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. 2013 Nov 25;3(16):5177–5188. doi: 10.1002/ece3.895

Table 2.

Comparison between the seasonal temperature relationship of in situ measurements for soil C emissions and of the temperature sensitivity of C mineralization data of spatially paired samples expressed as Q10 values for the control-irrigated treatment (I) and the fertilized-irrigated treatment (FI), respectively (mean and standard error in brackets of n = 2 field replicates × 3 subsamples = 6 samples, because there were no significant differences between field replicates). Field temperature measurements were made at 10 cm depth

Q10 for C mineralization

Seasonal Q10 for in situ C-CO2 fluxes O horizon E horizon
I 4.1 (0.5) 2.8 (0.2) 2.8 (0.2)
FI 4.8 (0.6) 3.4 (0.1) 3.6 (0.3)