Crop straw incorporation interacts with N fertilizer on N2O emissions in an intensively cropped farmland

被引:66
作者
Xu, Cong [1 ,2 ]
Han, Xiao [1 ]
Ru, Shuhua [3 ]
Cardenas, Laura [4 ]
Rees, Robert M. [5 ]
Wu, Di [1 ,6 ]
Wu, Wenliang [1 ]
Meng, Fanqiao [1 ]
机构
[1] China Agr Univ, Beijing Key Lab Biodivers & Organ Farming, Beijing Key Lab Farmland Soil Pollut Prevent & Re, Coll Resources & Environm Sci, Beijing 100193, Peoples R China
[2] Jiangsu Acad Agr Sci, Inst Agr Resources & Environm, Nanjing 210014, Jiangsu, Peoples R China
[3] Hebei Acad Agr & Forestry Sci, Inst Agroresource & Environm, Shijiazhuang 050051, Hebei, Peoples R China
[4] Rothamsted Res North Wyke, Dept Sustainable Soils & Grassland Syst, Okehampton EX20 2SB, Devon, England
[5] Scotlands Rural Coll, Edinburgh EH9 3JG, Midlothian, Scotland
[6] Bangor Univ, Sch Environm Nat Resources & Geog, Bangor LL57 2UW, Gwynedd, Wales
基金
英国生物技术与生命科学研究理事会;
关键词
Nitrous oxide; N-15; tracing; Straw incorporation; Nitrogen fertilization; Intensive farming; NITROUS-OXIDE EMISSIONS; GREENHOUSE-GAS EMISSIONS; SOIL ORGANIC-CARBON; NITRIFICATION INHIBITOR; FARMING PRACTICES; USE EFFICIENCY; NITRIC-OXIDE; CHINA PLAIN; WHEAT; MAIZE;
D O I
10.1016/j.geoderma.2019.01.014
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Nitrogen (N) fertilization and straw incorporation strongly influence nitrous oxide (N2O) emissions from agricultural fields. An in-situ micro-plot experiment on intensively farmed winter wheat (Triticum aestivum L.) was conducted to investigate the source and rate of N2O emissions from soils following labeled N-15 fertilization with and without straw incorporation. Four treatments, i.e., no N fertilizer and no straw incorporation (N0S0), straw incorporation only (N0S1), N fertilizer only (N1S0), and N fertilization plus straw incorporation (N1S1), were established in the experiment. The N2O emissions mainly occurred after N fertilization and lasted for approximately 1-2 weeks, accounting for 60%-67% of the wheat seasonal N2O emissions. Within the 6 days after basal fertilization and 2-4 days after top-dressing, most of the N2O fluxes (> 50%) were derived from fertilizer. Thereafter, soil-derived N2O dominated the total N2O emissions and within 10-20 days after N fertilization, fertilizer-derived N2O became negligible. Fertilizer N and soil N both accounted for 40%-60% of the seasonal N2O emissions, which may be explained by the high soil N stock due to long-term high N fertilization in the region. This implies the similar roles of soil N pool and fertilizer N in N2O generation under intensively farmed soils. The N fertilization had a significant priming effect on the turnover of soil N, which contributed 21.02%-50.47% of the total N2O emissions. During the basal fertilization/first irrigation event, straw incorporation significantly (P < 0.05) stimulated CO2 fluxes both in N-fertilized and non-N-fertilized plots; however, after the top-dressing/second irrigation event, the significant increase of CO2 fluxes induced by straw incorporation was only observed in the N-fertilized treatment. Straw incorporation interacted with N fertilization, and tended to enhance N2O emissions in the basal fertilization and lower N2O emissions in the top-dressing period. In N-fertilized plots, the seasonal N2O emissions from straw-incorporated and straw-removed treatments were similar, indicating that straw incorporation enhanced the N supply without increasing the N2O emissions. Our study highlights that there are significant benefits of straw incorporation to soil fertility improvement; however, the long-term impacts of straw incorporation on greenhouse gas emissions should be further examined.
引用
收藏
页码:129 / 137
页数:9
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