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Soil pH is defined as the negative logarithm of the hydrogen ion concentration. The pH scale goes from 0 to 14 with pH 7 as the neutral point. As the amount of hydrogen ions in thesoil increases the soil pH decreases thus becoming more acidic.
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Note On pH value of Soil
- Most soils have pH values between 3.5 and 10. In higher rainfall areas the natural pH of soils typically ranges from 5 to 7, while in drier areas the range is 6.5 to 9.
- Soils can be classified according to their pH value: 6.5 to 7.5—neutral.
- As the amount of hydrogen ions in the soil increases the soil pH decreases thus becoming more acidic.
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