/K_{a1} is tiny, so its square root — while larger than the ratio itself — is still small enough that y≪xy \ll x.

Step 4. Conclude: the second ionisation step adds a genuinely negligible amount to [H+][H^+] compared with the first. So for a polybasic acid, [H+]≈x=Ka1C[H^+] \approx x = \sqrt{K_{a1}C} is an excellent approximation, and the acid can be treated, for pH purposes, as if Ka1K_{a1} were its only ionisation constant — exactly the shortcut used throughout the worked example below.

Worked example

Extending carbonic acid to check the approximation numerically. A 0.10 M0.10\ M solution of H2CO3\text{H}_2\text{CO}_3 has Ka1=4.3×10−7K_{a1} = 4.3\times10^{-7} and Ka2=4.8×10−11K_{a2} = 4.8\times10^{-11}. Find [H+][H^+] using only the first ionisation, confirm the second step is negligible, and then use the ratio Ka1/Ka2K_{a1}/K_{a2} to comment on relative step sizes.

Step 1. Write the first-ionisation ICE table: [H2CO3]eq≈0.10−x[\text{H}_2\text{CO}_3]_{eq} \approx 0.10 - x, [H+]=x[H^+] = x, [HCO3−]=x[\text{HCO}_3^-] = x, with x≪0.10x \ll 0.10 expected since Ka1K_{a1} is small.

Step 2. Apply the small-xx approximation: Ka1≈x20.10=4.3×10−7  ⟹  x2=4.3×10−8K_{a1} \approx \dfrac{x^2}{0.10} = 4.3\times10^{-7} \implies x^2 = 4.3\times10^{-8}.

Step 3. Solve: x=4.3×10−8≈2.07×10−4 Mx = \sqrt{4.3\times10^{-8}} \approx 2.07\times10^{-4}\ M, so [H+]≈2.1×10−4 M[H^+] \approx 2.1\times10^{-4}\ M from the first step, and [HCO3−]≈2.1×10−4 M[\text{HCO}_3^-] \approx 2.1\times10^{-4}\ M.

Step 4. Estimate the second step's extra H+H^+: let yy be the additional ionisation from HCO3−\text{HCO}_3^-; y2≈Ka2×[HCO3−]≈4.8×10−11×2.1×10−4≈1.0×10−14y^2 \approx K_{a2} \times [\text{HCO}_3^-] \approx 4.8\times10^{-11}\times 2.1\times10^{-4} \approx 1.0\times10^{-14}, so y≈1.0×10−7 My \approx 1.0\times10^{-7}\ M — over 20002000 times smaller than xx, confirming the approximation.

Step 5. Compute Ka1/Ka2=4.3×10−74.8×10−11≈9.0×103K_{a1}/K_{a2} = \dfrac{4.3\times10^{-7}}{4.8\times10^{-11}} \approx 9.0\times10^{3}: the first ionisation is roughly 90009000 times more extensive than the second, which is exactly why y≪xy \ll x above and why the electrostatic-attraction argument (the doubly-negative CO32−\text{CO}_3^{2-} that would form holds its neighbouring proton far more tightly than neutral H2CO3\text{H}_2\text{CO}_3 does) is quantitatively confirmed, not just qualitatively plausible. Final answer: [H+]≈2.1×10−4 M[H^+] \approx 2.1\times10^{-4}\ M (pH ≈3.68\approx 3.68), essentially unchanged by including the second ionisation step.

Competitive stretch

For a triprotic acid like H3PO4\text{H}_3\text{PO}_4 (Ka1≈7.5×10−3K_{a1} \approx 7.5\times10^{-3}, Ka2≈6.2×10−8K_{a2} \approx 6.2\times10^{-8}, Ka3≈4.2×10−13K_{a3} \approx 4.2\times10^{-13}), the same reasoning applies twice over: Ka1/Ka2≈1.2×105K_{a1}/K_{a2} \approx 1.2\times10^{5} and Ka2/Ka3≈1.5×105K_{a2}/K_{a3} \approx 1.5\times10^{5}, so essentially all the H+H^+ in a phosphoric acid solution again comes from the first step. Note that Ka1K_{a1} here is far larger than either carbonic constant — phosphoric acid is simply a stronger acid at its first step, an entirely separate comparison from how sharply its own steps fall relative to each other.

Common traps

  • Adding all steps as if each contributes equally to [H+][H^+]. With Ka1≫Ka2≫Ka3K_{a1} \gg K_{a2} \gg K_{a3}, only the first step is needed for an accurate [H+][H^+]; summing all three overstates the acid's strength.
  • Writing one combined equation instead of separate stepwise equilibria. H2CO3⇌2H++CO32−\text{H}_2\text{CO}_3 \rightleftharpoons 2H^+ + \text{CO}_3^{2-} in a single step is chemically wrong; ionisation genuinely proceeds one proton at a time, each with its own KaK_a and its own equilibrium.
  • Treating the falling KaK_a values as an unexplained pattern. The drop from Ka1K_{a1} to Ka2K_{a2} (and to Ka3K_{a3}) follows directly from increasing electrostatic attraction between the departing proton and a progressively more negative conjugate base — always be ready to say why, not just quote the trend.
  • Assuming [HA−][HA^-] from step one is untouched by step two. Strictly, HA−HA^- is produced in step one and partly consumed in step two; the amount consumed is negligible only because Ka2≪Ka1K_{a2} \ll K_{a1} — that inequality is the justification for ignoring it, not a free pass to ignore it always.

Ask the tutor: Want to see how the first-ionisation shortcut extends to a full phosphoric-acid pH calculation, or how stepwise ionisation feeds into the next hydrolysis and buffer articles?

Why can't a diprotic acid just lose both protons in one step?

Because the two hydrogens are not equivalent once ionisation begins. The first proton leaves a neutral molecule, which is relatively easy. Removing the second proton means pulling a positively charged H+H^+ away from a species, HA−HA^-, that is already negatively charged — the electrostatic attraction between them is stronger, so it needs more energy and happens far less readily. Chemically, these are two distinct equilibria with two distinct constants, not one combined event, so they must be written and treated separately.

If Ka2 is so small, why bother writing the second ionisation equation at all?

Because Ka2K_{a2} still matters for questions that specifically ask about the second step — such as finding [CO32−][\text{CO}_3^{2-}] in carbonic acid, or working out buffer or hydrolysis behaviour involving the fully deprotonated species later in the course. It is only negligible for calculating overall [H+][H^+], not chemically absent. Dropping it from your pH calculation is a justified approximation, not a claim that the second ionisation does not happen.

Does the same Ka1 much greater than Ka2 pattern apply to polyacidic bases too?

Yes. A polyacidic base accepts protons one at a time, and each successive KbK_b is smaller than the one before, for an analogous electrostatic reason — once the base has accepted one proton it becomes positively charged (or less negative), making it harder to attract a second proton. ISC problems mostly use polybasic acids as worked examples, but the same stepwise logic and the same "use the first step's constant" shortcut carry over directly to bases.

Before this

Where this leads