Reference soil Indonesia 06: Gleysol
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.
Reference soil ID006: Gleysols
LOCATION: between Blangkejeren basin in Central Rift Valley and Blangpidie on the Westcoast, Gunung Leuser National Park. GEOLOGY: Eocene-Miocene regressive sediments, mixture of kaolinite, halloysite and gibbsite. CLIMATE: the mean annual temperature at site is be estimated to be 8 °C. VEGETATION: "blang vegetation", subalpine zone. ADDITIONAL NOTES ON PROFILE DESCRIPTION: Ah - when the soil dries out, horizontal (polygon-forms) and vertical cracks occur. Bg - mottling decreases with depth. Bg - after drying out of the soil in the laboratory, horizontal cracks occur along the sedimentation structures. Cg - after drying out of the soil in the laboratory, horizontal cracks occur along the sedimentation structures. C - clayey and sandy layers alternate. REFERENCES: - Van Beek, C.C.G., 1982. Een geomorfologische bodemkundige studie van het Gunung Leuser nationale park, Noord Sumatra, Indonesie (in Dutch). Utrechtse geografische studies 26. Geografisch instituut, Rijksuniversiteit Utrecht, The Netherlands.