沉积(地质)
温带森林
土壤碳
氮气
土壤水分
环境化学
碳循环
化学
碳纤维
土壤呼吸
铵
环境科学
分解
温带气候
硝酸盐
氮气循环
农学
生态系统
土壤科学
植物
生态学
生物
材料科学
沉积物
复合数
古生物学
复合材料
有机化学
作者
Yuhan Du,Peng Guo,Jianqiu Liu,Chunyu Wang,Yang Ning,Zhenxia Jiao
摘要
Nitrogen (N) deposition significantly affects the soil carbon (C) cycle process of forests. However, the influence of different types of N on it still remained unclear. In this work, ammonium nitrate was selected as an inorganic N (IN) source, while urea and glycine were chosen as organic N (ON) sources. Different ratios of IN to ON (1 : 4, 2 : 3, 3 : 2, 4 : 1, and 5 : 0) were mixed with equal total amounts and then used to fertilize temperate forest soils for 2 years. Results showed that IN deposition inhibited soil C cycle processes, such as soil respiration, soil organic C decomposition, and enzymatic activities, and induced the accumulation of recalcitrant organic C. By contrast, ON deposition promoted these processes. Addition of ON also resulted in accelerated transformation of recalcitrant compounds into labile compounds and increased CO2 efflux. Meanwhile, greater ON deposition may convert C sequestration in forest soils into C source. These results indicated the importance of the IN to ON ratio in controlling the soil C cycle, which can consequently change the ecological effect of N deposition.
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