Microbial controls of nitrogen retention and N2O production in cropping systems supporting soil carbon accrual

The fate of nitrate is central for increasing nitrogen use efficiency in cropping systems. It is influenced by ammonifiers and denitrifiers, two microbial guilds that compete for nitrate and contribute to nitrogen retention and loss, respectively, with the latter in the form of dinitrogen gas and the greenhouse gas nitrous oxide (N 2 O). We hypothesized that cropping systems causing higher soil carbon:nitrate favor ammonifiers and thereby lower N 2 O emissions and improve crop yield. We sampled long-term field experiments comparing annual cereal, w/wo straw return, and ley rotations under four fertilization regimes replicated in three pedoclimatic zones in Sweden. Soil carbon content has decreased in the cereal rotations since the establishment of the experiments, whereas positive effects of leys on soil carbon varied depending on clay content. Nevertheless, the ley rotations displayed consistently lower nitrate levels irrespective of fertilization regime, lower N 2 O production rates, and similar or higher cereal yields compared to cereal cropping. Sequencing of 16S rRNA genes showed major differences in the soil microbiome between ley and cereal rotations, with some effects of fertilization. To tease apart effects on the functional guilds, we quantified the genetic potential of ammonifying ( nrfA ), denitrifying ( nirK , nirS ) and N 2 O reducing ( nosZ I and nosZ II) microbial communities. Nitrate availability rather than carbon content explained the apparent control of carbon:nitrate on ammonifiers vs denitrifiers, with lower levels favoring the former. Altogether, our findings highlight the importance of integrating carbon and nitrogen management strategies to improve soil carbon content while also reducing N 2 O emissions from cropping systems. • Leys in rotations has a positive effect on the long-term trajectory of soil carbon content and cereal yields compared to cereal rotations with or without straw return • Nitrate availability rather than soil carbon content controls the competition between ammonifiers and denitrifiers, even in low carbon soils (< 2 %) • Higher soil carbon is not always associated with increased nitrous oxide emissions • Fertilization reduces microbial controls of nitrous oxide emissions

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Publication Details

Journal
Soil Biology and Biochemistry
Published
2025-05-19
DOI
https://doi.org/10.1016/j.soilbio.2025.109858
Citations
3
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
Field-Weighted Citation Impact
3.56
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article

Microbial controls of nitrogen retention and N2O production in cropping systems supporting soil carbon accrual

Sara Hallin, Christopher M. Jones, Aurélien Saghaï, Oliver C. Moore
3 citations
Soil Biology and Biochemistry
Soil Carbon and Nitrogen Dynamics
3.56
article

Microbial controls of nitrogen retention and N2O production in cropping systems supporting soil carbon accrual

Sara Hallin, Christopher M. Jones, Aurélien Saghaï, Oliver C. Moore
article en
3 citations

Abstract

The fate of nitrate is central for increasing nitrogen use efficiency in cropping systems. It is influenced by ammonifiers and denitrifiers, two microbial guilds that compete for nitrate and contribute to nitrogen retention and loss, respectively, with the latter in the form of dinitrogen gas and the greenhouse gas nitrous oxide (N 2 O). We hypothesized that cropping systems causing higher soil carbon:nitrate favor ammonifiers and thereby lower N 2 O emissions and improve crop yield. We sampled long-term field experiments comparing annual cereal, w/wo straw return, and ley rotations under four fertilization regimes replicated in three pedoclimatic zones in Sweden. Soil carbon content has decreased in the cereal rotations since the establishment of the experiments, whereas positive effects of leys on soil carbon varied depending on clay content. Nevertheless, the ley rotations displayed consistently lower nitrate levels irrespective of fertilization regime, lower N 2 O production rates, and similar or higher cereal yields compared to cereal cropping. Sequencing of 16S rRNA genes showed major differences in the soil microbiome between ley and cereal rotations, with some effects of fertilization. To tease apart effects on the functional guilds, we quantified the genetic potential of ammonifying ( nrfA ), denitrifying ( nirK , nirS ) and N 2 O reducing ( nosZ I and nosZ II) microbial communities. Nitrate availability rather than carbon content explained the apparent control of carbon:nitrate on ammonifiers vs denitrifiers, with lower levels favoring the former. Altogether, our findings highlight the importance of integrating carbon and nitrogen management strategies to improve soil carbon content while also reducing N 2 O emissions from cropping systems. • Leys in rotations has a positive effect on the long-term trajectory of soil carbon content and cereal yields compared to cereal rotations with or without straw return • Nitrate availability rather than soil carbon content controls the competition between ammonifiers and denitrifiers, even in low carbon soils (< 2 %) • Higher soil carbon is not always associated with increased nitrous oxide emissions • Fertilization reduces microbial controls of nitrous oxide emissions

Soil Biology and BiochemistryVol. 208
Swedish University of Agricultural Sciences (SE)
Zero hunger
Openalex Percentile: Top 8%
Soil Carbon and Nitrogen Dynamics
3.56
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