Reference soil Peru 23: Phaeozem
Phaeozems occur all over the world, but especially on the more moist side of the steppe regions, bordering Chernozems.
Characteristics
Soils having a mollic horizon (deep, brownish or blackish surface horizon with a significant accumulation of organic matter and high base saturation); a base saturation of 50 percent or more between 25 and 100 cm from the soil surface; a calcium carbonate-free soil matrix at least to a depth of 100 cm from the soil surface, or to a contrasting layer between 25 and 100 cm; no diagnostic horizons other than an albic, argic, cambic or vertic horizon, or a petrocalcic horizon in the substratum.
Reference soil PE023: Phaeozems
Short field description Soil profile located on the left bank of the Urubamba river, in a fan (derived from colluvium-alluvium material). It is a deep, well drained, dark reddish brown clay loam.. This land has been cultivated for about 100 years, the last nine years with Alfalfa in rotation with crops such as potatoes, corn and lima beans. The technology level is high (use of fertilizers, mechanization and pesticides).