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pH

pH is a measure of the acidity of a solution.

Definition

Definition

  • The mathematical definition of pH is:
    • pH = -log10[H+]
Rearranging the pH equation

Rearranging the pH equation

  • You can use the pH of a solution to calculate it's hydrogen ion concentration.
    • According to the rules of logarithms, you can rearrange the above equation to:
    • [H+] = 10-pH
Calculations of pH

Calculations of pH

  • Consider a one molar solution of HCl. The [H+] = 1moldm-3
    • pH = -log10(1) = 0
Uses of pH

Uses of pH

  • We use pH because the concentration of hydrogen ions varies massively over solutions.
    • It can vary between 2 or 3 moldm-3 to 1 × 10-20 or so.
    • This is a very big scale, so we use a logarithmic one to shorten it.
    • You can have negative pH, but it’s rare to see one below -1 or above 15.
    • This is a much smaller range, and much nicer to work with.
Jump to other topics
1

Physical Chemistry

1.1

Atoms, Molecules & Stoichiometry

1.2

Atomic Structure

1.3

Chemical Bonding

1.4

States of Matter

1.5

Chemical Energetics

1.6

Electrochemistry

1.7

Equilibria

1.8

Partition Coefficient

1.9

Reaction Kinetics

2

Inorganic Chemistry

3

Organic Chemistry & Analysis

3.1

Introduction to Organic Chemistry

3.2

Hydrocarbons

3.3

Halogen Derivatives

3.4

Hydroxy Compounds

3.5

Carbonyl Compounds

3.6

Carboxylic Acids & Derivatives

3.7

Nitrogen Compounds

3.8

Polymerisation

3.9

Analytical Techniques

3.10

Organic Synthesis

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