No abstract

<p>Over the last 80 years, intensive agriculture has had numerous consequences globally. In particular, it has led to a loss of soil organic carbon (SOC) and a decline in soil fertility, resulting in higher nitrogen (N) fertilizer application. Excess of fertilizer has driven the emissions of N<sub>2</sub>O, a greenhouse gas (GHG) 298 times more potent in inducing global warming than CO<sub>2</sub>. Under the UK target of net zero emissions by 2050 and considering the recent increase in fertilizer price, conservation agriculture appears a viable solution to sustain food production whilst reducing global warming. Along with species diversification and reduction (or absence) of tillage, a permanent soil organic cover is the third pillar of conservation agriculture. In particular, “leys” consist in temporary pastures planted in between crops or to restore exhausted soils. These leys are planted with a mix of N fixing plants, which have a unique symbiotic relationship with soil bacteria collectively called “Rhizobia” that transform atmospheric N<sub>2</sub> into organic nitrogen. The mineralization of this organic nitrogen is expected to reduce dependence on N fertilizer. In contrast with the traditional <strong>grass/clover</strong> mix, <strong>herbal leys</strong> have recently gained popularity amongst UK farmers. They consist in a more complex mixture of grasses, legumes and herbs, bringing a range of benefits to forage, livestock health and soil fertility.</p><p>Here we report a year’s worth of measurement of soil mineral N and SOC contents, N mineralization potential, <em>in situ</em> measurement of denitrification (which transforms N fertilizer into N<sub>2</sub>O and N<sub>2</sub>) and total GHG emissions (CO<sub>2</sub>, N<sub>2</sub>O, CH<sub>4</sub>) from a 4-year-old herbal ley in comparison with an arable field. We measured denitrification with our newly developed method (see Micucci et al., 2022) and GHG with conventional GHG chambers. First results show that during the early growing season (April to June), total N<sub>2</sub>O emissions measured from GHG chambers were 10 to 60 times higher in the arable field than in the herbal ley, due to N fertilizer application. Similarly, a high loss of this N fertilizer was observed during April in the form of denitrified N<sub>2</sub>.</p><p>Micucci, G., Sgouridis, F., Krause, S., Lynch, I., McNamara, N. P., Dos Santos Pereira, G., Roos, F., and Ullah, S. (2022). Towards enhanced sensitivity of the 15N Gas Flux method for quantifying denitrification in soil, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-585, https://doi.org/10.5194/egusphere-egu22-585</p><p> </p><p> </p><p> </p>

<p>Denitrification is one of the major pathways of nitrogen (N) output from soil. In this process, soil nitrate (NO<sub>3</sub><sup>-</sup>) is chemically reduced into dinitrogen (N<sub>2</sub>) through microbial respiration. Incomplete denitrification leads to the emission of nitrous oxide (N<sub>2</sub>O), a greenhouse gas 300 times more potent in inducing global warming than carbon dioxide (CO<sub>2</sub>). Denitrification is highly variable in space and time, which makes it one of the most unconstrained processes in the global N cycle.<br><br>Measuring denitrification is challenging because it emits small amounts of N<sub>2</sub>, hardly distinguishable from the high N<sub>2</sub> atmospheric background (78% in volume). The aim of this study was to increase the sensitivity of the <sup>15</sup>N Gas Flux method (<sup>15</sup>NGF), which is considered today, the only suitable method for in situ measurement of denitrification. The <sup>15</sup>NGF consists of injecting a stable isotopic tracer (<sup>15</sup>NO<sub>3</sub><sup>-</sup>) in a pre-determined area of soil and quantifying N<sub>2</sub> production via its isotopic composition over time under an enclosed chamber. In order to increase the sensitivity of this method, we aimed to optimize two parameters: the quantity of tracer injected and the N<sub>2</sub> background concentration. Increasing the amount of available nitrate represents a risk of stimulating microbes. Reducing the atmospheric N<sub>2</sub> background in situ can be challenging because of leaks and diffusion issues.<br><br>Our study focused on three different types of agricultural land uses: Arable, Herbal-Rich ley and Grass Clover ley. All three land uses were part of the same experimental field and the leys were in a 3-year rotation with the Arable. We first incubated homogenised soil under lab conditions and under different treatments of added tracer in order to increase sensitivity and observe if a microbial stimulation occurred. Gravimetric moisture was raised to 45% (on a dry mass basis) to simulate a rainfall event and increase the magnitude of denitrification. First experiments showed no detectable amount of evolved N<sub>2</sub> and thus, a custom-made gas mix had to be used. This gas mix contained 20% of dioxygen (O<sub>2</sub>), 5% of N<sub>2</sub> and 75% of Helium (He) and was used to replace the native atmosphere in the incubation chambers.</p><p>First results showed no significant difference in denitrified N for the ley soils treated with different amounts of tracer. The Arable soil however seemed to have been stimulated when using greater quantities of tracer but further results are expected to confirm this. The Arable treatment also had the highest potential of denitrification in the lab with a mean value of 6.26 x 10<sup>-1</sup> µgN/kg/h of emitted N<sub>2</sub>, compared to the leys who both emitted 1.65 x 10<sup>-1</sup> µgN/kg/h. The theoretical sensitivity is increased 24 times for the detection <sup>29</sup>N<sub>2</sub> and 97 times for the detection of <sup>30</sup>N<sub>2</sub> when using the gas mix and a 50% tracer enrichment, compared to a 20% enrichment under atmospheric conditions.</p><p>Finally, we measured denitrification directly in-situ using higher quantities of tracer and the custom-made gas mix. This was done using either modified greenhouse gas chambers or sealed plastic liners.</p>