Table 3

C/N ratios of the organic matter 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.

C/N ratios in grain size


Sand

Silt

Clay



Horizon

Depth cm

Coarse/Medium

Fine

Coarse

Medium

Fine



2.0-0.2

0.2-0.063

0.063-0.020

0.020-0.0063

0.0063-0.002

<0.002


mm


3 years

Ah

10(12)(1)

31.4

28.8

14.0

12.9

12.0

10.7

Ap1

22

25.0

24.2

14.2

12.1

12.0

11.2

33

34.7

nd

14.9

14.3

12.0

10.9

Ap2

40

nd

nd

23.2

14.9

12.0

9.6

20 years

Ah

2

21.0

24.5

16.5

13.2

12.4

8.3

Ap1

18

nd

nd

19.0

15.5

13.5

9.2

Ap2

25(28)

nd

nd

21.3

18.0

15.5

10.1

55 years

Ah-E

1

nd

nd

nd

nd

Nd

nd

Ap1

8

nd

nd

38.9

24.2

23.8

13.2

Ap2

19

nd

nd

45.2

26.3

24.2

15.0

100 years

E

2

nd

nd

29.8

30.4

21.7

18.9

Bsh

5

nd

nd

32.0

26.7

21.5

15.1

Ap

10

36.7

nd

30.9

24.0

21.6

13.7

170 years

E

2

53.1

42.8

24.0

24.4

18.5

14.8

Bsh

6

nd

nd

30.5

28.6

17.1

14.6

Ap

15

nd

nd

46.9

29.9

24.9

17.5

Albic Podzol

E

6(8)

nd

nd

44.6

38.0

28.5

17.7

Bsh

10

nd

nd

31.6

26.8

22.9

17.5


nd - not determined

(1) Depths descriptions in parentheses indicate partly thicker horizons

Kalinina et al. Carbon Balance and Management 2010 5:1   doi:10.1186/1750-0680-5-1

Open Data