Reference soil Australia 29: Plinthosol

AU029

Plinthosols occur mainly in the moist tropical regions in low-lying positions where iron from the soil and adjacent uplands is accumulating.

Characteristics

Soils having either a petroplinthic horizon within 50 cm from the soil surface, or a plinthic horizon which either starts within 50 cm from the soil surface, or within 100 cm from the soil surface if it underlies an albic horizon or a horizon with stagnic properties.

Distribution of Plinthosols (rough estimation supplied by soilgrids)

Reference soil AU029: Plinthosols

Classification

WRB 2006WRB 1998
Acric-Stagnic- Plinthosol (Albic Abruptic Endodystric)Albi-Acric- Plinthosol (Stagnic Abruptic)
40-130 cmargic horizon
5-30 cmalbic horizon
60-130 cmplinthic horizon
-reducing conditions
-stagnic colour pattern
-abrupt textural change
0-5 cmochric horizon
40-130 cmargic horizon
5-30 cmalbic horizon
60-130 cmplinthic horizon
-stagnic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Stagni-Albic PlinthosolEutric Planosol petric
0-5 cmochric A horizon
40-130 cmargic B horizon
5-30 cmalbic E horizon
-plinthite
-stagnic
0-5 cmochric A horizon
30-130 cmargillic B horizon
5-20 cmalbic E horizon
-abrupt textural change
-plinthite

 

Local classification:HAS: Lateritic Podzolic Soil; FK: Dy3.71