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1000 Titel
  • Soil gross N2O emission and uptake under two contrasting agroforestry systems: riparian tree buffer versus alley-cropping tree row
1000 Autor/in
  1. Luo, Jie |
  2. Beule, Lukas |
  3. Shao, Guodong |
  4. NIU, DAN |
  5. Veldkamp, Edzo |
  6. Corre, Marife D. |
1000 Verlag
  • Springer International Publishing
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-05-16
1000 Erschienen in
1000 Quellenangabe
  • 167(6):871-888
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1007/s10533-024-01141-3 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:title>Abstract</jats:title><jats:p>In addition to the removal of excess mineral nitrogen (N) via root uptake, trees in agroforestry systems may mitigate negative effects of high N fertilization of adjacent crops by enhancing complete denitrification of excess mineral N aside from root uptake. Presently, little is known about the potential for NO<jats:sub>3</jats:sub><jats:sup>−</jats:sup> reduction through denitrification (conversion to greenhouse gas N<jats:sub>2</jats:sub>O and subsequently to non-reactive N<jats:sub>2</jats:sub>) in contrasting agroforestry systems: riparian tree buffer versus tree row of an upland alley-cropping system. Our study aimed to (1) quantify gross N<jats:sub>2</jats:sub>O emissions (both N<jats:sub>2</jats:sub>O + N<jats:sub>2</jats:sub> emissions) and gross N<jats:sub>2</jats:sub>O uptake (N<jats:sub>2</jats:sub>O reduction to N<jats:sub>2</jats:sub>), and (2) determine their controlling factors. We employed the <jats:sup>15</jats:sup>N<jats:sub>2</jats:sub>O pool dilution technique to quantify gross N<jats:sub>2</jats:sub>O fluxes from 0 to 5 cm (topsoil) and 40 to 60 cm (subsoil) depths with seasonal field measurements in 2019. The riparian tree buffer exhibited higher topsoil gross N<jats:sub>2</jats:sub>O emissions and uptake than the alley-cropping tree row (<jats:italic>P</jats:italic> &lt; 0.03). Gross N<jats:sub>2</jats:sub>O emissions were regulated by N and carbon (C) availabilities and aeration status rather than denitrification gene abundance. Gross N<jats:sub>2</jats:sub>O uptake was directly linked to available C and <jats:italic>nirK</jats:italic> gene abundance. In the subsoil, gross N<jats:sub>2</jats:sub>O emission and uptake were low in both agroforestry systems, resulting from low mineral N contents possibly due to N uptake by deep tree roots. Nonetheless, the larger available C and soil moisture in the subsoil of riparian tree buffer than in alley-cropping tree row (<jats:italic>P</jats:italic> &lt; 0.05) suggest its large potential for N<jats:sub>2</jats:sub>O uptake whenever NO<jats:sub>3</jats:sub><jats:sup>−</jats:sup> is transported to the subsoil.</jats:p>
1000 Sacherschließung
lokal Agroforestry
lokal Alley cropping
lokal Riparian buffer
lokal Article
lokal Gross N
1000 Fächerklassifikation (DDC)
1000 Liste der Beteiligten
  1. https://orcid.org/0000-0001-8453-8585|https://orcid.org/0000-0003-1107-7540|https://orcid.org/0000-0001-7122-1319|https://orcid.org/0000-0002-2268-9035|https://orcid.org/0000-0002-8318-8349|https://orcid.org/0000-0003-0359-2104
1000 Hinweis
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1000 Label
1000 Förderer
  1. Bundesministerium für Bildung und Forschung |
  2. BonaRes |
  3. China Scholarship Council |
  4. Georg-August-Universität Göttingen |
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1000 Dateien
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    1000 Förderer Georg-August-Universität Göttingen |
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