Reference soil Germany 04: Luvisol
DE004
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 DE004: Luvisols
An imperfectly drained soil, situated on lower part of gentle slope in dissected terrace landscape, 20 m away from valley bottom. The material consists of weathered colluvial loess (ca. 75 cm) on fluviatile silt deposits on fluviatile gravel. In B horizons fine black Mn mottles appear; below 21 cm there are Fe mottles increasing with depth. In the 2Cg1 horizon an alternation of fine and coarser textured sedimentary layers is clearly visible. VEGETATION: Quercus pendunculata, Carpinus betulus; Euonymus europaeus, Lamium galeobdolon, Milium effusum, Mercurialis perennis, Deschampsia, Circea lutetiana, Athyrium felix-femina. (additional climatic data: insolation (hrs))
Classification
| WRB 2006 | WRB 1998 | ||
|---|---|---|---|
| Gleyic-Albic Luvisol (Ferric Ruptic Siltic) | Albi-Gleyic Luvisol (Ferric) | ||
| 21-38 cm | albic horizon | 0-21 cm | ochric horizon |
| 38-80 cm | argic horizon | 21-38 cm | albic horizon |
| 60-102 cm | ferric horizon | 38-80 cm | argic horizon |
| - | gleyic colour pattern | 60-102 cm | ferric horizon |
| - | reducing conditions | - | gleyic |
| FAO-UNESCO-ISRIC 1988 | FAO-UNESCO-ISRIC 1974 | ||
| Albi-Gleyic Luvisol | Gleyic Luvisol phreatic | ||
| 0-21 cm | ochric A horizon | 0-21 cm | ochric A horizon |
| 21-38 cm | albic E horizon | 21-38 cm | albic E horizon |
| 38-80 cm | argic B horizon | 38-80 cm | argillic B horizon |
| - | gleyic | 1 | hydromorphic |
Local classification
| Classification information | Gley-Podsol |
Location:
Nordrhein-Westphalen, 5km SE of Jülich in the Hambacher Wald