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DOI | 10.1016/j.soilbio.2021.108355 |
Shifts in the dynamic mechanisms of soil organic matter transformation with nitrogen addition: From a soil carbon/nitrogen-driven mechanism to a microbe-driven mechanism | |
Chen, Qiuyu; Hu, Yilun; Hu, Ang; Niu, Bin; Yang, Xiaoqin; Jiao, Hongzhe; Xu-Ri; Song, Lili; Zhang, Gengxin | |
通讯作者 | Zhang, GX (通讯作者) |
发表日期 | 2021 |
ISSN | 0038-0717 |
EISSN | 1879-3428 |
卷号 | 160 |
英文摘要 | Impacts of atmospheric nitrogen (N) deposition on soil carbon (C) dynamics are highly variable, and the underlying mechanisms remain unclear. This limits our ability to predict soil responses to climate change. Labilefraction soil organic matter (LF-SOM), which is the earliest-responding indicator of soil changes, was examined to investigate SOM dynamics on a Tibetan alpine steppe in response to N addition at six levels (0, 10, 20, 40, 80 and 160 kg.N.ha(-1).yr(-1)) after 2 and 5 years. LF-SOM fingerprints (pyrolysis-gas chromatography/tandem-mass spectrometry) combined with microbial community data (high-throughput sequencing) were used to explore LFSOM responses to N addition and their drivers. LF-SOM showed accumulation (N10-N20) and decomposition (N40-N160) in the 2nd year of N addition but only decomposition (N10-N160) in the 5th year. Organic compounds in LF-SOM showed high sensitivity (90% significant correlations with the N level) but low resistance (0.38 resistance index) and low sensitivity (no significant correlation) but high resistance (0.48) to the N level in the 2nd year and 5th year, respectively. Abiotic and biotic factors showed higher sensitivity to the N level in the 2nd year (more than 70% significant correlations) than in the 5th year (approximately 20% significant correlations), and biotic factors showed higher resistance (0.83) to the N level in the 5th year than in the 2nd year (0.73). Abiotic factors, mainly the soil C/N balance, were the primary drivers of LF-SOM transformation in the 2nd year, while biotic factors, primarily microbes, were the main drivers of LF-SOM decomposition in the 5th year. Our study demonstrated that the variable impacts of N deposition on LF-SOM transformation depended on shifts in the responses of abiotic and biotic factors to N accumulation. This understanding is significant for predicting terrestrial ecosystem functions under future N deposition. |
关键词 | CARBONPLANTLITTERSTOICHIOMETRYDECOMPOSITIONBIODIVERSITYSPECTROMETRYCOMMUNITIESGRASSLANDSLIMITATION |
英文关键词 | N deposition; Soil organic matter transformation; Abiotic factor; Biotic factor; Sensitivity; Resistance |
语种 | 英语 |
WOS研究方向 | Agriculture |
WOS类目 | Soil Science |
WOS记录号 | WOS:000692631600004 |
来源期刊 | SOIL BIOLOGY & BIOCHEMISTRY |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/260310 |
推荐引用方式 GB/T 7714 | Chen, Qiuyu,Hu, Yilun,Hu, Ang,et al. Shifts in the dynamic mechanisms of soil organic matter transformation with nitrogen addition: From a soil carbon/nitrogen-driven mechanism to a microbe-driven mechanism[J]. 中国科学院青藏高原研究所,2021,160. |
APA | Chen, Qiuyu.,Hu, Yilun.,Hu, Ang.,Niu, Bin.,Yang, Xiaoqin.,...&Zhang, Gengxin.(2021).Shifts in the dynamic mechanisms of soil organic matter transformation with nitrogen addition: From a soil carbon/nitrogen-driven mechanism to a microbe-driven mechanism.SOIL BIOLOGY & BIOCHEMISTRY,160. |
MLA | Chen, Qiuyu,et al."Shifts in the dynamic mechanisms of soil organic matter transformation with nitrogen addition: From a soil carbon/nitrogen-driven mechanism to a microbe-driven mechanism".SOIL BIOLOGY & BIOCHEMISTRY 160(2021). |
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