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Table 2 Contents of organic carbon within the grain size fractions of the topsoils after 3, 20, 55, 100, and 170 years under self-restoration and of an Albic Podzol, never been cultivated.

From: Dynamics of carbon pools in post-agrogenic sandy soils of southern taiga of Russia

  

OC content in grain size

  

Sand

Silt

Clay

Horizon

Depth

2.0 - 0.2 mm

0.2 - 0.063 mm

0.063 - 0.020 mm

0.020 - 0.0063 mm

0.0063 - 0.002 mm

<0.002 mm

 

cm

% of SOC

3 years

Ah

10(12)(1)

33.0

19.3

21.6

8.4

10.8

6.3

Ap1

22

34.6

15.8

22.2

5.7

13.9

7.5

 

33

35.0

9.5

16.4

6.9

10.8

8.7

Ap2

40

39.1

6.5

11.1

8.2

14.1

13.1

20 years

Ah

2

38.9

12.3

20.5

8.6

10.4

8.3

Ap1

18

20.4

10.5

17.1

12.5

16.6

15.2

Ap2

25(28)

22.5

9.4

21.2

12.2

21.3

13.1

55 years

Ah-E

1

Nd

nd

nd

nd

nd

nd

Ap1

8

32.2

6.8

10.1

12.3

11.4

9.1

Ap2

19

24.4

7.8

15.2

21.7

13.6

13.3

100 years

E

2

43.1

3.3

23.9

7.2

13.1

9.1

Bsh

5

41.3

5.1

15.2

15.3

10.9

6.8

Ap

10

37.1

6.5

16.4

23.6

8.9

7.0

170 years

E

2

50.1

4.4

14.5

9.0

13.8

8.1

Bsh

6

31.2

4.9

16.2

12.7

14.1

9.3

Ap

15

30.5

9.1

17.3

16.4

10.1

13.8

Albic Podzol

E

6(8)

41.6

5.2

16.7

13.3

12.6

10.4

Bsh

10

35.4

7.3

8.8

6.3

6.0

6.5

  1. nd - not determined
  2. (1) Depths descriptions in parentheses indicate partly thicker horizons