Journal article

Spatial-temporal patterns of foliar and bulk soil 15N isotopic signatures across a heterogeneous landscape: Linkages to soil N status, nitrate leaching, and N2O fluxes


Authors listWangari, Elizabeth Gachibu; Mwanake, Ricky Mwangada; Houska, Tobias; Kraus, David; Kikowatz, Hanna-Marie; Wolf, Benjamin; Gettel, Gretchen M.; Breuer, Lutz; Ambus, Per; Kiese, Ralf; Butterbach-Bahl, Klaus

Publication year2024

JournalSoil Biology and Biochemistry

Volume number199

ISSN0038-0717

eISSN1879-3428

DOI Linkhttps://doi.org/10.1016/j.soilbio.2024.109609

PublisherElsevier


Abstract
The natural abundance of plant and bulk soil N-15 isotopic signatures provides valuable insights into the magnitude of nitrogen cycling and loss processes within terrestrial ecosystems. However, N-15 isotopic signatures are highly variable in space due to natural and anthropogenic factors affecting N cycling processes and losses. To date, most studies on foliar and bulk soil N-15 isotopic signatures have focused on N-limited forest ecosystems at relatively large spatial scales, while similar studies in N-enriched ecosystems at finer spatial scales are lacking. To address this gap and evaluate links between soil N-15 isotopic signatures and ecosystem N cycling and loss processes (plant N uptake, N leaching, and gaseous loss), this study quantified foliar and bulk soil N-15 isotopic signatures, soil physicochemical parameters, gaseous (N2O), and hydrological (NO3) N losses at 80 sites distributed across a heterogeneous landscape (similar to 5.8 km(2)). To account for the spatial-temporal heterogeneity, the measurements were performed in four campaigns (March, June, September 2022, and March 2023) at sites that considered different land uses, soil types, and topography. Results indicated that foliar and bulk soil N-15 isotopic signatures were significantly (P < 0.05) more enriched in arable and grassland ecosystems than forests, suggesting a more open N cycle with significant N cycling and losses due to higher N inputs from fertilizers. Similar to soil inorganic N, N2O fluxes, and NO3 leaching rates, landscape-scale foliar and soil N-15 isotopic signatures varied widely spatially, particularly at grassland and arable land (-3 to 9.0 parts per thousand), with bivariate and multivariate analyses also showing significant relationships between landscape-scale soil N-15 isotopic signatures and the aforementioned parameters (r(2): 0.29 to 0.82). Based on these relationships, our findings suggested that foliar and bulk N-15 isotopic signatures may capture fine-scale areas with persistently high and low environmental N losses (N2O fluxes and NO3 leaching) within a heterogeneous landscape.



Authors/Editors




Citation Styles

Harvard Citation styleWangari, E., Mwanake, R., Houska, T., Kraus, D., Kikowatz, H., Wolf, B., et al. (2024) Spatial-temporal patterns of foliar and bulk soil 15N isotopic signatures across a heterogeneous landscape: Linkages to soil N status, nitrate leaching, and N2O fluxes, Soil Biology and Biochemistry, 199, Article 109609. https://doi.org/10.1016/j.soilbio.2024.109609

APA Citation styleWangari, E., Mwanake, R., Houska, T., Kraus, D., Kikowatz, H., Wolf, B., Gettel, G., Breuer, L., Ambus, P., Kiese, R., & Butterbach-Bahl, K. (2024). Spatial-temporal patterns of foliar and bulk soil 15N isotopic signatures across a heterogeneous landscape: Linkages to soil N status, nitrate leaching, and N2O fluxes. Soil Biology and Biochemistry. 199, Article 109609. https://doi.org/10.1016/j.soilbio.2024.109609


Last updated on 2025-21-05 at 17:55