Nitisol

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As Nitisol (formerly Nitosol) after World Reference Base for Soil Resources referred to a reference floor pan (WRB), which mainly in the tropics occurs. The soil profile has (according to the FAO Guidelines for Soil Description) either a horizon sequence A-Bo-C or A- (E-) Bto-C. The ground is deeply weathered . The source rocks are neutral to basic rocks rich in silicate .

Nitisols are found worldwide on an area of ​​200 million hectares, mainly under tropical rainforest and wet savannah , with about half of them occurring in tropical East Africa .

properties

The horizon borders are only weakly defined due to strong bioturbation , the color change is fluid. Overall, weathering has not progressed as much as with the ferralsoles , so that mostly weatherable (primary) minerals are still present.

The diagnostic horizon is the nitic horizon . This is a clay-rich (at least 30%), at least 30 cm thick subsoil horizon with partly shiny aggregate surfaces in a characteristic polyhedral (nutty) structure. The humus contents are relatively high. The soil profile is characterized by strong aggregation and high porosity (50–60%), and thus by good water conductivity (approx. 50 mm h −1 ). Due to the type of soil and the depth, a large amount of water can be stored.

These properties result in relatively high fertility as long as the problems associated with erosion and P fixation are controlled.

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