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The pH scale

pH is a measure of the concentration of hydrogen ions in a solution. The more hydrogen ions that are present, the more acidic is the solution. The pH scale ranges from zero (very acidic) to 14 (very basic).

Illustration of the pH scale from 0 to 14 showing examples of acidic and basic substances, hydrogen ion concentration, and seawater with a pH of approximately 8.1.

The pH scale measures how acidic or basic a solution is based on the concentration of hydrogen ions (H⁺). Seawater is naturally slightly basic, with an average pH of about 8.1.

pH is a measure of the concentration of hydrogen ions in a solution. The more hydrogen ions that are present, the more acidic is the solution. The pH scale ranges from zero (very acidic) to 14 (very basic).

A pH of 7 is neutral, a pH less than 7 is acidic, and a pH greater than 7 is basic. For example, the pH of lemon juice is 2 while some antacids have a pH of about 10.

Ocean water is normally slightly basic, with a surface-water pH of about 8.2, but that has declined in recent years to about 8.1. A decrease of 0.1 pH units may not seem like much, but because the pH scale is logarithmic, each unit on the pH scale represents a tenfold change in acidity.

For example, water with a pH of 6 is ten times more acidic than neutral water with a pH of 7, and 100 times more acidic than water with a pH of 8. So a decrease of 0.1 pH units represents a 26 percent increase in the relative acidity of ocean water.

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