Geoscience Reference
In-Depth Information
Table 11.2 (continued)
Order
Suborders Great groups Subgroups a
No. series
Oxisols
Udox
Eutrudox
Kandiudalfic
0
Udox
Kandiudox
All
3
Ustox
Eutrustox
Kandiustalfic
3
Ustox
Kandiustox All
1
Spodosols Aquods
Alaquods
Alfic Arenic (2), Arenic Ultic (2), Alfic (6),
Ultic (12)
22
Aquods
Endoaquods Argic
17
Aquods
Epiaquods
Alfic (17), Ultic (2)
19
Orthods
Alorthods
Alfic, Ultic, Arenic Ultic
0
Orthods
Fragiorthods Alfic (9), Alfic Oxyaquic (10), Ultic (1)
20
Orthods
Haplorthods Aqualfic (3), Alfic Oxyaquic (30), Alfic (36),
Lamellic (9), Lamellic Oxyaquic (2),
Ultic (1), Oxyaquic Ultic (2)
83
Ultisols
All
All
All
1,330
Vertisols
Aquerts
Natraquerts Typic
9
10,540
a Number of soil series within a subgroup given in parentheses
Alfic Humic subgroups) within nine great groups. Clay illuviation also is recog-
nized in Inceptisols at the subgroup level (Lamellic Eutrudepts, Lamellic
Haplustepts). However, the lamellae are considered part of the cambic horizon
and not the argillic horizon.
11.4 Distribution of Soils with Clay Enrichment
All of the Alfisols and Ultisols contain evidence of clay enrichment; these soils
contain 3,984 and 1,330 soil series and cover 1.2 million and 0.82 million km 2 of the
USA, respectively (Table 11.3 ). The distribution of these soils in the USA is shown in
Fig. 11.2 . Nearly half of the soil series in the Mollisol and Aridisol orders contain
diagnostic horizons or characteristics of clay enrichment. They comprise a large
number of soil series, 3,534 and 1,410, respectively, in the USA. Within the
Spodosols, there is a high number (161) and proportion (22 %) of soil series with
an argillic or kandic-like horizon. Andisols contain 109 soil series with an argillic
horizon, which constitutes 11 % of the total soil series in that order and an area of
about 17,150 km 2 . The remaining soil orders, Inceptisols, Oxisols, and Vertisols,
each contain eight soil series or less and collectively comprise about 4,275 km 2 in the
USA. A total of 44 % of the soil series in the USA contain taxonomically defined soil
horizons or characteristics reflecting clay illuviation. These soils account for an area
of 4.5 million km 2 , which is 56 % of the area of conterminous USA.
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