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Table 1 CH4 oxidation activity of soil incubated under aerobic and anaerobic conditions. Rate constant k is the slope of log scale CH4 concentration over time during the rapid decline incubation period

From: Methane oxidation and methane driven redox process during sequential reduction of a flooded soil ecosystem

Incubation condition

Day of incubation

Apparent rate constant

k (μg CH4 day−1 g−1 soil)

Aerobic

0

0.46 ± 0.05

5

0.64 ± 0.02

10

0.68 ± 0.01

20

0.68 ± 0.01

40

0.38 ± 0.01

60

0.32 ± 0.02

Anaerobic

0

0.46 ± 0.05

5

0.44 ± 0.02

10

0.44 ± 0.01

20

0.42 ± 0.01

40

0.15 ± 0.02

60

0.07 ± 0.01