Reference soil Nicaragua 04: Cambisol

NI004

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.

Distribution of Cambisols (rough estimation supplied by soilgrids)

 

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 2006WRB 1998
Haplic- Cambisol (Hypereutric Clayic Chromic)Hypereutri-Chromic- Cambisol
15-75 cmcambic horizon
0-15 cmochric horizon
15-75 cmcambic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Chromic CambisolChromic Cambisol
0-15 cmochric A horizon
15-75 cmcambic B horizon
0-15 cmochric A horizon
15-75 cmcambic B horizon
- cmargillic B horizon

 

Local classification:San Rafael Rivas Series