Management impacts on nitrous oxide emissions and nitrogen cycling gene abundances in an Okanagan Valley sweet cherry (Prunus avium) orchard soil

Agricultural soil management contributes to nitrous oxide (N₂O) emissions. The use of organic and inorganic amendments, and nitrification inhibitors can influence N₂O production by altering microbial nitrogen–cycling functional genes and metabolism. This thesis includes one in–field study and two microcosm studies aimed at identifying best management practices based on the impacts of organic amendments, nitrogen source, and the nitrification inhibitor 3,4–dimethylpyrazole phosphate (DMPP) on N₂O emissions, physicochemical properties, and abundances for total bacteria, archaea, and six nitrogen–cycling genes in a sweet cherry orchard soil in the Okanagan. Field plot treatments were bare, compost (CMP), and woodchip (WC); soil and gas sampling occurred in June and August (2020). The I1 and I2 microcosms contained soil from the field site and were incubated for 33 to 38 days. I1 had seven treatments varying NH₄⁺ (A), NO₃⁻ (N), and DMPP (I), and I2 had five treatments varying NH₄⁺, compost (C), and DMPP (I). Compost–treated field plots produced more N₂O, had a higher percent carbon and nitrogen, and lower CN ratio than WC plots. The higher CN ratio and proportion of insoluble carbon in WC plots likely increased nitrogen use efficiency and assimilation, and decreased denitrification–N₂O. In the I1 experiment the ANI treatment produced the most N₂O-N, while the uninhibited/inhibited pairs were comparable (A≈AI, N≈NI). Closed microcosms may have encouraged low oxygen, excess NH₄⁺ and NO₂⁻/NO₃⁻ in ANI, and, with low cation exchange capacity (CEC), may have facilitated co-denitrification and abiotic–N₂O production. In the I2 experiment, compost increased the N₂O-N produced in the presence of DMPP (ACI>AI), but N₂O-N was comparable between the uninhibited/inhibited pairs (A≈AI, AC≈ACI). The inhibitor DMPP may be ineffective if NO₃⁻ is available from sources besides nitrification (ACI/AI). Adding compost increased CEC and carbon, aiding NH₄⁺ adsorption and potentially assimilation, preventing drastically elevated N₂O-N compared to NH₄⁺ alone (AC≈A). In conclusion, high-CN organic matter with more insoluble carbon may reduce fertilizer and irrigation–induced N₂O in–field but DMPP needs in–field testing in the Okanagan with different soil types and management practices to identify ideal application rates and methods.

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Publication Details

Journal
Open Collections
Published
2026-01-01
DOI
https://doi.org/10.14288/1.0451098
Primary Topic
Soil Carbon and Nitrogen Dynamics
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article
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article

Management impacts on nitrous oxide emissions and nitrogen cycling gene abundances in an Okanagan Valley sweet cherry (Prunus avium) orchard soil

Katherine-Faye Karen Jansen
Open Collections
Soil Carbon and Nitrogen Dynamics
article

Management impacts on nitrous oxide emissions and nitrogen cycling gene abundances in an Okanagan Valley sweet cherry (Prunus avium) orchard soil

Katherine-Faye Karen Jansen
article en

Abstract

Agricultural soil management contributes to nitrous oxide (N₂O) emissions. The use of organic and inorganic amendments, and nitrification inhibitors can influence N₂O production by altering microbial nitrogen–cycling functional genes and metabolism. This thesis includes one in–field study and two microcosm studies aimed at identifying best management practices based on the impacts of organic amendments, nitrogen source, and the nitrification inhibitor 3,4–dimethylpyrazole phosphate (DMPP) on N₂O emissions, physicochemical properties, and abundances for total bacteria, archaea, and six nitrogen–cycling genes in a sweet cherry orchard soil in the Okanagan. Field plot treatments were bare, compost (CMP), and woodchip (WC); soil and gas sampling occurred in June and August (2020). The I1 and I2 microcosms contained soil from the field site and were incubated for 33 to 38 days. I1 had seven treatments varying NH₄⁺ (A), NO₃⁻ (N), and DMPP (I), and I2 had five treatments varying NH₄⁺, compost (C), and DMPP (I). Compost–treated field plots produced more N₂O, had a higher percent carbon and nitrogen, and lower CN ratio than WC plots. The higher CN ratio and proportion of insoluble carbon in WC plots likely increased nitrogen use efficiency and assimilation, and decreased denitrification–N₂O. In the I1 experiment the ANI treatment produced the most N₂O-N, while the uninhibited/inhibited pairs were comparable (A≈AI, N≈NI). Closed microcosms may have encouraged low oxygen, excess NH₄⁺ and NO₂⁻/NO₃⁻ in ANI, and, with low cation exchange capacity (CEC), may have facilitated co-denitrification and abiotic–N₂O production. In the I2 experiment, compost increased the N₂O-N produced in the presence of DMPP (ACI>AI), but N₂O-N was comparable between the uninhibited/inhibited pairs (A≈AI, AC≈ACI). The inhibitor DMPP may be ineffective if NO₃⁻ is available from sources besides nitrification (ACI/AI). Adding compost increased CEC and carbon, aiding NH₄⁺ adsorption and potentially assimilation, preventing drastically elevated N₂O-N compared to NH₄⁺ alone (AC≈A). In conclusion, high-CN organic matter with more insoluble carbon may reduce fertilizer and irrigation–induced N₂O in–field but DMPP needs in–field testing in the Okanagan with different soil types and management practices to identify ideal application rates and methods.

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Soil Carbon and Nitrogen Dynamics
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Management impacts on nitrous oxide emissions and nitrogen cycling gene abundances in an Okanagan Valley sweet cherry (Prunus avium) orchard soil — Katherine-Faye Karen Jansen · Open Collections (2026) | TGRS Research Map | TGRS