SECTION 1
Historical Context & Motivation
For centuries, chemists recognized that certain substances felt slippery, tasted bitter, and turned plant-based dyes specific colors — all hallmarks of what we now call bases. However, explaining why some bases react vigorously while others barely change the pH of water took decades of theoretical development. Understanding the behavior of weak bases — those that only partially ionize — required the concept of chemical equilibrium and the tools to quantify it.
1884 • Arrhenius Theory of Bases
1923 • Brønsted–Lowry Definition
1909 • The pH Scale
1930s–1940s • ICE Tables Emerge in Textbooks
Strong bases like NaOH dissociate completely, making pH calculations straightforward. But many bases you encounter in biology and everyday life — such as ammonia (NH3) in cleaning products or methylamine in biological reactions — are weak bases. The central question this lesson answers is: How do we calculate the pH of a solution when the base only partially reacts with water?
SECTION 2
Core Principles & Definitions
Before diving into calculations, you need a solid grasp of the foundational ideas that make weak-base pH problems work. These concepts build on what you already know about equilibrium and the pH scale, and they connect directly to the math you will use in an ICE table.
Weak Base
Kb (Base Ionization Constant)
ICE Table
pOH and pH Relationship
KEY TAKEAWAY
SECTION 3
Visual Explanation — The ICE Table Process
The diagram below shows the complete workflow for computing the pH of a weak base solution. It traces the path from writing the balanced equation all the way through to the final pH value, with the ICE table at the center of the process. Follow the arrows to see how each step feeds into the next.
Notice that the ICE table (shown in the purple-bordered box) is the heart of the process. The variable x represents the amount of base that reacts, and because the reaction produces one OH− for every molecule of base that ionizes, x also equals the equilibrium concentration of hydroxide ions. Once you find x, the rest is just logarithms and subtraction.
SECTION 4
Mathematical Framework
Let's formalize each step with equations. A generic weak base B reacts with water in the following equilibrium. We will use ammonia (NH3) as our model weak base throughout this section.
WEAK BASE EQUILIBRIUM
NH3 accepts a proton from water, producing the conjugate acid NH4+ and a hydroxide ion OH−. Water is a pure liquid and is not included in the Kb expression.
Kb EXPRESSION
Kb for ammonia at 25 °C is 1.8 × 10−5. Products go in the numerator; the unreacted base goes in the denominator.
Kb IN TERMS OF x
Here, C0 is the initial molar concentration of the weak base, and x is the equilibrium concentration of OH− (and of the conjugate acid). If C0 / Kb ≥ 400, you may approximate C0 − x ≈ C0.
pOH AND pH CONVERSION
Because weak bases generate OH− rather than H+ directly, you always find pOH first, then convert to pH using the relationship pH + pOH = 14.00 at 25 °C.
The 5% (or "400×") Approximation Rule
SECTION 5
Detailed ICE Table Breakdown
Let's zoom into the ICE table itself. The table below shows how to fill in each row for a general weak base B with initial concentration C0. Understanding the logic behind each entry is just as important as memorizing the pattern.
| B | H₂O | BH⁺ | OH⁻ | |
|---|---|---|---|---|
| Initial (I) | C₀ | — | 0 | ≈ 0 |
| Change (C) | − x | — | + x | + x |
| Equilibrium (E) | C₀ − x | — | x | x |
ICE table for the generic weak base reaction B + H₂O ⇌ BH⁺ + OH⁻
A few important details about filling in the ICE table. First, water is a pure liquid, so it does not appear in the Kb expression and gets a dash in the table. Second, we typically assume the initial concentrations of the products (BH+ and OH−) are zero. Technically, water's autoionization provides a tiny amount of OH− (10−7 M), but for most weak-base problems this is negligible compared to the OH− the base generates.
SECTION 6
Worked Example — pH of 0.15 M Ammonia
Let's calculate the pH of a 0.15 M ammonia (NH3) solution at 25 °C, given Kb = 1.8 × 10−5.
Find the pH of 0.15 M NH₃
- 1
Step 1 — Write the Equilibrium Equation
Ammonia reacts with water: NH3(aq) + H2O(l) ⇌ NH4+(aq) + OH−(aq). The Kb expression is Kb = [NH4+][OH−] / [NH3]. - 2
Step 2 — Set Up the ICE Table
Initial: [NH3] = 0.15 M, [NH4+] = 0, [OH−] = 0. Change: NH3 decreases by x; both products increase by x. Equilibrium: [NH3] = 0.15 − x, [NH4+] = x, [OH−] = x. - 3
Step 3 — Check the Approximation
C0 / Kb = 0.15 / (1.8 × 10−5) = 8333. Since 8333 ≥ 400, we can use the approximation: 0.15 − x ≈ 0.15.Approximation valid ✓ - 4
Step 4 — Solve for x
Substituting into the Kb expression: 1.8 × 10−5 = x² / 0.15. Rearranging: x² = (1.8 × 10−5)(0.15) = 2.7 × 10−6. Taking the square root: x = 1.64 × 10−3 M.[OH−] = 1.64 × 10⁻³ M - 5
Step 5 — Verify Approximation
(1.64 × 10−3 / 0.15) × 100% = 1.1%. This is well below 5%, so the approximation was justified.1.1% < 5% ✓ - 6
Step 6 — Calculate pOH, Then pH
pOH = −log(1.64 × 10−3) = 2.79. pH = 14.00 − 2.79 = 11.21.pH = 11.21
Sanity Check
SECTION 7
Strong Bases vs. Weak Bases — Key Differences
You might wonder: why bother with ICE tables at all? The answer is that the simpler approach you use for strong bases does not work for weak bases. The table below highlights the critical differences between the two types of calculations.
| Feature | Strong Base (e.g., NaOH) | Weak Base (e.g., NH₃) |
|---|---|---|
| Degree of ionization | 100% — dissociates completely | Partial — typically < 5% |
| [OH⁻] calculation | [OH⁻] = C₀ (direct) | Requires Kb and ICE table |
| Equilibrium involved? | No equilibrium — reaction goes to completion | Yes — equilibrium between B, BH⁺, and OH⁻ |
| Typical pH range (moderate conc.) | 13–14 | 8–12 |
| Common examples | NaOH, KOH, Ca(OH)₂ | NH₃, CH₃NH₂, C₅H₅N (pyridine) |
Comparison of strong and weak base pH calculations
KEY TAKEAWAY
SECTION 8
Connection to Ka, Kw, and Buffer Chemistry
The skills you build in this lesson form the foundation for several more advanced acid–base topics. The table below shows how weak-base pH calculations connect to concepts you'll encounter next.
| This Lesson | Advanced Extension |
|---|---|
| Using Kb to find [OH⁻] | Using Ka × Kb = Kw to convert between conjugate acid and base constants. If you know Ka of NH₄⁺, you can find Kb of NH₃ from Kw = 1.0 × 10⁻¹⁴. |
| Single weak base in water | Buffer solutions mix a weak base with its conjugate acid. The Henderson–Hasselbalch equation (pOH = pKb + log([BH⁺]/[B])) replaces the ICE table when both species are present. |
| The 5% approximation | For very dilute or stronger weak bases where the approximation fails, the quadratic formula or successive-approximation method is required. |
| Monoprotic weak bases | Polyprotic bases (like CO₃²⁻) involve two or more Kb values and sequential ICE tables. |
How this lesson connects to upcoming acid–base topics
One of the most important relationships to remember is Ka × Kb = Kw = 1.0 × 10−14 at 25 °C. This means that if you are given the Ka of a conjugate acid, you can always calculate Kb for the base and proceed with the ICE table method you've learned here. Mastering weak-base pH is not an isolated skill — it's the gateway to the entire world of aqueous equilibrium chemistry.
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
A weak base only partially ionizes in water, establishing an equilibrium described by Kb, the base ionization constant. To find the pH of a weak base solution, you write the balanced equilibrium reaction, construct an ICE table (Initial, Change, Equilibrium) to express all concentrations in terms of a single unknown x, and substitute the equilibrium expressions into the Kb formula. When C₀ / Kb ≥ 400, you can use the 5% approximation (C₀ − x ≈ C₀) to avoid the quadratic formula; otherwise, solve exactly.
Once you solve for x = [OH⁻], compute pOH = −log[OH⁻] and then convert using pH = 14.00 − pOH. Always verify your answer: the pH of a weak base solution at moderate concentration should fall between 7 and 14, and the percent ionization should be consistent with the base being "weak." This ICE-table method extends directly to buffer calculations and polyprotic base problems that you will encounter in advanced acid–base chemistry.