Reference soil Netherlands 6: Fluvisol

Code: 
NL006
Latitude: 
52.02
Longitude: 
5.25
Description: 
A deep, clayey soil with low chroma (/1), derived from holocene alluvial deposits, with a weak prismatic structure breaking into moderate subangular blocks. There are shallow drainage channels on site, the groundwater table is below 120 cm. In B1 horizon, there are some brick pieces. At 105 cm, there is the top part of a buried soil. (additional climatic data: xa - insolation (hrs))
Collection date: 
September, 1971
Soil surveyor: 
Buursink J & D Creutzberg
Location: 
Prov. of Utrecht, W of Werkhoven
Climate classification: 
Cfb
Classification: 

WRB 1998:

Eutri- Gleyic Fluvisol

FAO-UNESCO-ISRIC 1988:

FAO-UNESCO 1974:

Eutric Fluvisol
Eutric Fluvisol
0-0 cm ochric A horizon  

 

Physiography: 
The altitude of the soil profile relative to mean sea level, specified in meters 0 m asl
Regional landform alluvial plain
Topography of the surrounding country flat or almost flat
Physiographic Unit in the immediate surrounding of the site backswamp
The slope refers to the inclination of the land immediately surrounding the site. The measured or estimated slope angle is specified to the nearest per cent 0 %
The physiographic position of the site where the profile is located flat
Form of the slope surrounding the site  
Slope Aspect of the site
Parent material: 
The main parent rock/ material over which the soil has been formed (1st entry)  
Mode of Accumulation or deposition of parent material (1st entry) fluvial
Texture of parent material (1st entry)  
Weathering status of solid rock (1st entry) partially or moderately
Resistance against weathering (solid rock) (1st entry) moderate
Depth1 of lithological boundary cm
The main parent rock/ material over which the soil has been formed (2nd entry)  
Texture of parent material (2nd entry) clayey
Resistance against weathering (solid rock) (2nd entry)  
Soil Depth; depth to which roots can easily penetrate throughout the year cm
Remarks on Parent Materials backswamp deposits
Hydrology and drainage: 
Depth of groundwater table 120 cm
Groundwater Top 30 cm
Groundwater Bottom 120 cm
Kind of groundwater table groundwater table observed
Top Stagnating Layer cm
Bottom Stagnating Layer cm
Runoff very slow
Estimated permeablity (class) of least permeable part of the profile slow
Drainage Class imperfect
To Drainage Class  
Moisture conditions of the profile: dry from -to 0-50 cm
Moisture conditions of the profile: moist from -to 50 cm
Wet From - To cm
Land use: 
Current land use at the site cultivated pasture
Major crops  
Main type of irrigation  
Rotation scheme  
Vegetation Type;The natural vegetation at the site  
Status of vegetation  
Remarks on Land Use / Vegetation Land used as orchard some years ago
Erosion: 
Soil erosion type (1st entry)  
Occurrence of soil aggradation  
Slope Stability
Surface characteristics: 
Microrelief type: small-scale differences in relief in the direct vicinity of the site  
Microrelief Height  
Rockiness none
Stoniness none
Average size of stones  
Shape of stones (on average)  
Slaking of aggregates by tillage, rainfall or frost  
Evidence of salt non-saline
Evidence of alkali non-alkaline