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量化农业土壤中不同水分条件下硝化作用和反硝化作用产生氧化亚氮的速率:实验室研究与文献综述

Quantifying nitrous oxide production rates from nitrification and denitrification under various moisture conditions in agricultural soils: Laboratory study and literature synthesis.

作者信息

Wang Hui, Yan Zhifeng, Ju Xiaotang, Song Xiaotong, Zhang Jinbo, Li Siliang, Zhu-Barker Xia

机构信息

School of Earth System Science, Institute of Surface-Earth System Science, Tianjin University, Tianjin, China.

Critical Zone Observatory of Bohai Coastal Region, Tianjin Key Laboratory of Earth Critical Zone Science and Sustainable Development in Bohai Rim, Tianjin University, Tianjin, China.

出版信息

Front Microbiol. 2023 Jan 12;13:1110151. doi: 10.3389/fmicb.2022.1110151. eCollection 2022.

Abstract

Biogenic nitrous oxide (NO) from nitrification and denitrification in agricultural soils is a major source of NO in the atmosphere, and its flux changes significantly with soil moisture condition. However, the quantitative relationship between NO production from different pathways (i.e., nitrification vs. denitrification) and soil moisture content remains elusive, limiting our ability of predicting future agricultural NO emissions under changing environment. This study quantified NO production rates from nitrification and denitrification under various soil moisture conditions using laboratory incubation combined with literature synthesis. N labeling approach was used to differentiate the NO production from nitrification and denitrification under eight different soil moisture contents ranging from 40 to 120% water-filled pore space (WFPS) in the laboratory study, while 80 groups of data from 17 studies across global agricultural soils were collected in the literature synthesis. Results showed that as soil moisture increased, NO production rates of nitrification and denitrification first increased and then decreased, with the peak rates occurring between 80 and 95% WFPS. By contrast, the dominant NO production pathway switched from nitrification to denitrification between 60 and 70% WFPS. Furthermore, the synthetic data elucidated that moisture content was the major driver controlling the relative contributions of nitrification and denitrification to NO production, while NH and NO concentrations mainly determined the NO production rates from each pathway. The moisture treatments with broad contents and narrow gradient were required to capture the comprehensive response of soil NO production rate to moisture change, and the response is essential for accurately predicting NO emission from agricultural soils under climate change scenarios.

摘要

农业土壤中硝化作用和反硝化作用产生的生物源一氧化二氮(N₂O)是大气中N₂O的主要来源,其通量随土壤湿度条件的变化而显著变化。然而,不同途径(即硝化作用与反硝化作用)产生的N₂O与土壤含水量之间的定量关系仍不明确,这限制了我们预测变化环境下未来农业N₂O排放的能力。本研究采用实验室培养结合文献综合分析的方法,量化了不同土壤湿度条件下硝化作用和反硝化作用产生的N₂O速率。在实验室研究中,采用N标记方法区分了在8种不同土壤湿度(含水量为40%至120%的充水孔隙空间,即WFPS)下硝化作用和反硝化作用产生的N₂O,同时在文献综合分析中收集了全球农业土壤17项研究中的80组数据。结果表明,随着土壤湿度增加,硝化作用和反硝化作用产生的N₂O速率先增加后降低,峰值速率出现在80%至95% WFPS之间。相比之下,N₂O的主要产生途径在60%至70% WFPS之间从硝化作用转变为反硝化作用。此外,综合数据表明,含水量是控制硝化作用和反硝化作用对N₂O产生相对贡献的主要驱动因素,而NH₄⁺和NO₃⁻浓度主要决定了各途径产生的N₂O速率。需要采用宽含量和窄梯度的湿度处理来捕捉土壤N₂O产生速率对湿度变化的综合响应,而这种响应对于准确预测气候变化情景下农业土壤的N₂O排放至关重要。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bfd5/9877343/4c27c2e265e8/fmicb-13-1110151-g001.jpg

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