Possible Mechanisms Leading to a Delay in Carbon Stock Recovery after Land Use Change

Changes in land use sometimes lead to soil C loss, and a long time may be required for the C stock to recover to initial levels. Thus, it is important to evaluate the mechanisms related to accumulation of newly input C following land use changes. In this study, we sought to determine the signature of newly input C in the soil profile after land use change. We used stable and radioactive C isotopes with soil fractionation methods in a C3 coniferous plantation converted from C4 grassland in Japan. The difference in delta13C values between the surface litter and the soil organic carbon (SOC) below the litter was 5 ppt or greater; this large isotopic difference was attributed to rapid decomposition in the litter layer and preservation of C derived from the previous C4 vegetation. Most SOC delta14C values were negative throughout the soil profile, suggesting that most of the SOC in the soil profile was recalcitrant and had been preserved for a long time. Only the surface sand values were slightly positive. These results suggest that most newly input C is consumed at the soil surface. The low ability of these soils to preserve newly input C is one factor in the slow recovery of soil C.