SECTION 1
Historical Context & Motivation
Many of the acids you encounter every day — from phosphoric acid in soft drinks to carbonic acid in sparkling water — have more than one hydrogen that can be donated to water. These are called polyprotic acids, and understanding how they behave is essential to explaining everything from blood chemistry to ocean acidification. The study of acids with multiple ionizable protons unfolded over more than a century, driven by improvements in measurement techniques and theoretical models.
1834 • Faraday Defines 'Acid'
1884 • Arrhenius Theory
1909 • pH Scale Introduced
1923 • Brønsted-Lowry Theory
1960s • Computer-Aided Equilibrium
The central question these advances raised is straightforward yet powerful: if a single acid molecule can lose more than one proton, how do we figure out how many protons are actually lost at a given pH, and which form of the acid is most abundant in solution? That is exactly what this lesson will teach you to do.
SECTION 2
Core Principles & Definitions
Before diving into calculations, you need a solid grasp of the key ideas that govern polyprotic acid behavior. Unlike a monoprotic acid (such as HCl), which donates only one proton, a polyprotic acid donates its protons in distinct, sequential steps. Each step has its own equilibrium constant, and each step is weaker than the one before it.
Stepwise Dissociation
Decreasing Kₐ Values
Dominant Species
pKₐ as a Boundary
KEY TAKEAWAY
SECTION 3
Visualizing Stepwise Dissociation
The diagram below shows the stepwise dissociation of phosphoric acid (H3PO4), a triprotic acid with three dissociation steps. Notice how each arrow represents one proton being donated to water, and how the Ka decreases dramatically at each step.
The dramatic decrease in Ka from one step to the next is not a coincidence — it reflects a fundamental physical reality. Once an acid has lost a proton, it carries a negative charge. Removing a positively charged proton from a negatively charged ion requires fighting an increasingly strong electrostatic attraction. This principle ensures that in most problems, only the first dissociation significantly affects the pH.
SECTION 4
Mathematical Framework
Every polyprotic acid problem relies on writing the correct equilibrium expressions for each dissociation step and recognizing which one matters most. Let's use a generic diprotic acid H2A as our model. It has two dissociation steps.
FIRST DISSOCIATION
H2A = fully protonated acid; HA⁻ = intermediate (conjugate base of step 1); Ka1 = acid dissociation constant for the first proton.
SECOND DISSOCIATION
HA⁻ = intermediate species; A²⁻ = fully deprotonated form; Ka2 = acid dissociation constant for the second proton. Typically Ka2 ≪ Ka1.
SIMPLIFICATION RULE
Because Ka2 is so much smaller, the second step contributes negligible additional H⁺. The concentration of the fully deprotonated form [A²⁻] ≈ Ka2 (see the shortcut explanation in Section 4 below).
DOMINANT SPECIES RULE
Compare the solution pH to the pKa values. The species that exists in the region surrounding the current pH is the dominant species. At pH = pKa, two species are present in equal concentrations.
Remember This Shortcut
SECTION 5
Identifying the Dominant Species
The concept of dominant species is one of the most practical tools in acid-base chemistry. Given a polyprotic acid and a known pH, you can instantly determine which form of the acid is present in the greatest amount by comparing the pH to the pKa values. The diagram below maps out the dominant species regions for carbonic acid (H2CO3), a diprotic acid that plays a critical role in blood buffering and ocean chemistry.
This map is incredibly useful. For example, if you know that blood has a pH of about 7.4, you can glance at the diagram and immediately see that 7.4 falls between pKa1 and pKa2, which means bicarbonate (HCO₃⁻) is the dominant species in blood. This is exactly why your body's primary blood buffer is the carbonic acid–bicarbonate system.
| Acid | pKₐ₁ | pKₐ₂ | pKₐ₃ |
|---|---|---|---|
| Sulfurous acid (H₂SO₃) | 1.81 | 6.91 | — |
| Carbonic acid (H₂CO₃) | 6.35 | 10.33 | — |
| Phosphoric acid (H₃PO₄) | 2.15 | 7.20 | 12.35 |
| Citric acid (H₃C₆H₅O₇) | 3.13 | 4.76 | 6.40 |
| Oxalic acid (H₂C₂O₄) | 1.25 | 4.27 | — |
Common Polyprotic Acids and Their pKₐ Values
SECTION 6
Worked Example — Carbonic Acid
Let's solve a complete introductory polyprotic acid problem step by step. We'll find the pH and identify the dominant species when 0.10 M carbonic acid (H2CO3) is dissolved in water. Given: Ka1 = 4.3 × 10⁻⁷ and Ka2 = 4.7 × 10⁻¹¹. Note: The Ka1 value of 4.3 × 10⁻⁷ is the conventional apparent Ka1 for the carbonate system as it exists in water, which includes dissolved CO2 in equilibrium with H2CO3. This is the value most commonly used in general chemistry and is the standard convention for problems involving the carbonate system.
Finding pH of 0.10 M H₂CO₃
- 1
Step 1 — Check the Simplification Rule
Calculate Ka1 / Ka2 = (4.3 × 10⁻⁷) / (4.7 × 10⁻¹¹) ≈ 9,100. Since this is much greater than 100, we can treat the first dissociation as a simple monoprotic acid problem and ignore the second dissociation's contribution to [H⁺].Kₐ₁ / Kₐ₂ ≈ 9,100 ≫ 100 → Use Kₐ₁ only - 2
Step 2 — Set Up ICE Table for First Dissociation
Write the equilibrium: H₂CO₃ ⇌ H⁺ + HCO₃⁻. Initial concentrations: [H₂CO₃] = 0.10 M, [H⁺] = 0, [HCO₃⁻] = 0. Change: −x, +x, +x. Equilibrium: (0.10 − x), x, x. - 3
Step 3 — Write and Solve the Kₐ₁ Expression
Ka1 = x² / (0.10 − x) = 4.3 × 10⁻⁷. Since Ka1 is very small compared to 0.10, we can approximate 0.10 − x ≈ 0.10. Then x² = (4.3 × 10⁻⁷)(0.10) = 4.3 × 10⁻⁸. Taking the square root: x = √(4.3 × 10⁻⁸) ≈ 2.07 × 10⁻⁴ M.[H⁺] = x ≈ 2.07 × 10⁻⁴ M - 4
Step 4 — Calculate pH
pH = −log[H⁺] = −log(2.07 × 10⁻⁴) ≈ 3.68.pH ≈ 3.68 - 5
Step 5 — Identify the Dominant Species
Compare pH = 3.68 to the pKa values. Using the given Ka1 = 4.3 × 10⁻⁷: pKa1 = −log(4.3 × 10⁻⁷) ≈ 6.37. The reference table lists pKa1 = 6.35, a slight difference due to rounding of the Ka1 value. Either way, pKa2 = −log(4.7 × 10⁻¹¹) ≈ 10.33. Since pH (3.68) < pKa1 (6.35–6.37), the fully protonated form is dominant.Dominant species: H₂CO₃ - 6
Step 6 — Find [CO₃²⁻] (Bonus Insight)
A useful shortcut: when you dissolve a diprotic acid, the concentration of the fully deprotonated species equals Ka2. Here is why: the ICE table for the first dissociation gives [H⁺] ≈ [HCO₃⁻] = x ≈ 2.07 × 10⁻⁴ M. Substituting into the Ka2 expression: Ka2 = [H⁺][CO₃²⁻] / [HCO₃⁻]. Because [H⁺] ≈ [HCO₃⁻] from step 1, these terms cancel, giving [CO₃²⁻] ≈ Ka2 = 4.7 × 10⁻¹¹ M. This shortcut is valid because [H⁺] ≈ [HCO₃⁻] holds when the first dissociation dominates (Ka1 / Ka2 ≫ 100). This confirms the second dissociation barely occurs.[CO₃²⁻] ≈ 4.7 × 10⁻¹¹ M
SECTION 7
Monoprotic vs. Polyprotic: Key Differences
Students often wonder: "Why can't I just treat a polyprotic acid exactly like a monoprotic acid?" In many ways you can — and that's the beauty of the simplification rule. But there are important differences to keep in mind.
| Feature | Monoprotic Acid | Polyprotic Acid |
|---|---|---|
| Number of ionizable H⁺ | 1 | 2 or more (diprotic, triprotic, etc.) |
| Equilibrium expressions | 1 Kₐ expression | Separate Kₐ for each step (Kₐ₁, Kₐ₂, ...) |
| pH calculation | One ICE table | Usually one ICE table (Kₐ₁ only), with [A²⁻] ≈ Kₐ₂ |
| Dominant species question | Either HA or A⁻ | Multiple possible forms (H₂A, HA⁻, A²⁻) |
| Titration curve | 1 equivalence point | Multiple equivalence points (1 per proton) |
Monoprotic vs. Polyprotic Acid Comparison
KEY TAKEAWAY
SECTION 8
Connection to Advanced Theory
The introductory approach you've learned here — treating only the first dissociation and using pKa boundaries to identify dominant species — is a powerful starting point. As you advance, you'll encounter situations where the simplification breaks down and more sophisticated techniques are needed.
| Topic | Introductory Level (This Lesson) | Advanced Level (Future Topics) |
|---|---|---|
| pH calculation | Use Kₐ₁ only with an ICE table | Solve simultaneous equilibria; alpha (α) fraction equations |
| Dominant species | Compare pH to pKₐ values | Calculate exact fractions using alpha expressions: α₀, α₁, α₂ |
| Titration | Recognize multiple equivalence points | Calculate pH at each equivalence point and half-equivalence point |
| Buffers | Understand that pKₐ = pH at equal concentrations | Design polyprotic buffers; use Henderson-Hasselbalch for each step |
| Special cases | Assume Kₐ₁ ≫ Kₐ₂ | Handle cases where Kₐ values are close (e.g., sulfuric acid's second dissociation) |
Introductory vs. Advanced Polyprotic Acid Analysis
One particularly important advanced topic is the pH of an amphoteric species — the intermediate form like HA⁻ that can act as either an acid or a base. In future courses, you'll learn that the pH of a solution of the intermediate is approximately (pKa1 + pKa2) / 2. For now, just know that this connection exists and that your understanding of stepwise dissociation lays the groundwork for it.
SECTION 9
Practice Problems
Question 1: CONCEPTUAL
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Question 2: BASIC CALCULATION
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Question 3: INTERMEDIATE
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Question 4: APPLIED
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Question 5: CRITICAL THINKING
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SUMMARY
Lesson Summary
Summary
Polyprotic acids donate protons in stepwise dissociations, each governed by its own equilibrium constant (Kₐ₁, Kₐ₂, Kₐ₃). Each successive Ka is much smaller than the last because removing a proton from an increasingly negative ion is harder. When Kₐ₁ / Kₐ₂ > 100, you can simplify the problem by treating only the first dissociation with an ICE table to find the pH — exactly like a monoprotic weak acid problem.
To identify the dominant species at any given pH, compare the pH to the pKₐ values: if pH < pKa1, the fully protonated form dominates; if pKa1 < pH < pKa2, the intermediate form dominates; if pH > pKa2, the fully deprotonated form dominates. A bonus shortcut: when dissolving the fully protonated diprotic acid, [A²⁻] ≈ Kₐ₂ (because [H⁺] ≈ [HA⁻] from the first dissociation, so these terms cancel in the Kₐ₂ expression). These tools prepare you for more advanced topics like polyprotic titrations and buffer design.