Reference soil Sri Lanka 03: Gleysol

LK003

Gleysols occur throughout the world where groundwater comes near to the surface, causing soils to become wet for a prolonged part of the year. They are particularly abundant in the low-lying river basins.

Characteristics

Soils having gleyic properties (properties associated with prolonged wetness) within 50 cm from the soil surface. They have no diagnostic horizons other than an anthraquic, histic, mollic, ochric, takyric, or umbric horizon at the surface, or an andic, calcic, cambic, gypsic, plinthic, salic, sulfuric, or vitric horizon within 100 cm from the soil surface.

Distribution of Gleysols (rough estimation supplied by soilgrids)

 

Reference soil LK003: Gleysols

Parent material: Weathered gneisses, Highland series (precambrian). Mineralogy: Quartz (fine to coarse), mica (fine spects), feldspar. Soil aggradation: Very slight by water. Vegetation and land use: Also some mixed tree crops ( mixed forest home gardens). Human influence: Hill slope is terraced for wet rice. Additional notes on profile description: Ap1g: Also medium and coarse fresh quartz gravel and stones. Bt1g: Also fine (slightly) weathered mica and quartz. Bt2g: Also few very fine and fine feldspar fragments; few medium and coarse (slightly) weathered mica, quartz and feldspar gravel and stones. BC: Also frequent medium and coarse, (slightly) weathered feldspar; frequent fine, (slightly) weathered mica, feldspar and quartz. C: Parent rock (gneiss).

 

Classification

WRB 2014 
Gleysol 
FAO-UNESCO-ISRIC 1974 
Dystric Gleysol  
  
- cmcambic B horizon
-hydromorphic