Reference soil Nicaragua 04: Cambisol
Cambisols occur mainly in the temperate and boreal regions of the world, where the soil’s parent material is still young or where low temperatures slow down the processes of soil formation.
Characteristics
Soils having either a cambic horizon (a horizon showing evidence of alteration with respect to the underlying material), or a mollic horizon overlying a subsoil, which has a base saturation of less than 50 percent in some part within 100 cm from the soil surface, or one of the following diagnostic horizons within the specified depth: an andic, vertic, or vitric horizon starting between 25 and 100 cm; a (petro-)plinthic or salic horizon starting between 50 and 100 cm, in absence of loamy sand or coarser textures above these horizons.
Reference soil NI004: Cambisols
The thickness of the solum (A+B) varies within the pit from about 25 cm to 50 cm. The shallow soil classifies as chromic Cambisol (eutropept), the deeper soils as ferric Cambisol (rhodustalf). The landscape is strongly sloping with maximum slopes of 30 to 40%. At a distance, break of slopes and in gullies rock outcrops. Soil has still some moisture left, but general feeling of dry soil (irrespect of the rain of the last days). C horizons have a multicoloured (weathering colours) appearance. Most brown/reddish colours in the upper C horizons, becoming yellowish in the deeper C horizons. BC show clearly the rock structure, although a substancial part of the rock has been transformed in clay.
Classification
WRB 2006 | WRB 1998 | ||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Haplic- Cambisol (Hypereutric Clayic Chromic) | Hypereutri-Chromic- Cambisol | ||||||||||||
|
| ||||||||||||
FAO-UNESCO-ISRIC 1988 | FAO-UNESCO-ISRIC 1974 | ||||||||||||
Orthi-Chromic Cambisol | Chromic Cambisol | ||||||||||||
|
|
Local classification: | San Rafael Rivas Series |