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. 2020 Aug 6;7(19):2001242. doi: 10.1002/advs.202001242

Figure 3.

Figure 3

The temperature sensitivity of soil organic carbon decomposition (Q 10) with soil depth among biome types. Shaded areas indicate the 95% confidence intervals for each biome type. Linear mixed‐effects models are used to evaluate the effect of soil depth on Q 10 with excluding autocorrelations of different sampling sites and depths, showing that Q 10 for each biome type significantly increases with soil depth (P < 0.001).