Reference soil China 35: Phaeozem

CN035

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 CN035: Phaeozems

PROFILE DESCRIPTION : Deep, well drained, very dark grayish brown clay loam overlying a strongly mottled, slightly altered subsoil. The soil is derived from alluvial deposits and has a fluctuating groundwater level which reached to about 120 cm below the surface. The general structure is crumb, however, angular blocky structures dominate on the surface horizons. A plough pan has formed below the arable surface layer. The soil has a medium content in organic matter and a neutral reaction. CLIMATE: climatic data regarding sunshine hours per month: J 187.2 F 192.3 M 233.4 A 236.3 M 244.9 J 251.2 J 208.5 A 227.9 S 236.1 O 208.5 N 180.2 D 174.3 Year 2570.0

 

Classification

WRB 2006WRB 1998
Haplic- Phaeozem (Pachic Siltic)Silti-Pachic- Phaeozem
0-120 cmmollic horizon
0-120 cmmollic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Silti-Haplic Phaeozem phreaticHaplic Phaeozem phreatic
0-120 cmmollic A horizon
- cmmollic A horizon
0-120 cmmollic A horizon

 

Local classification:Haplic thermo-black soil; Hapli-Udic Isohumosol
Common name:Black earth