Reference soil France 09: Planosol

FR009

Planosols occur in level landscapes throughout the world often associated with broad river valleys.

Characteristics

Soils having an eluvial horizon, the lower boundary of which is marked. within 100 cm from the soil surface, by an abrupt textural change associated with stagnic properties above that boundary. The feature of albeluvic tonguing, however, is lacking.

Distribution of Planosols (rough estimation supplied by soilgrids)

 

Reference soil FR009: Planosols

PARENT MATERIAL: Lozère sands. horizontally bedded. Miocene-Pliocene. VEGETATION AND LAND USE: coverage(%) Trees 50 herbs & grasses 90 ADDITIONAL NOTES ON PROFILE DESCRIPTION: O1 - organic matter: also wood fragments. O2 - mor. Ah1 - texture: also slightly stony. - highly organic. Ah2 - texture: also slightly stony. E - texture: also slightly stony. - with pebbles. Btg1 - texture: also stony (flints). - pockets of sandy clay Btg2 - texture: also slightly stony. - silex cobbles. Btg3 - texture: also slightly stony. C - horizontal banding. Textural change between EBg and Btg1 is probably partly geogenetic.

 

Classification

WRB 2006WRB 1998
Alic-Folic- Planosol (Albic Dystric)Albi-Alic- Planosol (Dystric)
0-11 cmfolic horizon
26-53 cmalbic horizon
53-126 cmanthric horizon
-reducing conditions
-stagnic colour pattern
-abrupt textural change
0-11 cmfolic horizon
11-26 cmochric horizon
26-53 cmalbic horizon
53-126 cmargic horizon
-stagnic
-abrupt textural change
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Albi-Dystric PlanosolDystric Planosol
11-26 cmochric A horizon
26-53 cmalbic E horizon
53-126 cmargic B horizon
-abrupt textural change
-stagnic
11-26 cmochric A horizon
26-53 cmalbic E horizon
53-126 cmargillic B horizon
-hydromorphic

 

Local classification:Sol podzolique à pseudogley