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Abstract
The soils on which the "salvia" is have a different degree of evolution from Litosols to Cambisols including Rendzinas. They have a mollic ochric epipedon rich in organic matter with degree of transformation which very from medium to high. The content in macronutrients is variable for the potasium and relatively low for the phosphorous. The soils are alkatine-soils wholly saturated where de calcium is the dominant cation folows by the magnesium which Na + and K+ are minoritarius.
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