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Table 1 Effects of temperature, moisture and forest type on cumulative mineralized carbon (Cmin)

From: Recalcitrant carbon controls the magnitude of soil organic matter mineralization in temperate forests of northern China

Variable

Df

Sum Sq

Mean Sq

F

P

F

2

5989

2994

7.066

0.0011

M

2

87,270

43,635

102.98

<2e-16

T

5

15,736

3147

7.427

1.89e-06

F × M

4

3387

847

1.998

0.959

F × T

10

3683

368

0.869

0.563

M × T

10

5403

540

1.275

0.246

F × M × T

20

3041

152

0.359

0.995

  1. F, M and T represent forest type, moisture content, and temperature, respectively