Nutrient Cycling in Agroecosystems · 2026
No difference in nitrate leaching between digestates and untreated cattle slurry over eight years of organic arable farming
Diener, M., Agostini, L., Bünemann, E. K., Walter, A., Liebisch, F., Mayer, J.
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No difference in nitrate leaching between digestates and unt…
Abstract
Organic fertilizers often contribute to nitrate (NO 3 − ) leaching and impair drinking water quality, because the mineralization of applied organic nitrogen (N) is often asynchronous with crop N uptake. Crop yield, crop N uptake, seepage water and NO 3 − leaching were investigated in a lysimeter facility (Zurich, Switzerland) under temperate climate conditions during two consecutive four-year organically managed crop rotations. The study compared untreated cattle slurry, anaerobically digested slurry, liquid digestate from a non-agricultural biogas plant and a zero-N fertilization control. The ammonium N (NH 4 -N) fraction of the organic fertilizers was labeled with 15 N tracer to investigate the fate of NH 4 -N in the plant-soil–water system. Organic fertilization significantly increased crop yields and N uptake, with no differences among organic fertilizers, despite the higher NH 4 -N proportion of the digestates. Mean annual NO 3 − leaching was low (12–18 kg N ha −1 ) and was not increased by organic fertilization, indicating that N inputs were balanced by crop N uptake. Digestates did not differ from untreated cattle slurry in NO 3 − leaching. Higher modeled ammonia (NH 3 ) emissions of digestates suggest that N losses may occur primarily via NH 3 volatilization rather than NO 3 − leaching. The 15 N recovery showed ~1% of the applied NH 4 -N was lost through NO 3 − leaching, whereas 23–31% was recovered in crops, and 18–23% remained in the topsoil. These results highlight the importance of crop N uptake and the role of the soil as a long-term reservoir for fertilizer-derived N, with direct NO 3 − leaching from the NH 4 -N fraction of organic fertilizers playing only a minor role.
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Organic fertilizers often contribute to nitrate (NO 3 − ) leaching and impair drinking water quality, because the mineralization of applied organic nitrogen (N) is often asynchronous with crop N uptake. Crop yield, crop N uptake, seepage water and NO 3 − leaching were investigated in a lysimeter facility (Zurich, Switzerland) under temperate climate conditions during two consecutive four-year organically managed crop rotations. The study compared untreated cattle slurry, anaerobically digested slurry, liquid digestate from a non-agricultural biogas plant and a zero-N fertilization control. The ammonium N (NH 4 -N) fraction of the organic fertilizers was labeled with 15 N tracer to investigate the fate of NH 4 -N in the plant-soil–water system. Organic fertilization significantly increased crop yields and N uptake, with no differences among organic fertilizers, despite the higher NH 4 -N proportion of the digestates. Mean annual NO 3 − leaching was low (12–18 kg N ha −1 ) and was not increased by organic fertilization, indicating that N inputs were balanced by crop N uptake. Digestates did not differ from untreated cattle slurry in NO 3 − leaching. Higher modeled ammonia (NH 3 ) emissions of digestates suggest that N losses may occur primarily via NH 3 volatilization rather than NO 3 − leaching. The 15 N recovery showed ~1% of the applied NH 4 -N was lost through NO 3 − leaching, whereas 23–31% was recovered in crops, and 18–23% remained in the topsoil. These results highlight the importance of crop N uptake and the role of the soil as a long-term reservoir for fertilizer-derived N, with direct NO 3 − leaching from the NH 4 -N fraction of organic fertilizers playing only a minor role.
Organic fertilizers often contribute to nitrate (NO 3 − ) leaching and impair drinking water quality, because the mineralization of applied organic nitrogen (N) is often asynchronous with crop N uptake. Crop yield, crop N uptake, seepage water and NO 3 − leaching were investigated in a lysimeter facility (Zurich, Switzerland) under temperate climate conditions during two consecutive four-year organically managed crop rotations. The study compared untreated cattle slurry, anaerobically digested slurry, liquid digestate from a non-agricultural biogas plant and a zero-N fertilization control. The ammonium N (NH 4 -N) fraction of the organic fertilizers was labeled with 15 N tracer to investigate the fate of NH 4 -N in the plant-soil–water system. Organic fertilization significantly increased crop yields and N uptake, with no differences among organic fertilizers, despite the higher NH 4 -N proportion of the digestates. Mean annual NO 3 − leaching was low (12–18 kg N ha −1 ) and was not increased by organic fertilization, indicating that N inputs were balanced by crop N uptake. Digestates did not differ from untreated cattle slurry in NO 3 − leaching. Higher modeled ammonia (NH 3 ) emissions of digestates suggest that N losses may occur primarily via NH 3 volatilization rather than NO 3 − leaching. The 15 N recovery showed ~1% of the applied NH 4 -N was lost through NO 3 − leaching, whereas 23–31% was recovered in crops, and 18–23% remained in the topsoil. These results highlight the importance of crop N uptake and the role of the soil as a long-term reservoir for fertilizer-derived N, with direct NO 3 − leaching from the NH 4 -N fraction of organic fertilizers playing only a minor role.
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