The reducing effect of aglime on N₂O and CO₂ emissions balance from an acidic soil: A study on intact soil cores

Abstract

The functioning of the nitrous oxide (N2O) reductase enzyme involved in the last step of denitrification is pH sensitive, with an optimum of 6.8. A solution to mitigate N2O emissions would be to bring soil pH close to neutrality by adding agricultural liming products (aglime). Nevertheless, the influence of aglime on the soil greenhouse gas (GHG) balance (CO2–N2O) is a subject of debate, particularly when considering the fate of the carbon (C) derived from carbonates. Our objective was to investigate the results of the effect of calcium carbonate (CaCO3) aglime on the CO2–N2O balance. Sixteen cylinders of undisturbed acidic soil were taken from a sandy loam profile and incubated at 20°C for 107 days in anaerobic conditions (water‐filled pore space >60%). Eight limed treatment cylinders received 1.45 g of aglime on the soil surface (2 t NV ha−1) and 0.08 g of N (100 kg of N ha−1). Eight control treatment cylinders received only 0.08 g of N. N2O and CO2 fluxes were measured and converted into CO2 equivalents to perform a GHG balance calculation. Furthermore, soil and leachate properties were measured. Aglime application triggered a reduction of N2O emissions, probably due to an increase in soil pH at the beginning of the experiment, which would have led to the N2O reductase activation. High NO3−$$ {{\mathrm{NO}}_3}^{-} $$‐N content in the soil may inhibit the high N2O reduction potential in the limed treatment. CO2 emissions were unexpectedly lower in the limed treatment. Aglime addition did not enhance C mineralisation, which may be explained by the possible stabilisation of soil organic carbon. A significant 11.3% reduction of GHG emissions was observed in the limed treatment. Overall, our results show that a strategy of liming acidic agricultural soil could be implemented for its potential in GHG mitigation. Nevertheless, future in‐depth research is necessary to better understand the fate of the C brought about by aglime.

A review of measurement for quantification of carbon dioxide removal by enhanced weathering in soil

“…It should also be stressed that CDR via EW is embedded in a complex network of organic and inorganic processes between multiple stocks of carbon involving fluxes of several greenhouse gasses, which have temporally variable responses. This complexity applies to agricultural systems in general, including traditional or sustainable land management practices with (no)tilling, fertilizers and AgLime (Golchin et al, 1995;Marland et al, 2003;West and McBride, 2005;Smith et al, 2010;Rousset et al, 2023). A holistic assessment of the CDR impact of EW must therefore account for changes in organic carbon reservoirs and resulting fluxes (Dietzen et al, 2018;Almaraz et al, 2022;Yan et al, 2023;Buss et al, 2024).…”

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“…It should also be stressed that CDR via EW is embedded in a complex network of organic and inorganic processes between multiple stocks of carbon involving fluxes of several greenhouse gasses, which have temporally variable responses. This complexity applies to agricultural systems in general, including traditional or sustainable land management practices with (no)tilling, fertilizers and AgLime (Golchin et al, 1995;Marland et al, 2003;West and McBride, 2005;Smith et al, 2010;Rousset et al, 2023). A holistic assessment of the CDR impact of EW must therefore account for changes in organic carbon reservoirs and resulting fluxes (Dietzen et al, 2018;Almaraz et al, 2022;Yan et al, 2023;Buss et al, 2024).…”