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Table 10.3 Analytical properties of alpine cryosols
Depth
(cm)
Silt
(%)
Clay
(%)
SOC
(%)
CEC
(cmol+/kg)
BS
(%)
Fe d
(%)
Location
Horizon
pH
C:N
Polar Urals; Typic Aquiturbels (Lesovaya et al. 2012 )
Cjjg1
0-10
35.2
11.1
8.8
0.7
17.1
4
2.06
Cjjg2
10-20
47.3
17.2
7.8
0.5
28.1
5
1.34
Polar urals; Typic A quiturbels (Lesovaya et al. 2012 )
A
0-4
20.8
7.8
7.2
16.3
25.5
26
2.68
Cg1
4-15
23.3
6.8
7
4.7
27.6
14
4.05
Cg2
15-30
48.6
17.4
8
1.9
24.2
4
1.53
Subpolar
Ural
Mtns.,
Pedon: 25-09; Typic Aquiturbels (Dymov et al. 2013 )
Russia
Oi
0-5
3.9
41.4
56
66
Ag
5-14
36
21
5.2
0.8
12
8.8
BCg
14-37
37
22
5.1
0.7
12
9.6
Cg
37
30
18
5.2
0.1
2
8.1
Northern Rocky Mtns., Sapristels (Johnson and
Billings 1962 )
Oa1 2-5 45.7 4.2 6.4 10.5
Oa2 15-20 41.2 12 5.2 8.8
Oa3 36-46 34.5 10.5 6.2 1
Northern Rocky Mtns., Haploturbels (Johnson and Billings
1962 )
A 2-16 30.9 4.9 5.3 9.8
C 15-30 28.4 4.7 5.5 5.9
Northern Rocky Mtns., Haploturbels (Johnson and Billings
1962 )
C1 2-5 66.9 7.3 5.8 0.29
C2 10-15 65.6 7.6 5.6 0.29
C3 36-38 69.5 8.5 6.6 0
Central Khangai, Mongolia, Haplorthels (Krasnoshchekov
2010 )
O
0-1
nd
nd
5.6
45.2
24.5
60
A
1-19
34
17
5.3
10.6
23.4
50
C
19-25
20
11
5.8
1.4
3.1
78
Central Khangai, Mongolia, Umbrorthels (Krasnoshchekov
2010 )
Oa
0-15
16
7
4.7
28.5
17
25.1
52
AC
15-25
10
6
4.2
15.7
34
23.2
70
Central Khangai, Mongolia, Histoturbels (Krasnoshchekov
2010 )
Oi
0-6
5.4
45.3
40.8
57
Oe
6-20
5.8
38.8
57.5
67
Crg
25-36
46
22
5.3
2.3
18.7
56
(continued)
 
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