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Manganese

Manganese in the soil

Manganese occurs mainly in oxide form but also occurs in silicates. Mn2+ ions are released into the soil solution during weathering of silicates. As well as the clay content of the soil, the pH and the redox potential of the soil are also important factors determining the potential of a soil to hold such readily exchangeable manganese.

 

With a decreasing pH value and decreasing redox potential comes an increase in the concentration of plant available Mn ions. A low redox potential occurs during low oxygen concentrations in the soil i.e. compaction, flooding, standing water). In contrast, a high pH value and adequate soil aeration decreases the concentration of Mn-ions.

 

Manganese deficiency mainly occurs in organic and carbonate rich soils, high pH soils and very light sandly soils which are often well aerated because of manganese fixation. Humus rich and podsol sandy soils are rather Mn poor as the manganese is less fixed.

 

Manganese in the plant

Manganese is taken up by the plant only as Mn2+-ions. This process can be inhibited by high concentrations of Mg2+-, Ca2+-, Cu2+- and iron ions. Manganese either stimulates, or is a component of many enzymes and, therefore, greatly affects the metabolism of the plant.

 

Functions of manganese in the plant:

 

Manganese deficiency

 

Manganese toxicity

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