摘要：The edaphic structure of a territory is a fundamental natural resource, because soil is the support and living environment of plants, especially crops; the agricultural practice could not be conceived in the absence of the edaphic couverture. The various pedogenesis conditions led to the relative diversification of soil, pointing out a great typological variety, among which the following stand out: cambic chernozems and luvisoils, brown luvisoils, marsh and gleic soils, regosols and erodisoils, alluviosoils, etc.
