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Source partitioning using N 2 O isotopomers and soil WFPS to establish dominant N 2 O production pathways from different pasture sward compositions.

Authors :
Bracken CJ
Lanigan GJ
Richards KG
Müller C
Tracy SR
Grant J
Krol DJ
Sheridan H
Lynch MB
Grace C
Fritch R
Murphy PNC
Source :
The Science of the total environment [Sci Total Environ] 2021 Aug 10; Vol. 781, pp. 146515. Date of Electronic Publication: 2021 Mar 17.
Publication Year :
2021

Abstract

Nitrous oxide (N <subscript>2</subscript> O) 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 N <subscript>2</subscript> O 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 N <subscript>2</subscript> O fluxes and associated isotopomers from eight experimental plots (7.8 m <superscript>2</superscript> ) post a urea-N fertiliser application (40 kg N ha <superscript>-1</superscript> ). 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. N <subscript>2</subscript> O 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 = δ <superscript>15</superscript> N <superscript>α</superscript> - δ <superscript>15</superscript> N <superscript>β</superscript> ) and δ <superscript>15</superscript> N <superscript>bulk</superscript> ((δ <superscript>15</superscript> N <superscript>α</superscript> + δ <superscript>15</superscript> N <superscript>β</superscript> ) / 2) values were used to attribute N <subscript>2</subscript> O production to nitrification, denitrification or a mixture of both nitrification and denitrification over a range of soil WFPS (%). Daily N <subscript>2</subscript> O fluxes ranged from 8.26 to 86.86 g N <subscript>2</subscript> O-N ha <superscript>-1</superscript> d <superscript>-1</superscript> . Overall, 34.2% of daily N <subscript>2</subscript> O 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 δ <superscript>15</superscript> N <superscript>bulk</superscript> indicated that the inclusion of ribwort plantain may decrease N <subscript>2</subscript> O 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 N <subscript>2</subscript> O 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 N <subscript>2</subscript> O mitigation strategies.<br />Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.<br /> (Copyright © 2021 The Authors. Published by Elsevier B.V. All rights reserved.)

Details

Language :
English
ISSN :
1879-1026
Volume :
781
Database :
MEDLINE
Journal :
The Science of the total environment
Publication Type :
Academic Journal
Accession number :
33812119
Full Text :
https://doi.org/10.1016/j.scitotenv.2021.146515