How to Calculate pH & pOH — Strong/Weak Acids

Introduction

Understanding how to calculate pH and pOH is fundamental to chemistry, biology, and environmental science. pH quantifies the acidity or alkalinity of a solution, influencing everything from enzyme function to water quality. While the core concept is simple—pH is the negative log of hydrogen ion concentration—the calculations become nuanced when dealing with strong acids, weak acids, bases, and buffers. This comprehensive guide walks you through the step-by-step methods for each scenario, explains when to use approximations versus exact solutions (like the quadratic formula), and clarifies the role of Ka, pKa, and ICE tables. With practical examples and pro tips, you’ll gain the confidence to tackle any acid-base problem.

The Foundation: Water, pH, and pOH

All pH calculations stem from the autoionisation of water:

H₂O ⇌ H⁺ + OH⁻

At 25°C, the ion product of water is:

Kw = [H⁺][OH⁻] = 1.0 × 10⁻¹⁴

From this, we derive the key relationships:

  • pH = -log₁₀[H⁺]
  • pOH = -log₁₀[OH⁻]
  • pH + pOH = 14.00 (at 25°C)

These equations allow you to interconvert between [H⁺], [OH⁻], pH, and pOH.

1. Strong Acids and Bases: Complete Dissociation

Strong acids (e.g., HCl, HNO₃) and strong bases (e.g., NaOH, KOH) dissociate 100% in water.

Strong Acid Example:

For a 0.01 M HCl solution:

  • [H⁺] = 0.01 M (since HCl → H⁺ + Cl⁻)
  • pH = -log(0.01) = 2.00

Strong Base Example:

For a 0.001 M NaOH solution:

  • [OH⁻] = 0.001 M
  • pOH = -log(0.001) = 3.00
  • pH = 14.00 – 3.00 = 11.00

⚠️ Assumption: Valid for concentrations > 10⁻⁶ M. For very dilute solutions, water’s contribution to [H⁺] or [OH⁻] must be considered.

2. Weak Acids and Bases: Partial Dissociation

Weak acids (e.g., CH₃COOH) establish an equilibrium:

HA ⇌ H⁺ + A⁻

The acid dissociation constant (Ka) is:

Ka = [H⁺][A⁻] / [HA]

The ICE Table Method

For a weak acid with initial concentration C: | Species | Initial (M) | Change (M) | Equilibrium (M) | |--------|------------|-----------|----------------| | HA | C | –x | C – x | | H⁺ | 0 | +x | x | | A⁻ | 0 | +x | x |

Substitute into Ka:

Ka = x² / (C – x)

When to Use the Approximation

If C / Ka > 100, then x ≪ C, so:

Ka ≈ x² / Cx ≈ √(Ka·C)

Example: 0.10 M acetic acid (Ka = 1.8 × 10⁻⁵)

  • C / Ka = 0.10 / 1.8e-5 ≈ 5,555 > 100 → approximation valid
  • [H⁺] ≈ √(1.8e-5 × 0.10) = √(1.8e-6) ≈ 1.34 × 10⁻³ M
  • pH ≈ -log(1.34e-3) ≈ 2.87

When to Solve the Quadratic

If C / Ka below 100, solve:

x² + Ka·x – Ka·C = 0

Example: 1.0 × 10⁻⁴ M weak acid (Ka = 1.0 × 10⁻⁵)

  • C / Ka = 10 below 100 → use quadratic
  • x² + (1.0e-5)x – (1.0e-9) = 0
  • x = [H⁺] ≈ 9.5 × 10⁻⁵ M (vs. 1.0 × 10⁻⁴ M from approximation—5% error)

3. Buffer Solutions: The Henderson-Hasselbalch Equation

A buffer contains a weak acid (HA) and its conjugate base (A⁻). Its pH is given by:

pH = pKa + log₁₀([A⁻] / [HA])

Example: 0.30 M HA and 0.20 M A⁻ (pKa = 4.74)

  • pH = 4.74 + log(0.20 / 0.30) = 4.74 + log(0.667) ≈ 4.74 – 0.176 = 4.56

💡 Buffer capacity is highest when [A⁻] = [HA] → pH = pKa

Pro Tips & Common Mistakes

  • Always identify the system first: Strong vs. weak vs. buffer.
  • Check the C/Ka ratio before using the approximation.
  • Use concentrations, not moles, in Henderson-Hasselbalch (unless volume is identical).
  • Report pH to 2 decimal places for typical lab concentrations (e.g., 0.10 M).
  • Temperature matters: Kw = 1.0 × 10⁻¹⁴ only at 25°C.
  • For polyprotic acids, usually only the first dissociation matters (Ka₁ >> Ka₂).

Practical Applications

  • Biological systems: Blood pH buffered at ~7.4 by H₂CO₃/HCO₃⁻
  • Environmental science: Monitoring acid rain (pH below 5.6)
  • Industrial processes: Controlling pH in fermentation, dyeing, wastewater treatment
  • Laboratory work: Preparing buffer solutions for experiments

Related Calculators

Call to Action

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