Reference soil Mozambique 09: Solonetz

MZ009

Solonetzes occur where a sodium source supplies the clay-rich subsoil with exchangeable Na, causing peptization of clay and organic substances and deterioration of the topsoil.

Characteristics

Soils having a natric horizon (a subsurface horizon with distinct higher clay content than the overlying horizon and more than 15% exchangeable sodium) within 100 cm from the soil surface.

Distribution of Solonetz (rough estimation supplied by soilgrids)

 

Reference soil MZ009: Solonetz

PHYSIOGRAPHY: Slope length: - 200 m. Termite mounds: - inactive, 4/ha, 20-50 cm high, 5-15 m across, with concentration of vegetation. Surface characteristics: - 1 mm soft crust, below 3-4 cm rather compact. - surface is covered by quartz grains. Surface drainage: - hardly existent, only fossile drainage system. VEGETATION AND LAND USE: coverage(%) regional local Shrubs 5 2 Herbs 5 5 Grasses 45-65 60 Bare ground 30-50 35 SOIL FAUNA: - insect nests. ADDITIONAL NOTES ON PROFILE DESCRIPTION: Bt - consistency dry: also extremely hard. - cutans: also moderately thick. - roots: along ped faces. - tonguing along cracks of not very bleached quartz grains. BC - pockets of not very bleached quartz grains.

 

Classification

WRB 2006WRB 1998
Haplic- Solonetz (Abruptic Magnesic)Magnesic- Solonetz
16-50 cmargic horizon
50-75 cmnatric horizon
-abrupt textural change
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Abrupti-Haplic SolonetzOrthic Solonetz
0-16 cmochric A horizon
16-50 cmargic B horizon
50-75 cmnatric B horizon
-abrupt textural change
0-16 cmochric A horizon
16-50 cmargillic B horizon
50-75 cmnatric B horizon
-abrupt textural change