Xiao Wang , Xiangming Zhu , Yunying Fang , Tony Vancov , Zhichao Zou , Xiaoying Jin , Lixiao Ma , Di Wu , Zhangliu Du
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The results showed that N fertilization distinctly modified the molecular signature of SOM (e.g., biomolecules, degradation, and source) within the soil profile, particularly within the top 20 cm layer. N additions led to a 13.6–17.3 % increase in microbial-derived free lipids (predominantly short-chain lipids, <C<sub>20</sub>) and accelerated the degradation of aliphatic lipids in the topsoil, as indicated by an increased average chain length of aliphatic lipids. The response of lignin phenols and their degradation to varying levels of N addition differed across soil layers. Compared to the control, N enrichment increased cutin compounds by 26.7–93.7 %, whereas the impact on cutin and suberin<em>-</em>derived lipids was negligible. N fertilization reduced plant-derived neutral sugars by 5.8–26.5 % and microbial-derived neutral sugars by 10.2–15.9 % relative to ambient. Changes in bacterial and fungal necromass C, total microbial necromass C, and their contributions to soil organic C varied across treatments within specific soil layer. Furthermore, N enrichment was associated with microbial C limitation (as indicated by increased vector length) and a decrease in soil microbial C use efficiency, with a bias towards the decomposition of more labile biomolecules such as short-chain lipids, O-alkyl C, while more recalcitrant compounds (e.g., alkyl C, aromatic + phenolic C) were preserved. Collectively, our study offers mechanistic insights into the consequences of N enrichment on SOM compositions and stability at the molecular level, critical for understanding its persistence and broader functionality under impending global change paradigms.</div></div>","PeriodicalId":7512,"journal":{"name":"Agriculture, Ecosystems & Environment","volume":"379 ","pages":"Article 109373"},"PeriodicalIF":6.0000,"publicationDate":"2024-11-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Long-term nitrogen fertilization accelerates labile biomolecules decomposition and retains recalcitrant compounds in a temperate agroecosystem\",\"authors\":\"Xiao Wang , Xiangming Zhu , Yunying Fang , Tony Vancov , Zhichao Zou , Xiaoying Jin , Lixiao Ma , Di Wu , Zhangliu Du\",\"doi\":\"10.1016/j.agee.2024.109373\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The influence of long-term nitrogen (N) fertilization on the quantity, molecular constituents, and origin of soil organic matter (SOM) within the soil profile remains an area of ongoing investigation. We employed a comprehensive set of biomarkers (including free lipids, bound lipids, lignin phenols, neutral sugars, and amino sugars), <sup>13</sup>C NMR techniques, and soil extracellular enzyme activities, to evaluate the SOM characteristics in response to 18-year N fertilizer gradients (i.e., 0, 57.5, 97.5, 137.5 kg N ha<sup>−1</sup> yr<sup>−1</sup>) to a depth of 60 cm in Northeast China. The results showed that N fertilization distinctly modified the molecular signature of SOM (e.g., biomolecules, degradation, and source) within the soil profile, particularly within the top 20 cm layer. N additions led to a 13.6–17.3 % increase in microbial-derived free lipids (predominantly short-chain lipids, <C<sub>20</sub>) and accelerated the degradation of aliphatic lipids in the topsoil, as indicated by an increased average chain length of aliphatic lipids. The response of lignin phenols and their degradation to varying levels of N addition differed across soil layers. Compared to the control, N enrichment increased cutin compounds by 26.7–93.7 %, whereas the impact on cutin and suberin<em>-</em>derived lipids was negligible. N fertilization reduced plant-derived neutral sugars by 5.8–26.5 % and microbial-derived neutral sugars by 10.2–15.9 % relative to ambient. Changes in bacterial and fungal necromass C, total microbial necromass C, and their contributions to soil organic C varied across treatments within specific soil layer. Furthermore, N enrichment was associated with microbial C limitation (as indicated by increased vector length) and a decrease in soil microbial C use efficiency, with a bias towards the decomposition of more labile biomolecules such as short-chain lipids, O-alkyl C, while more recalcitrant compounds (e.g., alkyl C, aromatic + phenolic C) were preserved. 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引用次数: 0
摘要
长期施氮(N)对土壤剖面中土壤有机质(SOM)的数量、分子成分和来源的影响仍然是一个正在研究的领域。我们采用了一整套生物标志物(包括游离脂质、结合脂质、木质素酚类、中性糖和氨基糖)、13C NMR 技术和土壤胞外酶活性,评估了中国东北地区土壤有机质对 18 年氮肥梯度(即 0、57.5、97.5 和 137.5 kg N ha-1 yr-1)的响应特征。结果表明,氮肥施用明显改变了土壤剖面中 SOM 的分子特征(如生物大分子、降解和来源),尤其是顶部 20 厘米层。氮的添加导致微生物衍生的游离脂质(主要是短链脂质,C20)增加了 13.6-17.3%,并加速了表层土壤中脂肪族脂质的降解,脂肪族脂质平均链长的增加表明了这一点。不同土层的木质素酚及其降解对不同水平氮添加的反应各不相同。与对照组相比,氮的富集使木质素化合物增加了 26.7%-93.7% ,而对木质素和次木质素衍生脂类的影响则可以忽略不计。与环境相比,氮肥使植物衍生的中性糖减少了 5.8-26.5%,微生物衍生的中性糖减少了 10.2-15.9%。在特定土层中,不同处理的细菌和真菌死亡物质 C、微生物死亡物质 C 总量及其对土壤有机碳的贡献各不相同。此外,氮的富集与微生物的碳限制(表现为矢量长度增加)和土壤微生物的碳利用效率下降有关,偏向于分解更易腐烂的生物大分子,如短链脂类、O-烷基碳,而保留更难分解的化合物(如烷基碳、芳香族+酚类碳)。总之,我们的研究从机理上揭示了氮富集在分子水平上对 SOM 组成和稳定性的影响,这对理解其在即将到来的全球变化模式下的持久性和更广泛的功能至关重要。
Long-term nitrogen fertilization accelerates labile biomolecules decomposition and retains recalcitrant compounds in a temperate agroecosystem
The influence of long-term nitrogen (N) fertilization on the quantity, molecular constituents, and origin of soil organic matter (SOM) within the soil profile remains an area of ongoing investigation. We employed a comprehensive set of biomarkers (including free lipids, bound lipids, lignin phenols, neutral sugars, and amino sugars), 13C NMR techniques, and soil extracellular enzyme activities, to evaluate the SOM characteristics in response to 18-year N fertilizer gradients (i.e., 0, 57.5, 97.5, 137.5 kg N ha−1 yr−1) to a depth of 60 cm in Northeast China. The results showed that N fertilization distinctly modified the molecular signature of SOM (e.g., biomolecules, degradation, and source) within the soil profile, particularly within the top 20 cm layer. N additions led to a 13.6–17.3 % increase in microbial-derived free lipids (predominantly short-chain lipids, <C20) and accelerated the degradation of aliphatic lipids in the topsoil, as indicated by an increased average chain length of aliphatic lipids. The response of lignin phenols and their degradation to varying levels of N addition differed across soil layers. Compared to the control, N enrichment increased cutin compounds by 26.7–93.7 %, whereas the impact on cutin and suberin-derived lipids was negligible. N fertilization reduced plant-derived neutral sugars by 5.8–26.5 % and microbial-derived neutral sugars by 10.2–15.9 % relative to ambient. Changes in bacterial and fungal necromass C, total microbial necromass C, and their contributions to soil organic C varied across treatments within specific soil layer. Furthermore, N enrichment was associated with microbial C limitation (as indicated by increased vector length) and a decrease in soil microbial C use efficiency, with a bias towards the decomposition of more labile biomolecules such as short-chain lipids, O-alkyl C, while more recalcitrant compounds (e.g., alkyl C, aromatic + phenolic C) were preserved. Collectively, our study offers mechanistic insights into the consequences of N enrichment on SOM compositions and stability at the molecular level, critical for understanding its persistence and broader functionality under impending global change paradigms.
期刊介绍:
Agriculture, Ecosystems and Environment publishes scientific articles dealing with the interface between agroecosystems and the natural environment, specifically how agriculture influences the environment and how changes in that environment impact agroecosystems. Preference is given to papers from experimental and observational research at the field, system or landscape level, from studies that enhance our understanding of processes using data-based biophysical modelling, and papers that bridge scientific disciplines and integrate knowledge. All papers should be placed in an international or wide comparative context.