Source partitioning using N2O isotopomers and soil WFPS to establish dominant N2O production pathways from different pasture sward compositions

被引:0
|
作者
Bracken, Conor J. [1 ,2 ,3 ]
Lanigan, Gary J. [3 ]
Richards, Karl G. [3 ]
Müller, Christoph [2 ,4 ,5 ]
Tracy, Saoirse R. [1 ,2 ]
Grant, James [6 ]
Krol, Dominika J. [3 ]
Sheridan, Helen [1 ,7 ]
Lynch, Mary Bridget [1 ,7 ]
Grace, Cornelia [1 ,7 ]
Fritch, Rochelle [1 ,7 ]
Murphy, Paul N.C. [1 ,2 ]
机构
[1] UCD School of Agriculture and Food Science, University College Dublin, Belfield, Dublin 4, Ireland
[2] UCD Earth Institute, University College Dublin, Belfield, Dublin 4, Ireland
[3] Teagasc, Environmental Research Center, Johnstown Castle, Wexford, Ireland
[4] Institute of Plant Ecology, Justus-Liebig University, Heinrich-Buff-Ring 26, Giessen,35392, Germany
[5] UCD School of Biology and Environmental Science, University College Dublin, Belfield, Dublin 4, Ireland
[6] Teagasc Food Research Center Ashtown, Dublin 15, Ireland
[7] UCD Lyons Farm, Lyons Estate, Celbridge, Naas, Co. Kildare, Ireland
关键词
$+15$/N - Isotopomers - N fertilizers - N$-2$/O - Nitrous oxide - Perennial ryegrass (lolium perenne) - Ribwort plantain (plantago lanceolata) - Site preferences - Soil WFPS - White clover (trifolium repen);
D O I
暂无
中图分类号
学科分类号
摘要
Nitrous oxide (N2O) is a potent greenhouse gas (GHG) emitted from agricultural soils and is influenced by nitrogen (N) fertiliser management and weather and soil conditions. Source partitioning N2O emissions related to management practices and soil conditions could suggest effective mitigation strategies. Multispecies swards can maintain herbage yields at reduced N fertiliser rates compared to grass monocultures and may reduce N losses to the wider environment. A restricted-simplex centroid experiment was used to measure daily N2O fluxes and associated isotopomers from eight experimental plots (7.8 m2) post a urea-N fertiliser application (40 kg N ha−1). Experimental pastures consisted of differing proportions of grass, legume and forage herb represented by perennial ryegrass (Lolium perenne), white clover (Trifolium repens) and ribwort plantain (Plantago lanceolata), respectively. N2O isotopomers were measured using a cavity ring down spectroscopy (CRDS) instrument adapted with a small sample isotope module (SSIM) for the analysis of gas samples ≤20 mL. Site preference (SP = δ15Nα – δ15Nβ) and δ15Nbulk ((δ15Nα + δ15Nβ) / 2) values were used to attribute N2O production to nitrification, denitrification or a mixture of both nitrification and denitrification over a range of soil WFPS (%). Daily N2O fluxes ranged from 8.26 to 86.86 g N2O-N ha−1 d−1. Overall, 34.2% of daily N2O fluxes were attributed to nitrification, 29.0% to denitrification and 36.8% to a mixture of both. A significant diversity effect of white clover and ribwort plantain on predicted SP and δ15Nbulk indicated that the inclusion of ribwort plantain may decrease N2O emission through biological nitrification inhibition under drier soil conditions (31%–75% WFPS). Likewise, a sharp decline in predicted SP indicates that increased white clover content could increase N2O emissions associated with denitrification under elevated soil moisture conditions (43%–77% WFPS). Biological nitrification inhibition from ribwort plantain inclusion in grassland swards and management of N fertiliser source and application timing to match soil moisture conditions could be useful N2O mitigation strategies. © 2021
引用
收藏
相关论文
共 50 条
  • [21] Microbial pathways account for the pH effect on soil N2O production
    Zhang, Yi
    Zhao, Jun
    Huang, Xinqi
    Cheng, Yi
    Cai, Zucong
    Zhang, Jinbo
    Mueller, Christoph
    EUROPEAN JOURNAL OF SOIL BIOLOGY, 2021, 106
  • [22] Soil N2O fluxes in integrated production systems, continuous pasture and Cerrado
    de Carvalho, Arminda Moreira
    Duarte de Oliveira, Willian Roberson
    Gerosa Ramos, Maria Lucrecia
    Coser, Thais Rodrigues
    de Oliveira, Alexsandra Duarte
    Pulrolnik, Karina
    Souza, Kleberson Worslley
    Vilela, Lourival
    Marchao, Robelio Leandro
    NUTRIENT CYCLING IN AGROECOSYSTEMS, 2017, 108 (01) : 69 - 83
  • [23] Photodissociation of N2O: Energy partitioning
    Schmidt, J. A.
    Johnson, M. S.
    Lorenz, U.
    McBane, G. C.
    Schinke, R.
    JOURNAL OF CHEMICAL PHYSICS, 2011, 135 (02):
  • [24] Microbial N2O consumption in and above marine N2O production hotspots
    Sun, Xin
    Jayakumar, Amal
    Tracey, John C.
    Wallace, Elizabeth
    Kelly, Colette L.
    Casciotti, Karen L.
    Ward, Bess B.
    ISME JOURNAL, 2021, 15 (05): : 1434 - 1444
  • [25] Microbial N2O consumption in and above marine N2O production hotspots
    Xin Sun
    Amal Jayakumar
    John C. Tracey
    Elizabeth Wallace
    Colette L. Kelly
    Karen L. Casciotti
    Bess B. Ward
    The ISME Journal, 2021, 15 : 1434 - 1444
  • [26] Inoculation with nitrous oxide (N2O)-reducing denitrifier strains simultaneously mitigates N2O emission from pasture soil and promotes growth of pasture plants
    Gao, Nan
    Shen, Weishou
    Kakuta, Hiroko
    Tanaka, Nobuhiro
    Fujiwara, Toru
    Nishizawa, Tomoyasu
    Takaya, Noriko
    Nagamine, Tadashi
    Isobe, Kazuo
    Otsuka, Shigeto
    Senoo, Keishi
    SOIL BIOLOGY & BIOCHEMISTRY, 2016, 97 : 83 - 91
  • [27] A Study on the N2O Separation Process from Crude N2O
    Cho, Jungho
    Lee, Taekhong
    Park, Jongki
    KOREAN CHEMICAL ENGINEERING RESEARCH, 2005, 43 (04): : 467 - 473
  • [28] N2O production by heterotrophic N transformations in a semiarid soil
    McLain, Jean E. T.
    Martens, Dean A.
    APPLIED SOIL ECOLOGY, 2006, 32 (02) : 253 - 263
  • [29] Biochar mitigates the stimulatory effects of straw incorporation on N2O emission and N2O/(N2O + N2) ratio in upland soil
    Li, Chenglin
    Wei, Zhijun
    Wang, Xiaomin
    Ma, Xiaofang
    Tang, Quan
    Zhao, Bingzi
    Shan, Jun
    Yan, Xiaoyuan
    JOURNAL OF ENVIRONMENTAL MANAGEMENT, 2024, 369
  • [30] Drought turns a Central European Norway spruce forest soil from an N2O source to a transient N2O sink
    Goldberg, Stefanie Daniela
    Gebauer, Gerhard
    GLOBAL CHANGE BIOLOGY, 2009, 15 (04) : 850 - 860