Difference between revisions of "Planosol"
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A '''planosol''' (PL) can be defined through : | A '''planosol''' (PL) can be defined through : | ||
| − | * 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 | + | * an eluvial horizon, the lower boundary of which is marked, within 100 cm from the soil surface, by an [[Has for diagnostic property::Abrupt textural change (WRB)|abrupt textural change]] associated with [[Has for diagnostic property::Stagnic colour pattern (WRB)|stagnic properties]] above that boundary |
and : | and : | ||
| − | * no albeluvic tonguing | + | * no [[Albeluvic tonguing (WRB)|albeluvic tonguing]] |
==Possible qualifiers== | ==Possible qualifiers== | ||
Latest revision as of 19:24, 28 June 2017
A planosol (PL) can be defined through :
- 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
and :
Possible qualifiers
For each RSG, there are some possible prefix and suffix qualifiers :
|
Prefix qualifiers |
| |
Source
- The FAO website
