pH and pOH

Logarithmic concentration scales for aqueous ions

Lesson 1793 of 4,500 · Equilibrium: Chemical and Ionic

Learning objectives

Introduction

Hydronium and hydroxide concentrations vary over many powers of ten, so logarithmic scales make them easier to compare. A one-unit pH change represents a tenfold change in hydronium activity, not a small linear adjustment. Temperature and activity conventions matter when translating between pH, pOH and concentration.

Core explanation

Thermodynamically, pH = −log₁₀ a(H₃O⁺) and pOH = −log₁₀ a(OH⁻), where activities are dimensionless. In dilute introductory calculations, activities are approximated by numerical molar concentrations relative to a 1 M standard reference, giving pH ≈ −log₁₀[H₃O⁺] and pOH ≈ −log₁₀[OH⁻]. The logarithm should not be applied to a dimensional quantity without that understood normalization.

At 25 °C, Kw ≈ 1.0 × 10⁻¹⁴, so pKw ≈ 14.00 and pH + pOH ≈ 14.00 under the usual approximation. If pH = 3.00, then pOH = 11.00 and hydronium activity is about 10⁻³ relative to standard state. The relation pH + pOH = pKw is general at a specified temperature, but the number 14.00 is particular to approximately 25 °C.

The inverse relation is a(H₃O⁺) = 10⁻pH, and similarly for hydroxide. In a dilute solution, a numerical pH of 4 corresponds approximately to [H₃O⁺] = 10⁻⁴ M. pH 5 corresponds to about 10⁻⁵ M, ten times less hydronium. This tenfold interpretation is more important than imagining pH as a linear “acidity percentage.”

Neutral water has equal hydronium and hydroxide activities, giving pH = pOH = pKw/2. At 25 °C this is about 7.00. A pH below that neutral value is acidic; above it is basic under the same temperature and convention. Values outside 0–14 can occur in sufficiently concentrated solutions or under other conditions, although simple dilute classroom problems often stay within that range.

Significant figures in logarithms require care: decimal places in pH relate to significant figures in activity or concentration. A pH of 3.00 implies more precision than pH 3. A meter reading also has calibration and junction uncertainties beyond arithmetic precision.

Step-by-step reasoning

1. Choose a temperature-specific Kw or pKw. 2. Convert ion activity to pH or pOH using negative base-ten logarithm. 3. Use pH + pOH = pKw if the other scale is needed. 4. Reverse with 10⁻pH and interpret tenfold changes correctly.

Visual explanation

Draw a horizontal pH scale with marks at 3, 4 and 5. Label corresponding hydronium approximations 10⁻³, 10⁻⁴ and 10⁻⁵ M to show each step is tenfold.

Real-world analogy

A logarithmic earthquake scale compresses a huge numerical range into manageable steps. pH similarly compresses many powers of ten in hydronium activity into a short scale.

Real-world example

A calibrated pH meter can monitor a titration or buffer. Its reading estimates an activity-based acidity scale, not simply a direct count of free ions per litre.

Why?

Why does pH fall when hydronium rises? The logarithm increases with activity, but the negative sign reverses the direction of the reported numerical pH scale in water.

Common misconception

“pH 4 is twice as acidic as pH 8.” Under comparable dilute conditions, the hydronium activity ratio is about 10⁴, not two.

Worked example

At 25 °C, a dilute solution has [H₃O⁺] ≈ 2.0 × 10⁻⁴ M. Then pH ≈ −log₁₀(2.0 × 10⁻⁴) = 3.70. With pKw ≈ 14.00, pOH ≈ 10.30. The corresponding [OH⁻] ≈ 10⁻¹⁰·³⁰ ≈ 5.0 × 10⁻¹¹ M, matching Kw/[H₃O⁺] for the stated temperature.

Quick check

1. By what factor does hydronium activity differ between pH 3 and pH 4? Answer: pH 3 has ten times the hydronium activity of pH 4.

Exam focus

Use base-ten logs and a temperature-specific pKw. Distinguish rigorous activities from dilute concentration approximations and do not assume pH is restricted to 0–14 universally.

Advanced insight

The operational definition of pH involves electrochemical measurement and conventions for single-ion activity, which cannot be measured independently without assumptions. Introductory concentration formulas are useful approximations.

Summary

pH and pOH are negative logarithms of hydronium and hydroxide activities. Their sum equals pKw, approximately fourteen at 25 °C, and each unit represents a tenfold activity change.

Practice questions

1. What is pH for [H₃O⁺] ≈ 1.0 × 10⁻⁶ M in a dilute solution? Answer: Approximately 6.00. 2. At 25 °C, what is pOH if pH = 9.00? Answer: Approximately 5.00. 3. Is a solution at pH 2 ten or one hundred times higher in hydronium than pH 4? Answer: One hundred times, because the pH difference is two units.