Intensive slurry management and climate change promote nitrogen mining from organic matter-rich montane grassland soils. Schlingmann, M., Tobler, U., Berauer, B., Garcia-Franco, N., Wilfahrt, P., Wiesmeier, M., Jentsch, A., Wolf, B., Kiese, R., & Dannenmann, M. Plant and Soil, 456(1-2):81–98, November, 2020.
Intensive slurry management and climate change promote nitrogen mining from organic matter-rich montane grassland soils [link]Paper  doi  abstract   bibtex   
Abstract Aims Consequences of climate change and land use intensification on the nitrogen (N) cycle of organic-matter rich grassland soils in the alpine region remain poorly understood. We aimed to identify fates of fertilizer N and to determine the overall N balance of an organic-matter rich grassland in the European alpine region as influenced by intensified management and warming. Methods We combined 15 N cattle slurry labelling with a space for time climate change experiment, which was based on translocation of intact plant-soil mesocosms down an elevational gradient to induce warming of +1 °C and + 3 °C. Mesocosms were subject to either extensive or intensive management. The fate of slurry-N was traced in the plant-soil system. Results Grassland productivity was very high (8.2 t - 19.4 t dm ha −1  yr −1 ), recovery of slurry 15 N in mowed plant biomass was, however, low (9.6–14.7%), illustrating low fertilizer N use efficiency and high supply of plant available N via mineralization of soil organic matter (SOM). Higher 15 N recovery rates (20.2–31.8%) were found in the soil N pool, dominated by recovery in unextractable N. Total 15 N recovery was approximately half of the applied tracer, indicating substantial loss to the environment. Overall, high N export by harvest (107–360 kg N ha −1  yr −1 ) markedly exceeded N inputs, leading to a negative grassland N balance. Conclusions Here provided results suggests a risk of soil N mining in montane grasslands, which increases both under climate change and land use intensification.
@article{schlingmann_intensive_2020,
	title = {Intensive slurry management and climate change promote nitrogen mining from organic matter-rich montane grassland soils},
	volume = {456},
	issn = {0032-079X, 1573-5036},
	url = {https://link.springer.com/10.1007/s11104-020-04697-9},
	doi = {10.1007/s11104-020-04697-9},
	abstract = {Abstract 
             
              Aims 
              Consequences of climate change and land use intensification on the nitrogen (N) cycle of organic-matter rich grassland soils in the alpine region remain poorly understood. We aimed to identify fates of fertilizer N and to determine the overall N balance of an organic-matter rich grassland in the European alpine region as influenced by intensified management and warming. 
             
             
              Methods 
               
                We combined 
                15 
                N cattle slurry labelling with a space for time climate change experiment, which was based on translocation of intact plant-soil mesocosms down an elevational gradient to induce warming of +1 °C and + 3 °C. Mesocosms were subject to either extensive or intensive management. The fate of slurry-N was traced in the plant-soil system. 
               
             
             
              Results 
               
                Grassland productivity was very high (8.2 t - 19.4 t dm ha 
                −1 
                 yr 
                −1 
                ), recovery of slurry 
                15 
                N in mowed plant biomass was, however, low (9.6–14.7\%), illustrating low fertilizer N use efficiency and high supply of plant available N via mineralization of soil organic matter (SOM). Higher 
                15 
                N recovery rates (20.2–31.8\%) were found in the soil N pool, dominated by recovery in unextractable N. Total 
                15 
                N recovery was approximately half of the applied tracer, indicating substantial loss to the environment. Overall, high N export by harvest (107–360 kg N ha 
                −1 
                 yr 
                −1 
                ) markedly exceeded N inputs, leading to a negative grassland N balance. 
               
             
             
              Conclusions 
              Here provided results suggests a risk of soil N mining in montane grasslands, which increases both under climate change and land use intensification.},
	language = {en},
	number = {1-2},
	urldate = {2022-11-02},
	journal = {Plant and Soil},
	author = {Schlingmann, Marcus and Tobler, Ursina and Berauer, Bernd and Garcia-Franco, Noelia and Wilfahrt, Peter and Wiesmeier, Martin and Jentsch, Anke and Wolf, Benjamin and Kiese, Ralf and Dannenmann, Michael},
	month = nov,
	year = {2020},
	pages = {81--98},
}

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