Reference soil Thailand 06: Luvisol

TH006

Luvisols occur mainly in temperate regions, particularly in areas with a Mediterranean-type of climate.

Characteristics

Soils having an argic horizon (a subsurface horizon with a distinct higher clay content than the overlying horizon) with a cation exchange capacity equal to or more than 24 cmolc per kg clay throughout.

Distribution of Luvisols (rough estimation supplied by soilgrids)

 

Reference soil TH006: Luvisols

LOCATION: 500 m W of highway U Thong - Kampaeng Saen, near Ban Sa Yai Som. MICRO RELIEF: Slightly undulating. CRACKING: not observed. CLIMATE: Tropical savanna, 85% of the total annual rainfall of 1275 mm falls in the period May - October. Data source: Agroclimatological data Asia 2, FAO. Rome 1987. ADDITIONAL NOTES ON PROFILE DESCRIPTION: A3 - Some inclusions of Ap. The neutral soil reaction in the A horizons is probably due to the burning of the crop remnants. REFERENCES: - Kawaguchi, K.; Kyuma, K.: Lowland rice soils in Thailand; report on research in Southeast Asia, Natural Science Series. Tokyo 1969. - Moormann, F.R.; Rojanasoonthon, S.: Soils of Thailand; report SSR-72, Soil Survey Division, Kingdom of Thailand. Bangkok 1968. - Rice, O.W.: Notes on soils temperature regimes in Thailand; report SSR-79, Soil Survey Division, Kingdom of Thailand. Bangkok 1969. - Rojanasoonthon, S.; Moormann, F.R.: No. 48 final report on the Great Soil Group Survey of seven selected areas in Thailand; Soil Survey Division, Kingdom of Thailand. Bangkok June 1966. - Van der Kevie, W.; Yenmanas, Banchong: Detailed reconnaissance soil survey of Southern Central Plain Area; Soil Survey Division, Ministry of National Development, report SSR-89. Bangkok 1972.

 

Classification

WRB 2014 
Luvisol 
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Haplic LuvisolOrthic Luvisol
- cmargic B horizon
- cmochric A horizon
- cmargillic B horizon
- cmochric A horizon

 

Local classification:see classification remarks