土壤碳
碳纤维
总有机碳
土壤水分
环境科学
土壤科学
环境化学
碳循环
溶解有机碳
化学
生态学
生态系统
数学
生物
算法
复合数
作者
Volker Hahn,Nina Buchmann
摘要
A new model is presented that uses bomb carbon ( 14 C enrichment) to calculate the turnover times of active soil organic carbon (SOC). The new approach overcomes major deficiencies of older models, particularly in respect to the 14 C content of carbon input to SOC and of carbon output from SOC. Calculated turnover times of active carbon for ten European forest sites ranged from 4.0 to 15.1 years with a mean of 8.2 years. The model was successfully validated in soil incubation experiments, where the measured 14 C content of (microbially) respired CO 2 was on average 9.6% (ΔpM) higher than that of bulk SOC, but agreed considerably well with the modeled 14 C content. Furthermore, we used the model's sensitivity tests to show that over long time periods (decades), soils can only sequester small amounts of carbon.
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