Geoscience Reference
In-Depth Information
Table 11.4 (continued)
Area
Soil taxa
Role of soil-forming factor
Citations
ND
Hapludolls
Stronger argillic with stratified par-
ent materials
Hopkins and
Franzen
(
2003
)
Edwards Pla-
teau, TX
Calciustolls,
Haplustalfs
Argillic more strongly developed in
soils with abundant coarse
fragments
Rabenhorst and
Wilding
(
1986a
,
b
)
KY
Hapludults,
Paleudults,
Paleudalfs
Loess rejuvenation increases
argilluviation and mineral
weathering
Mubiru and
Karathanasis
(
1994
)
CA, NV, AZ
Haplargids,
Paleargids
Argillic forms more readily in allu-
vium than dune sands
Nettleton
et al. (
1975
)
VA
Hapludalfs,
Paleudalfs
Argilluviation enhanced by litho-
logic discontinuities
Ogg and Baker
(
1999
)
GA
Kandiudults,
Paleudults
The base of the argillic is controlled
by lithologic discontinuities
Shaw et al. (
2004
)
OH
Hapludalfs
Argillic forms more readily with low
CaCO
3
in parent materials
Smeck
et al. (
1968
)
FL coastal
plain
Hapludults,
Paleudults
Clay translocation enhanced by lith-
ologic discontinuities
Cabrera
et al. (
1989
)
IN
[Not provided]
Clay content of argillic strongly
related to clay content of parent
material
Franzmeier
et al. (
1985
)
MI, OH
Epiaqualfs,
Hapludalfs
Clay content of argillic strongly
related to clay content of parent
material
Smith and Wild-
ing (
1972
)
Relief
ND
Hapludolls
Argillic horizons more strongly
developed under well-drained
conditions
Hopkins and
Franzen
(
2003
)
TX coast
prairie
Calciaquolls,
Argiaquolls,
Vermaqualfs,
Glossaqualfs
Argillans more strongly developed in
micro-lows
Sobecki and
Wilding
(
1983
)
Southern IL
Hapludalfs,
Epiaqualfs
Argillic best developed on sideslope
and headslope
Wilson
et al. (
2010
)
MO
[Not provided]
Argillic more strongly developed on
backslopes than ridges and
shoulders
Young and Ham-
mer (
2000
)
IL
Hapludalfs
Argillic more developed on stable
ridge crests and depressions than
shoulders
Olson
et al. (
2005
)
MI
Hapludalfs
Argillic more developed and deeper
in well-drained areas
Cremeens and
Mokma
(
1986
)
Time
IL
[Not provided]
Clay-rich lamellae form in
3,500 year
Berg (
1984
)
MT
Paleudolls,
Paleustolls
Argillic forms in early Wisconsin-
late Illinoian soils and not late
Wisconsin soils
Karlstrom (
2000
)
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