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Influence of hydromorphic soil condition (1)

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Table 1
Fig. 1. Mean values ± standard error of the mean for (A) soil water content (vol.%), (B) soil temperature (�C), (C) N2O flux (lg N2O–N m�2 h�1), (D) CH4 flux (lg CH4–C m�2 h�1), (E) soil carbon stock (Mg C ha�1), (F) soil nitrogen stock (Mg N ha�1), (G) mine
Table 2
Fig. 3. Comparison of mean ± standard error potential rates of (A) CH4 oxidation at a starting concentration of 2 lL L�1, (B) CH4 oxidation at a starting concentration of10,000 lL L�1, (C) CH4 production, (D) N2O production and (E) indirect measure of N2 p

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