2.5.2

pH (A2 Only)

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pH

pH is a measure of the acidity of a solution.

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Definition

  • The mathematical definition of pH is:
    • pH = -log10[H+]
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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
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Calculations of pH

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

1Physical Chemistry

2Physical Chemistry 2 (A2 Only)

3Inorganic Chemistry

4Inorganic Chemistry 2 (A2 Only)

5Organic Chemistry 1

6Organic Chemistry 2 (A2 Only)

6.1Optical Isomerism (A2 Only)

6.2Aldehydes & Ketones (A2 Only)

6.3Carboxylic Acids & Esters (A2 Only)

6.4Aromatic Chemistry (A2 Only)

6.5Amines (A2 Only)

6.6Polymers (A2 Only)

6.7Biological Organic (A2 Only)

6.8Organic Synthesis (A2 Only)

6.9NMR Spectroscopy (A2 Only)

6.10Chromatography (A2 Only)

6.11A-A* (AO3/4) - Organic 2

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