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Due to the ability of legumes to fix nitrogen in the ground and the wide range of soils where they can grow up, Leucaena genus has been proposed for recovering deserted soils.
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Compared to desert soils, the chestnut-brown soils are easier to work and are more productive under irrigation.
These give way to soils with accumulations of lime and ultimately to desert soils with soluble salt efflorescence (powdery crust) near the surface.
The desert soils contain a high percentage of soluble salts.
Desert soils are mainly immature, weakly developed in terms of their soil profiles, and mostly alkaline.
In the arid north, gray-brown desert soils occupy the largest expanses.
The arid regions of northeastern Somalia have mainly thin and infertile desert soils.
Soil zonation is simple in structure, with steppe soils and desert soils, both including those of the alpine group, predominating.
Desert soils are commonly poorly developed with shallow profiles and low organic content.
This suggests that desert soils may have preserved past evidence of small variations in continental precipitation.
This was no mean feat when you consider that desert soils are more like concrete than dirt.
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