Copper

Copper in the soil

The copper content of unpolluted soils typically ranges between 2-40 mg Cu kg-1 soil. Copper has a tendency to bind to the soil organic matter of the soil. It is adsorbed by manganese and iron oxides or it can be bound to the lattice silicates. In addition, it can precipitate as the hydroxide, carbonate or phosphate form.

 

The concentration of copper in the soil solution depends on the pH value and the available chelating agents. The proportion of exchangeable copper generally increases with decreasing pH.

 

Copper deficiency occurs on recently cultivated moorland soils and due to Cu fixation also in podsol soils rich in organic matter.

 

Copper in the plant

Plants take up Cu2+-ions freely from the soil solution or as soluble copper complexes. As a component of several enzymes, copper has a positive effect on the plant metabolism.

 

Function of copper in the plant

 

Copper deficiency

 

Copper excess

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