17-year in situ 15N tracing reveals turnover and functional roles of residual fertilizer nitrogen in soil organic and fixed ammonium pools of a rice–wheat system

• A 17-year in situ 15 N tracing revealed the decline and transformation of residual N pools. • Over 98% of residual fertilizer N persisted in SON and fixed ammonium forms. • Long-term N fertilization accelerated the turnover of labile organic N and fixed ammonium. • Long-term N input increased crop recovery of residual N by 19 points over 17 years. Intensive nitrogen (N) fertilization has led to the accumulation of residual fertilizer N in agricultural soils, yet its long-term dynamics and functional significance remain inadequately understood. We conducted a 17-year in situ 15 N tracing and N fractionation study in a rice–wheat rotation system, where 15 N-labeled urea was applied in the initial season followed by either continued unlabeled urea applications or no further N input. Over 98 % of residual fertilizer N persisted in slow-release forms, primarily as soil organic nitrogen (SON) and fixed ammonium. Among SON fractions, amino acid N, ammonium N, and hydrolysable unknown N were the main initial sinks, collectively accounting for 85–86 % of total residual N, and functioned as active, fast-cycling pools. In contrast, amino sugar N and acid-insoluble N were less abundant but more stable, with acid-insoluble N exhibiting the slowest turnover. These active SON fractions dominated crop recovery of residual N, contributing 94–95 % of total uptake, with amino acid N alone accounting for 42–46 %. Long-term N fertilization accelerated the mineralization of amino acid N and ammonium N and enhanced fixed ammonium turnover, thereby reshaping soil N pool dynamics, shortening the half-life of residual N, and increasing cumulative crop 15 N recovery by 48 %. These findings provide novel insights into the functional partitioning and turnover of residual N pools, offering important implications for improving nitrogen use efficiency and sustainability in intensive cropping systems.

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Publication Details

Journal
Geoderma
Published
2025-11-25
DOI
https://doi.org/10.1016/j.geoderma.2025.117621
Citations
1
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
Field-Weighted Citation Impact
1.19
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article

17-year in situ 15N tracing reveals turnover and functional roles of residual fertilizer nitrogen in soil organic and fixed ammonium pools of a rice–wheat system

1 citations
Geoderma
Soil Carbon and Nitrogen Dynamics
1.19
article

17-year in situ 15N tracing reveals turnover and functional roles of residual fertilizer nitrogen in soil organic and fixed ammonium pools of a rice–wheat system

article en
1 citations

Abstract

• A 17-year in situ 15 N tracing revealed the decline and transformation of residual N pools. • Over 98% of residual fertilizer N persisted in SON and fixed ammonium forms. • Long-term N fertilization accelerated the turnover of labile organic N and fixed ammonium. • Long-term N input increased crop recovery of residual N by 19 points over 17 years. Intensive nitrogen (N) fertilization has led to the accumulation of residual fertilizer N in agricultural soils, yet its long-term dynamics and functional significance remain inadequately understood. We conducted a 17-year in situ 15 N tracing and N fractionation study in a rice–wheat rotation system, where 15 N-labeled urea was applied in the initial season followed by either continued unlabeled urea applications or no further N input. Over 98 % of residual fertilizer N persisted in slow-release forms, primarily as soil organic nitrogen (SON) and fixed ammonium. Among SON fractions, amino acid N, ammonium N, and hydrolysable unknown N were the main initial sinks, collectively accounting for 85–86 % of total residual N, and functioned as active, fast-cycling pools. In contrast, amino sugar N and acid-insoluble N were less abundant but more stable, with acid-insoluble N exhibiting the slowest turnover. These active SON fractions dominated crop recovery of residual N, contributing 94–95 % of total uptake, with amino acid N alone accounting for 42–46 %. Long-term N fertilization accelerated the mineralization of amino acid N and ammonium N and enhanced fixed ammonium turnover, thereby reshaping soil N pool dynamics, shortening the half-life of residual N, and increasing cumulative crop 15 N recovery by 48 %. These findings provide novel insights into the functional partitioning and turnover of residual N pools, offering important implications for improving nitrogen use efficiency and sustainability in intensive cropping systems.

GeodermaVol. 464
University of Chinese Academy of Sciences (CN), Institute of Soil Science (CN)
Zero hunger
Openalex Percentile: Top 15%
Soil Carbon and Nitrogen Dynamics
1.19
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