Traditional agricultural practices and the effects of global climate change are some of the factors that can lead to serious degradation processes that limit or completely inhibit the functionality of agricultural soils. The consequences are evident only when they are irreversible or they are in such an advanced state that restoration has become extremely expensive. According to the FAO, 33% of the soils are now degraded and affected by problems of salinization, compaction, acidification and nutrient depletion. The direct effect on the agricultural system is a progressive loss of agricultural production. A more rational and eco-sustainable management of the soil, and in particular of the rhizosphere, is the basis for restoring optimal production levels.
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