Abstract

AimsConsequences 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.MethodsWe combined 15N 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.ResultsGrassland productivity was very high (8.2 t - 19.4 t dm ha−1 yr−1), recovery of slurry 15N 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 15N recovery rates (20.2–31.8%) were found in the soil N pool, dominated by recovery in unextractable N. Total 15N 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.ConclusionsHere provided results suggests a risk of soil N mining in montane grasslands, which increases both under climate change and land use intensification.

Highlights

  • In the pre-alpine and alpine region of south Germany, grasslands cover over one million hectares (BMLEV2012), and are of similar importance in comparable areas in Austria, Italy and Switzerland

  • We combined 15N 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

  • Here provided results suggests a risk of soil N mining in montane grasslands, which increases both under climate change and land use intensification

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Summary

Introduction

In the pre-alpine and alpine region of south Germany, grasslands cover over one million hectares (BMLEV2012), and are of similar importance in comparable areas in Austria, Italy and Switzerland. The dominant N input to montane grassland systems in the alpine and pre-alpine region is the fertilization with liquid cattle slurry, a N fertilization form which can result in high gaseous losses especially under warming (Zistl-Schlingmann et al 2019). This is of particular importance in the European alpine and pre-alpine region, where climate warming is occurring at twice the rate compared to global average, a trend that is expected to continue or even accelerate in the coming decades (Pepin et al 2015; Smiatek et al 2009; Wagner et al 2013)

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