the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Environmental conditions rather than nitrogen availability limit nitrous oxide (N2O) fluxes from a temperate birch forest
Abstract. Forest ecosystems play an important role in the terrestrial nitrogen (N) cycle, accounting for over a quarter of the land area of the Earth. However, our understanding of nitrogen dynamics in forest systems is limited. The consequences of N deposition to forest ecosystems are often overlooked. In this study, dry deposition of NH3 was replicated over a two-year period in a temperate semi-natural birch forest via a unique custom-built automated NH3 release system to investigate the impact on emissions of the greenhouse gas nitrous oxide (N2O). This study provides evidence that in both natural forest soils (in-situ) and soils under controlled laboratory conditions (ex-situ), the substantial addition of reduced N compounds (NH3/NH4+) had no direct impact on N2O emissions. Emissions of N2O from these soils were dependant on the meeting of several additional thresholds, below which N2O producing activity was constrained. When environmental conditions in-situ were considered warm and wet (soil temperature >12 °C and volumetric water content >20 %), emissions of N2O were an order of magnitude higher than when either of these thresholds was not met, regardless of exposure to NH3 deposition. Ex-situ experiments indicated that microbial activity in the soils was highly constrained by the availability of labile carbon. The addition of glucose to these soils resulted in a considerable increase in N2O emissions after N application. While cumulative NH3 deposition to the in-situ soils was relatively large over the measurement period, there was no accumulation of mineral N observed in the soil, suggesting plant-uptake of N was able to mitigate N loading. The implication of these results is that forest ecosystems may be able to mitigate localised NH3 pollution plumes, in the short-term at least, without incurring an N2O penalty. However, the long-term impacts of N enhancement remain unclear and further long-term field experiments are required to examine the impact of prolonged exposure to high quantities of N deposition to forest soils.
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RC1: 'Comment on egusphere-2025-3233', Anonymous Referee #1, 02 Sep 2025
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I have thoroughly enjoyed reviewing this manuscript describing experiments to quantify impact of NH3 deposition on N2O emissions from forest soil, and additionally impact of potential carbon limitation on the magnitude of emissions. The manuscript is well written, using clear and precise language, and contains sufficient detail to easily follow described work. In particular, methodology section is well developed and would be useful to early career researchers seeking to improve their understanding of these methodologies.
The topic itself is of importance due to large uncertainty associated with N2O emissions from non-agricultural soils and in response to NH3 deposition. While tree belts are suggested as a potential measure to mitigate impacts of high NH3 producing industries (i.e. pig and poultry farms) by capturing NH3 plume, little is known of the impact on N2O. This manuscript provides experimental data to address this knowledge gap and clearly shows that environmental conditions (soil moisture and temperature) as well as carbon availability can be the main drivers behind N2O emissions rather than N availability.
I only have few minor comments below:
L167, please correct information around analytical uncertainties-one number for N2O and one for CH4
Some of the highest observed N2O fluxes occurred in July and August 2021, prior to the start of NH3 release. I cannot find any narrative or explanation for this in the discussion section. Do you have any idea why this happened? What were the environmental conditions on the experimental site during this time?
In L507-508 you say that observations in this study are consistent with the IPCC EF for non-agricultural soils. However, there is no mention anywhere in text what an indicative EF from the current experiment could be. Could you stipulate based on data from the control and impact chambers?
Citation: https://doi.org/10.5194/egusphere-2025-3233-RC1 -
RC2: 'Comment on egusphere-2025-3233', Anonymous Referee #2, 08 Sep 2025
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This study assesses the effect of NH3 deposition on N2O emissions in a temperate birch forest. NH3 deposition was simulated in the forest for 2 years throuhg an NH3 release system, and N2O emissions subsequently measured. Additionally, they performed laboratory studies with soils from the same forest, where they simulated N deposition under the different amounts of C. The study shows that NH3 deposition did not lead to an increase in N2O emissions in the forest, which only occurred in the ex-situ/laboratory experiemnts in the presence of labile C and under warm and moist conditions. This shows that forest may be able to mitigate NH3 pollution, at least on the short term, without leading to N2O penalies.
The topic is relevant and very well fits the scope of the journal. The study is well designed, and very well presented. The methodoloy used is appropiate to address the question. The soil incubations performed on top of the field trial are an excellent approach to understand the mechanisms that justify the observed resesults. The figures are clear and the article is very well written. Therefore, I only have very minor suggestions:
- Please clarify in the methods why the addition of N In the lab is done with both NH4+ and NH4NO3, instead of opting to only apply NH4+, which better simulates the addition of NH3 as it was done in the field. This comes clear in the results, in order to check the effects of both reduced and oxidized N forms, but not before.
- In Fig 2 it could be indicated that the NH3 release system was not working in July 22, as the previous 2 months N2O fluxes were high, and higher in the impact areas.
- Is there a reason in the field for the higher fluxes, before the start of the application of the NH3 treatment, in the control areas? Fluxes reached very high levels in June-July 2021, which did not happen again. Can meteorologiocal conditions (temperture or soil moisture) at that time help explaining these extremely large fluxes?
- L384-385 and Table 2: I do not think the abbreviation AN was explained before, please clarify that this stands for NH4NO3.
Citation: https://doi.org/10.5194/egusphere-2025-3233-RC2
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