Reference soil Greece 05: Phaeozem

GR005

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.

Distribution of Phaeozems (rough estimation supplied by soilgrids)

 

Reference soil GR005: Phaeozem

LOCATION: Eastern borders of the village of Myloros. VEGETATION AND LAND USE: Fallow after being used for cereals. At present short grasses and a very sparse cover of Pyrus amygdaliformis and Paliuris australis. Originally deciduous forest with mainly oak. The soil has been ploughed in the past. CLIMATE: Mediterranean with pronounced dry summer. ADDITIONAL NOTES ON PROFILE DESCRIPTION: A1p, A2p & Bw - rock fragments: indurated marl. BC - pedotubules: root channels filled with material from the Ap horizon. C - white (when dry) marl, massive. - concretions: calcium carbonate.

 

Classification

WRB 2014  
Phaeozem