Secondary
Carbonates in Three Fine and
Fine-loamy
Alfisols in Michigan
Randall J. Schaetzl, William E. Frederick, and Lawrence Tornes
Secondary pedogenic carbonates are
usually associated with ustic or drier soil moisture regimes; when found
elsewhere, their interpretation can be troublesome. We studied three Alfisol pedons in Michigan that contained
secondary carbonates on ped faces. The
purpose of the research was to (i) characterize these accumulations, (ii)
examine possible genetic explanations for the accumulations, (iii) determine if
these soils have calcic horizons, given the recent redefinition of this
diagnostic horizon, and (iv) evaluate how current k horizon nomenclature
might apply to these soils. Three
different drainage classes and two soil temperature regimes were represented in
the sampled pedons: a fine, mixed Glossic Eutroboralf; a fine, illitic, mesic
Aquic Hapludalf; and a fine-loamy, mixed, mesic Aeric Endoaqualf. All three pedons had thin (<50 cm)
leached zones near the surface, and carbonate coatings (calcans) on ped faces
within the lower B and/or upper C horizons.
Two of the three pedons had horizons that met calcic horizon criteria. Horizons of preferential carbonate
accumulation sometimes occurred near subtle textural breaks in the lower
solum. Some B horizons in one pedon
contained carbonate accumulations in amounts that exceeded that of the presumed
parent material. The calcans have
probably resulted both from vertical translocation of carbonates, followed by
precipitation at depth, as well as internal redistribution of carbonates from
ped interiors to ped faces. Use of the
k subscript is warranted for some horizons in these soils. We recommend that its usage should be
similar to t or s, i.e., horizons with evidence of secondary carbonates merit
the k subscript.