Wang Jinsong, Wu L, Zhang Chunyu, Zhao Xiuhai, Bu Wensheng, Gadow Klaus V
Key Laboratory for Forest Resources and Ecosystem Processes, Beijing Forestry University, Beijing, 100083, China.
Synthesis Research Center of Chinese Ecosystem Research Network, Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, 100101, China.
Environ Sci Pollut Res Int. 2016 Nov;23(22):22701-22710. doi: 10.1007/s11356-016-7474-7. Epub 2016 Aug 25.
The response of soil respiration (Rs) to nitrogen (N) addition is one of the uncertainties in modelling ecosystem carbon (C). We reported on a long-term nitrogen (N) addition experiment using urea (CO(NH)) fertilizer in which Rs was continuously measured after N addition during the growing season in a Chinese pine forest. Four levels of N addition, i.e. no added N (N0: 0 g N m year), low-N (N1: 5 g N m year), medium-N (N2: 10 g N m year), and high-N (N3: 15 g N m year), and three organic matter treatments, i.e. both aboveground litter and belowground root removal (LRE), only aboveground litter removal (LE), and intact soil (CK), were examined. The Rs was measured continuously for 3 days following each N addition application and was measured approximately 3-5 times during the rest of each month from July to October 2012. N addition inhibited microbial heterotrophic respiration by suppressing soil microbial biomass, but stimulated root respiration and CO release from litter decomposition by increasing either root biomass or microbial biomass. When litter and/or root were removed, the "priming" effect of N addition on the Rs disappeared more quickly than intact soil. This is likely to provide a point of view for why Rs varies so much in response to exogenous N and also has implications for future determination of sampling interval of Rs measurement.
土壤呼吸(Rs)对氮(N)添加的响应是生态系统碳(C)建模中的不确定因素之一。我们报道了一项在中国油松林生长季节使用尿素(CO(NH))肥料进行的长期氮添加实验,在添加氮后持续测量Rs。研究了四个氮添加水平,即不添加氮(N0:0 g N m² 年)、低氮(N1:5 g N m² 年)、中氮(N2:10 g N m² 年)和高氮(N3:15 g N m² 年),以及三种有机质处理,即地上凋落物和地下根系去除(LRE)、仅地上凋落物去除(LE)和完整土壤(CK)。每次添加氮后连续3天测量Rs,并在2012年7月至10月的每个月剩余时间内大约测量3 - 5次。氮添加通过抑制土壤微生物生物量来抑制微生物异养呼吸,但通过增加根系生物量或微生物生物量来刺激根系呼吸和凋落物分解过程中的CO₂ 释放。当凋落物和/或根系被去除时,氮添加对Rs的“激发”效应比完整土壤消失得更快。这可能为Rs对外源氮的响应为何变化如此之大提供一个观点,也对未来Rs测量采样间隔的确定具有启示意义。