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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