Reference soil Nicaragua 10: Andosol

NI010

Andosols occur throughout the world where volcanic activity is common, especially in the circum-Pacific region and along the mid-Atlantic Ridge.

Characteristics

Soils with a vitric or andic horizon (slightly to moderately weathered horizons in pyroclastic deposits dominated by short-range-order minerals, notably allophane and imogolite) starting within 25 cm from the soil surface. In addition, they may have a histic, fulvic, melanic, mollic, umbric, ochric, duric, or cambic horizon. Other diagnostic horizons (unless buried deeper than 50 cm by volcanic deposits) are absent.

Distribution of Andosols (rough estimation supplied by soilgrids)

 

Reference soil NI010: Andosols

Shallow, (moderately) well drained, dark yellowish brown to (dark) brown silty clay loam to silt loam soil developed from volcanic ejecta, derived from unconsolidated pyroclastic materials. The soil contains fresh talpetate fragments, is weakly to moderately structured and moderately porous. The strongly cemented layers at 23 and 67 cm depth, called "talpetate" (Bm horizon) are in this part of Nicaragua probably of geogenetic and pedogenetic origin. The shallowness of the soil and the drought hazard due to the semi-dry climate determine the selected land use type. The profile forms part of a toposequence (El Crucero- Montelimar) of soils with "talpetate", studied by the Department of Soil Science of the Nicaraguan Agricultural University.

 

Classification

WRB 2006WRB 1998
Petroduric-Eutrosilic- Andosol (Siltic)Petroduri-Eutrisilic- Andosol
23-42 cmpetroduric horizon
-andic
0-23 cmochric horizon
23-42 cmpetroduric horizon
23-67 cmandic horizon
67-115 cmvitric horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic Andosol duripanVitric Andosol duripan
0-23 cmochric A horizon
- cmmollic A horizon
0-23 cmochric A horizon
- cmduripan horizon
- cmmollic A horizon
-exchange complex dominated by amorphous material

 

Local classification:Santo Domingo Series