Table 3 model predictions of SOC stocks (in t ha−1), parenthesis contains minimum and maximum of the 95% C.I.

From: Generic parameters of first-order kinetics accurately describe soil organic matter decay in bare fallow soils over a wide edaphic and climatic range

 

Askov 1

Askov 2

Grignon

Kursk

Rothamsted

Ultuna

Versailles

300 years

17.1 (12.1–21.6)

15.7 (11.1–19.8)

16.6 (10.3–20.6)

58.5 (28.7–71.1)

16.6 (14–19.8)

14.9 (12–18.2)

14.1 (12–16.7)

1000 years

12 (6.9–17.2)

11 (6.4–15.7)

11.8 (9.7–14.1)

66.2 (57.8–72.4)

12.2 (10.9–13.5)

11.2 (8.4–13.7)

9.3 (8.3–10.1)

3000 years

7.7 (4.7–12.6)

7 (4.3–11.5)

9.4 (6.3–13.1)

45.8 (34.8–60.8)

13.5 (11.6–15.2)

8.4 (6.1–11.6)

10.8 (9.6–12.4)

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