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Los Arroyuelos

"HAPLOXEREPT TIPICO"

Inceptisol developed on Cambrian slate and phyllite. Family thick textural skeletal loamy. Soil acid with pH < 6. High content of organic matter. Intermediate fertility potential, dependent on organic matter. Saturated complex change. Effective depth 60 cm.



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Alto camino de Melque

HAPLOXERALF LAMELLICO

Alfisol developed at the contact between the Miocene sands and underlying shales and phyllites of Cambrian. Family sandy texture. Acid soil with pH < 6. Under organic matter content. low fertility potential. Unsaturated exchange complex over 50%. effective depth 100 cm.



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Prado las viñas

HAPLOXERALF LAMELLICO

Alfisol developed on Miocene sands. Presence of an argillic horizon in bands, high power. Family sandy texture. Acid soil (5.5 < pH < 6.5) slightly. Organic matter content intermediate. low fertility potential, dependent on organic matter. Complex next change to saturation. effective 150 cm depth.



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Los Navales

HAPLOXERALF TIPICO

Alfisol developed on Miocene sands. Presence of an argillic horizon with a moderate clay content (20%). Family franca fine sandy texture on skeletal. Acid soil with pH < 6. Content of intermediate organic matter. low fertility potential, dependent on clay content. Complex next change to saturation. Effective depth 90 cm.



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Los Hoyos

HAPLOXERALF TIPICO

AAlfisol developed on Miocene sands. Presence of an argillic horizon with a high clay content (40%). Family clayey textural. Acid soil (5.5 < pH < 6.5) slightly. High content of organic matter. high potential fertility, dependent on clay content. Saturated complex change. Effective depth 80 cm.



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