This means a pH value in which the availability of macronutrients for plants is at its highest, and an acid- base balance occurs in the soil. When the soil has a pH in the range of 6.0–7.0, then the highest amounts of nitrogen, potassium, phosphorus and calcium available are available to the plant from soil resources and mineral fertilisers.
However, this situation is unfavourable for the availability of micronutrients in the soil. Paradoxically, slightly acidic and acidic soils offer the highest availability of micronutrients to plants, i.e. copper, zinc, iron, boron or manganese. In turn, alkaline soils offer the highest supply of molybdenum.
Nutrient | Share of micronutrient forms available for plants in soil in relation to the entire component pool |
---|---|
Boron | 10% |
Copper | 25% |
Manganese | 10% |
Molybdenum | 19% |