Abstract

Nitrogen (N) addition is an important nutrient strategy for alpine grassland in northwestern China to improve productivity for livestock needs. A field experiment was conducted in a semi-arid alpine grassland in northwestern China to investigate the effect of N addition rates on soil N2O emissions over the growing seasons of 2017 and 2018. Treatments included six N addition rates (0, 10, 30, 60, 120, 240 kg N ha−1 y−1), which were applied before each growing season. The N2O fluxes increased with N addition rates and showed different episodic changes between the two growing seasons. In 2017, the maximum N2O flux rate occurred within 2 weeks following N addition. In 2018, however, the maximum N2O flux rate occurred later in the growing season due to a heavy rainfall event. Growing season cumulative N2O emissions ranged between 0.32 and 1.11 kg N ha−1, and increased linearly with N addition rates. Increasing N addition rates over 60 kg N ha−1 yr−1 did not further increase plant above-ground biomass. The inter-annual variability of N2O flux suggests the importance of soil moisture in affecting N2O emissions. It is particularly important to avoid over-applying N nutrients beyond plant needs to reduce its negative effect on the environment while maintaining livestock productivity. The N2O flux rate increased with soil dissolved organic carbon (DOC) and soil pH. These results suggest the optimal N addition rate to the livestock grassland in this region should be 60 kg N ha−1 yr−1.

Highlights

  • Nitrous oxide (N2 O) is one of the most important greenhouse gases (GHGs), with a substantial contribution of 7.9% to the global warming effect [1]

  • This study aimed to find out the optimal N addition rate at which the highest grassland production can be achieved with less N2 O emissions

  • Lower water content and dissolved organic carbon (DOC) can limit the growth and reproduction of nitrification and denitrification bacteria; reducing the production of N2 O [42,43]. These results suggest that applying IPCC default EF will overestimate the N2 O emission for the alpine grassland in semi-arid regions

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Summary

Introduction

Nitrous oxide (N2 O) is one of the most important greenhouse gases (GHGs), with a substantial contribution of 7.9% to the global warming effect [1]. The concentration of atmospheric N2 O has increased from 270 ppb in the preindustrial period to 330 ppb in recent years, mainly due to anthropogenic industrial and agricultural activities. 50% of N2 O emissions are related to the application of soil nitrogen (N) fertilizers to agricultural ecosystems [2,3]. Grassland is one of the most widely distributed vegetation types on the land ecosystem. Grassland has been the largest source of N2 O emissions after forests and cultivated land [7]. Quantification of N2 O emissions from grassland is necessary to assess the N2 O budgets at the regional or global scales [8]. Understanding the mechanism of how N addition affects N2 O emission from alpine grassland is of great importance for developing reasonable nutrient management strategies

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