Abstract

Nitrification inhibitors (NIs) are useful tools to reduce nitrogen (N) losses derived from fertilization in agriculture. However, it remains unclear whether a future climate scenario with elevated CO2 could affect NIs efficiency. Thus, the objective of this work was to study whether the increase of atmospheric CO2 concentration would affect the efficiency of two dimethylpyrazole-based NIs: 3,4-dimethylpyrazol phosphate (DMPP) and 3,4-dimethylpyrazol succinic acid (DMPSA) in a plant-soil microcosm. To do so, Hordeum vulgare var. Henley plants were grown in soil fertilized with ammonium sulphate (AS) with or without NIs under controlled environmental conditions at ambient CO2 (aCO2) or elevated CO2 (eCO2; 700 ppm). In the soil, mineral nitrogen and N2O emission evolution were monitored together with nitrifying and denitrifying population that were quantified by qPCR. In the plant, biomass, total amino acid content and isotopic discrimination of N and C were measured. Both NIs showed greater efficiency to maintain soil NH4+ content under eCO2 compared to aCO2, as a consequence of 80% reduction of AOB abundance in eCO2. Indeed, both inhibitors were able to lessen 53% the N2O emissions in eCO2 compared to aCO2. Regarding the plant, DMPP and DMPSA negatively affected plant biomass at aCO2 but this effect was restored at eCO2 due to a better ammonium tolerance associated with an increase in total amino acid content. Overall, DMPP and DMPSA NIs were highly efficient under eCO2, reducing N2O emissions and keeping N in the soil stable for longer while maintaining plant biomass production.

Highlights

  • Atmospheric CO2 concentration will presumably rise to 450 ppm by 2030 and between 750 and 1300 ppm by 2100 (IPPC, 2014), which could produce different effects in the soil–plant system

  • At ambient CO2 (aCO2), plant biomass was reduced by 37% in presence of dimethylpyrazol phosphate (DMPP) and DMPSA compared to ammonium sulphate (AS) treatment

  • Amino acid content was always higher in AS + DMPP (AS+DP) and AS + DMPSA (AS+DS) respect to plants grown in AS (Fig. 1C)

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Summary

Introduction

Atmospheric CO2 concentration will presumably rise to 450 ppm by 2030 and between 750 and 1300 ppm by 2100 (IPPC, 2014), which could produce different effects in the soil–plant system. Be­ sides, eCO2 can stimulate the productivity of C3 species (Ainsworth and Long, 2005; Shimono et al, 2019) by increasing photosynthesis (Song et al, 2020), changing plant physiology and metabolism (McGrath and Lobell, 2013; Jauregui et al, 2015) and decreasing plant stomatal conductance improving water use efficiency (Dieleman et al, 2012). This decrease in stomatal conductance has been associated with the root capacity to vary the absorption and assimilation of different nitrogen (N) sources (Torralbo et al, 2019).

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