The Q10* values (±SD) of SOC decomposition for different particle-size fractions in grassland and forest soils (n = 4).
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*Q10 value was calculated using Eqn. 3 with the parameters for the fitted curves in Figure 2.§The mean was calculated including each replicate among the three temperature-change cycles (n = 12).¶Different lowercase letters in the same row indicate significance differences (p#Different capital letters in the same column indicate significance differences (p
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2015-12-02



