Soil Science

pH (soil)

Definition

A measure of the acidity or alkalinity of soil on a scale of 0–14, with 7 being neutral. Most plants grow best between pH 6.0 and 7.0. pH affects nutrient availability: iron becomes unavailable above pH 7.5, while manganese can become toxic below pH 5.5.

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Explore Plant Species

See how the concept of "pH (soil)" applies across different plant species.