Reference soil Philippines 06: Gleysol

PH006

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 PH006: Gleysols

A fine-textured, poorly drained, irrigated dark paddy soil (chroma /1 - /2), derived from volcanic tuff, with paddy dikes and sligh cracking during dry season. (FAO: anthraquic, dystric Gleysol SOIL TAX: vertic/lithic/entic Tropaquept)

 

Classification

WRB 2014 
Gleysol 
FAO-UNESCO-ISRIC 1974 
Dystric Gleysol