Reference soil Indonesia 42: Fluvisol

ID042
Distribution of Fluvisols (rough estimation supplied by soilgrids)

Near artificial drain.

Micro relief: Crab mounds. Down to 56 cm there is a lot of activity of marine organisms (crabs).

Flooding: Tidal floods occuring between 13:00 and 19:00 hour. Tidal fluctuation is 2 to 5 meters.

Additional noteson profile description: 1 - mottles are irregular. 2 - mottles : many rounded and ex along roots. 3,4&5 - unripe clay. In all the horizons organic matter is encountered, like small and fine root remnants.

WRB 2006:

Salic Tidalic Fluvisol(Thionic Sodic Siltic)  
0-120 cm n salic horizo
81-120 cm thionic horizon
  fluvic material

FAO-UNESCO-ISRIC 1988:

FAO-UNESCO 1974:

Sali- Thionic Fluvisol
Thionic Fluvisol saline phase
81-120 cm sulfuric horizon
  fluvic properties
  sulfidic materials
81-120 cm sulfuric horizon
  sulfidic materials

Other classification

USDA-NRCS (1999)

Sulfaquept

USDA-SCS (1975)

Sulfaquept

Classification (other)

Gleysol Thionik
  Deep, very poorly drained, gray silty clay of marine origin under a mangrove forest. Flooded daily by tide.
Location: 

Sumatra, Riau, Bengkalis, Bukit Kapur, Geniut