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压缩作用促进城市公园土壤的反硝化作用:¹⁵N 示踪技术的应用。

Compaction stimulates denitrification in an urban park soil using ¹⁵N tracing technique.

机构信息

Key Laboratory of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, 361021, Xiamen, China.

出版信息

Environ Sci Pollut Res Int. 2014 Mar;21(5):3783-91. doi: 10.1007/s11356-013-2355-9. Epub 2013 Nov 28.

Abstract

Soils in urban areas are subjected to compaction with accelerating urbanization. The effects of anthropogenic compaction on urban soil denitrification are largely unknown. We conducted a study on an urban park soil to investigate how compaction impacts denitrification. By using (15)N labeling method and acetylene inhibition technique, we performed three coherent incubation experiments to quantify denitrification in compacted soil under both aerobic and anaerobic conditions. Uncompacted soil was set as the control treatment. When monitoring soil incubation without extra substrate, higher nitrous oxide (N2O) flux and denitrification enzyme activity were observed in the compacted soil than in the uncompacted soil. In aerobic incubation with the addition of K(15)NO3, N2O production in the compacted soil reached 10.11 ng N h(-1) g(-1) as compared to 0.02 ng N h(-1) g(-1) in the uncompacted soil. Denitrification contributed 96 % of the emitted N2O in the compacted soil and 36 % of the emitted N2O in the uncompacted soil; total denitrification rate was higher in the compacted soil (up to 79.35 ng N h(-1) g(-1)) than in the uncompacted soil (0.11 ng N h(-1) g(-1)). Under anaerobic incubation with the addition of K(15)NO3, no statistical difference in total N losses and (15)N-(N2O+N2) flux between the uncompacted soil and the compacted soil was detected. Compaction promoted soil denitrification and may impact urban N biogeochemical cycling.

摘要

随着城市化的加速,城市土壤受到压实的影响。人为压实对城市土壤反硝化的影响在很大程度上尚不清楚。我们对城市公园土壤进行了一项研究,以调查压实如何影响反硝化作用。我们使用(15)N 标记法和乙炔抑制技术,进行了三个连贯的培养实验,以量化有氧和厌氧条件下压实土壤中的反硝化作用。未压实的土壤作为对照处理。在监测没有额外基质的土壤培养时,压实土壤中的硝态氮(N2O)通量和反硝化酶活性较高。在有氧培养中添加 K(15)NO3 时,压实土壤中的 N2O 生成量达到 10.11ngN h(-1) g(-1),而未压实土壤中的 N2O 生成量仅为 0.02ngN h(-1) g(-1)。在压实土壤中,反硝化作用贡献了排放的 N2O 的 96%,而在未压实土壤中贡献了 36%;压实土壤中的总反硝化速率较高(高达 79.35ngN h(-1) g(-1)),而未压实土壤中的总反硝化速率较低(0.11ngN h(-1) g(-1))。在有氧培养中添加 K(15)NO3 时,未压实土壤和压实土壤之间的总氮损失和(15)N-(N2O+N2)通量没有统计学差异。压实促进了土壤反硝化作用,并可能影响城市氮生物地球化学循环。

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