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t
translocation and accumulation of clay (B horizons commonly)
k or kk
accumulation of CaCO3 (B horizons commonly), kk=CaCO3>50%
n
accumulation of exchangeable sodium (typically columnar structure)
ss
presence of slickensides (high shrink swell eg. montmorillonite, smectite)
h
illuvial accumulation of SOM (only w/ B horizons), SOM is in the form of OM-sesquioxide complexes
s
illuvial accumulation of sesquioxides and SOM (only w/ B horizons)
q
accumulation of pedogenic silica (usually B horizons)
m
induration or cementation from pedogenisis (B horizons)
w
weak subsoil development (B horizons), only use this if there is nothing else for B
r
soft or weathered rock (C horizons only)
i
slightly decomposed SOM (O horizons only), can see plant parts
e
moderately decomposed SOM (O horizons)
a
highly decomposed SOM (O horizons), canât tell pieces/parts apart
p
plowed (usually A horizons), usually platy structure
b
burial
g
strong gleying (neutral chromas), reducing conditions
u
presence of human artifacts