Reference soil Ecuador 10: Phaeozem

EC010

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 EC010: Phaeozems

EC10 is comparable to profile Ecuador No.12 in: part III-tourguide for Ecuador of the sixth international soil classification workshop (1984). The soil has been redescribed and resampled by G.del Posso in May 1988, additionally two monoliths have been taken. The volcanic ash is probably of an acid type. To a depth of 130 cm are present a few (1%) artifacts, fragments of brick, stone and tools.

 

Classification

WRB 2006WRB 1998
Endovitric- Phaeozem (Pachic)Pachi-Vitric- Phaeozem
0-83 cmmollic horizon
102-150 cmargic horizon
-vitric
0-83 cmmollic horizon
102-150 cmargic horizon
52-102 cmvitric horizon
-strongly humic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Andi-Luvic PhaeozemLuvic Phaeozem
0-83 cmmollic A horizon
102-150 cmargic B horizon
-andic
-strongly humic
0-83 cmmollic A horizon
102-150 cmargillic B horizon