资源环境科技发展态势分析平台

Terrestrial carbon cycle feedbacks to global warming are major uncertainties in climate models. For in-depth understanding of changes in soil organic carbon (SOC) after soil warming, long-term responses of SOC stabilization mechanisms such as aggregation, organo-mineral interactions and chemical recalcitrance need to be addressed. This study investigated the effect of 6 years of geothermal soil warming on different SOC fractions in an unmanaged grassland in Iceland. Along an extreme warming gradient of + 0 to similar to+ 40 degrees C, we isolated five fractions of SOC that varied conceptually in turnover rate from active to passive in the following order: particulate organic matter (POM), dissolved organic carbon (DOC), SOC in sand and stable aggregates (SA), SOC in silt and clay (SC-rSOC) and resistant SOC (rSOC). Soil warming of 0.6 degrees C increased bulk SOC by 22 +/- 43% (0-10 cm soil layer) and 27 +/- 54% (20-30 cm), while further warming led to exponential SOC depletion of up to 79 +/- 14% (0-10 cm) and 74 +/- 8% (20-30) in the most warmed plots (similar to+ 40 degrees C). Only the SA fraction was more sensitive than the bulk soil, with 93 +/- 6% (0-10 cm) and 86 +/- 13% (20-30 cm) SOC losses and the highest relative enrichment in C-13 as an indicator for the degree of decomposition (+ 1.6 +/- 1.5 parts per thousand in 0-10 cm and + 1.3 +/- 0.8 parts per thousand in 20-30 cm). The SA fraction mass also declined along the warming gradient, while the SC fraction mass increased. This was explained by deactivation of aggregate-binding mechanisms. There was no difference between the responses of SC-rSOC (slow-cycling) and rSOC (passive) to warming, and C-13 enrichment in rSOC was equal to that in bulk soil. We concluded that the sensitivity of SOC to warming was not a function of age or chemical recalcitrance, but triggered by changes in biophysical stabilization mechanisms, such as aggregation.