the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Episodic N2O emissions following tillage of a legume-grass cover crop mixture
- School for Environment and Sustainability, University of Michigan, Ann Arbor, 48104, USA
- School for Environment and Sustainability, University of Michigan, Ann Arbor, 48104, USA
Abstract. Nitrogen fertilizer inputs to agricultural soils are a leading cause of nitrous oxide (N2O) emissions in the U.S. Legume cover crops are an alternative N source that can reduce agricultural N2O emissions compared to fertilizer N. However, our understanding of episodic N2O flux following cover crop incorporation by tillage is limited and has focused on single species cover crops. Our study explores whether increasing cover crop functional diversity with a legume-grass mixture can reduce pulse emissions of N2O following tillage. In a field experiment, we planted crimson clover (Trifolium incarnatum L.), cereal rye (Secale cereal L.), a clover-rye mixture, and a no-cover control at two field sites with contrasting soil fertility properties in Michigan. We hypothesized that N2O flux following tillage of the cover crops would be lower in the mixture and rye compared to the clover treatment, because rye litter can decrease N mineralization rates. We measured N2O for approximately two weeks following tillage to capture the first peak of N2O emissions in each site. Across cover crop treatments, the higher fertility site, CF, had greater cover crop biomass, twofold higher aboveground biomass N, and higher cumulative N2O emissions than the lower fertility site, KBS (413 ± 67.5 g N2O-N ha−1 vs. 230 ± 42.5 g N2O-N ha−1; P = 0.0037). There was a significant treatment effect on daily emissions at both sites. At CF, N2O fluxes were higher following clover than the control 6 days after tillage. At KBS, fluxes from the mixture were higher than rye 8 and 11 days after tillage. When controlling for soil fertility properties across sites, clover and mixture led to approximately twofold higher N2O emissions compared to rye and fallow treatments. We found partial support for our hypothesis that N2O would be lower following incorporation of the mixture than clover. However, treatment patterns differed by site, suggesting that interactions between cover crop functional types and background soil fertility influence N2O emissions during cover crop decomposition.
Alison Bressler and Jennifer Blesh
Status: closed
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RC1: 'Comment on bg-2022-39', Anonymous Referee #1, 24 Feb 2022
This manuscript explores short-term N2O emissions after incorporation of cover crops – clover, rye and a clover/rye mix – at two field sites. There are many studies of N2O emissions after incorporation of plant material (cover crops, crop and tree residues), including those that compare legumes vs non-legumes, and so the novelty of the work you present, and the additional knowledge that this provides, are not apparent.
This is confounded by your study being limited in number of spp – legume, non legume and a mix – and only over a two week period, so that relationships between crop characteristics (eg N content, biomass) or functional traits, can not be rigorously determined, and consequently the discussion provides little insight into trait effects on emissions. I don’t consider this limited selection to truly represent ‘functional diversity’. You state that little is known about multiple spp, but you are only using one mixture of two spp, and there have been other studies that have measured emissions from these spp, and more rigorously examined effect of spp mixtures. The magnitude of emissions will depend on the chemical composition of the plant material, and this is well established in the literature. The magnitude of emissions from the mixture will depend on the ratio of the component material, and so I find it disappointing that you only applied one ratio of the mix.
In the introduction text why do you just focus on emissions from the US? This is a global issue, and by focusing just on the US you are limiting the reach and reader interest of your work.
Line 53 – 20 years – do you mean 20 days?
Can you please explain why you measured N2 fixation in the legume, rather than just the total biomass N – above + belowground?
Did you measure changes in soil mineral N after incorporation? I don’t see this data, but it will be essential in helping explain the impact on soil processes resulting in emissions, for example net N immobilisation (line 317). It is a major omission not to include this data. Likewise, I don’t see any measure of CO2 emissions, despite residue addition likely to stimulate microbial activity.
I may have missed this, but I don’t see data of the chemical characteristics of the clover, rye or weeds?
It would be helpful to have the daily fluxes of N2O also presented as fluxes per biomass or % C applied basis. I think you give this for cumulative N2O, but not for the daily fluxes.
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AC1: 'Reply on RC1', Alison Bressler, 31 Mar 2022
Section 1: "This manuscript explores short-term N2O emissions after incorporation of cover crops – clover, rye and a clover/rye mix – at two field sites. There are many studies of N2O emissions after incorporation of plant material (cover crops, crop and tree residues), including those that compare legumes vs non-legumes, and so the novelty of the work you present, and the additional knowledge that this provides, are not apparent."
Author's Response: Thank you for your comment. The novelty of our study is not in comparing legume and non-legume cover crops, but as we discuss in the paper, to our knowledge only two other studies have measured N2O emissions from fields with legumes as the sole external N input in organically managed grain agroecosystems (lines 306-310). Other studies have measured N2O following legume N inputs + fertilizers/manure, which typically increases overall N inputs compared to our study and does not isolate the effect of legume N sources in organically managed soils. Our study is also one of the first to include measures of labile SOM fractions relevant to internal nutrient cycling processes (i.e., POM) in a study of N2O emissions. We found one other study (Kong et al. 2009) that measured how soil organic matter fractions and N2O change over time after conversion to no-till under irrigation in a Mediterranean climate. Based on our review of the literature, our study thus provides new knowledge about episodic N2O emissions following tillage in agroecosystems with only legume N sources and is also unique for including measurements of SOM fractions.
Section 2: "This is confounded by your study being limited in number of spp – legume, non legume and a mix – and only over a two week period, so that relationships between crop characteristics (eg N content, biomass) or functional traits, can not be rigorously determined, and consequently the discussion provides little insight into trait effects on emissions. I don’t consider this limited selection to truly represent ‘functional diversity’. You state that little is known about multiple spp, but you are only using one mixture of two spp, and there have been other studies that have measured emissions from these spp, and more rigorously examined effect of spp mixtures."
Author's Response: Thank you for this feedback. We have double checked that the manuscript does not claim to draw conclusions about the role of functional traits or functional diversity per se, which was not our intention. In the paper, we simply intend to convey that we increased the functional trait diversity of the main treatment of interest (the two species mixture) by planting a legume and a grass together, which is expected to impact N2O through effects on plant litter quality and soil N availability. We plan to better justify this in the introduction with the following language: “In agroecosystems, even small increases in crop functional diversity (e.g., 2-3 species cover crop mixtures with complementary traits) can substantially impact ecosystem function (e.g., SOC, N cycling processes, microbial biomass, weed suppression) (Drinkwater et al., 1998; McDaniel et al., 2014; Tiemann et al., 2015; Blesh, 2017).” And in the discussion with: “There is growing evidence that small increases in cover crop functional diversity can simultaneously enhance multiple agroecosystem functions, including nutrient retention (Storkey et al., 2015; Blesh 2017; Kaye et al. 2019). For instance, Storkey et al. (2015) found that low to intermediate levels of species richness (1-4 species) provided an optimal balance of multiple ecosystem services when species exhibited contrasting functional traits related to growth habit and phenology.” We also propose to change headings of sections 3.3. and 4.1 to specify that we are discussing a legume-grass mixture and not functional diversity more broadly. Please see the justification for intensively measuring N2O during the weeks following tillage on lines 50-58. We have further supplemented this argument with: “Gomes et al. (2009) found greater N2O emissions during the first 45 days after terminating cover crops with a roller cutter and herbicide compared to the rest of the year.”
Gomes, J., Bayer, C., Costa, F. D., Piccolo, M. D., Zanatta, J. A., Vieira, F. C. B., and Six, J.: Soil nitrous oxide emissions in long-term cover crops-based rotations under subtropical climate. Soil Tillage Res. 106, 35-44, https://doi.org/10.1016/j.still.2009.10.001, 2009.
Section 3: "The magnitude of emissions will depend on the chemical composition of the plant material, and this is well established in the literature. The magnitude of emissions from the mixture will depend on the ratio of the component material, and so I find it disappointing that you only applied one ratio of the mix."
Author's Response: This is an important point, which we plan to expand on in the discussion at the end of section 4.1. We note that findings would likely differ for mixtures of different ratios of legume to grass. We conducted our experiment at two sites with contrasting soil fertility levels and did not have the capacity to increase the number of treatments to also test different ratios of legume to grass. However, the strength of our study is that the mixture had similar ratios at both sites, allowing for better comparison of results across sites, and we also achieved a relatively even mixture with strong legume presence, which allowed us to understand the role of fixed N inputs specifically. A growing literature on mixtures argues that mixture evenness is related to agroecosystem multifunctionality, and evenness is thus an important goal of management with mixtures. We have added this point to the discussion. We also note that testing a range of mixture ratios is an important and interesting future research need (lines 341-344).
Section 4: "In the introduction text why do you just focus on emissions from the US? This is a global issue, and by focusing just on the US you are limiting the reach and reader interest of your work."
Author's Response: Thank you for this suggestion. We plan to add the global context to the beginning of the introduction with: “Globally, N2O emissions from agricultural soils increased by 11% from 1990 to 2005 and are projected to increase by another 35% between 2005 and 2030 (USEPA, 2012).”
Section 5: "Line 53 – 20 years – do you mean 20 days?"
Author's Response: Gelfand et al.’s paper reporting on a long-term study at KBS measured N2O emissions over 20 years. The point we are making here is that by measuring N2O over 20 years, the authors found that differences in emissions between years were driven by the episodic emissions immediately following tillage every year, which we use to justify the timing of our sampling to address our research question focused on this particular emissions event following overwintering cover crops.
Section 6: "Can you please explain why you measured N2 fixation in the legume, rather than just the total biomass N – above + belowground?"
Author's Response: Yes, we will better explain why N2 fixation is an important aspect of our study to address our question about the role of legume N sources by adding the following to the first paragraph of the introduction: “Generally, total N inputs are correlated with N losses (Robertson and Vitousek 2009). However, diversified grain rotations with legume N sources which add biologically fixed N2 to fields, better balance N inputs with harvested exports and have lower potential for N losses compared with synthetic fertilizer inputs (Drinkwater et al., 1998; Blesh and Drinkwater, 2013; Robertson et al., 2014).”
From an ecosystem perspective, total N inputs to an agroecosystem (regardless of source) are correlated with N losses through leaching or as a gas. For instance, a meta-analysis on N2O emissions in agroecosystems found that higher total N inputs drive higher N2O losses by increasing N mineralization (Han et al. 2017) (lines 292-294). Legume cover crops add a new N source to soil by fixing atmospheric N2. It is therefore important to partition the legume N into the “new” N, which represents an external input (and is, in principle, more likely to explain loss pathways), compared to N that is assimilated from soil N mineralization and recycled. We also recognize that cover crops (including non-legumes) can increase internal nutrient cycling over time by scavenging and accumulating N and other nutrients in biomass and returning them to soil in relatively labile forms. This dynamic also seems to be a factor in our study and we discuss these processes in the discussion in section 4.2.
Section 7: "Did you measure changes in soil mineral N after incorporation? I don’t see this data, but it will be essential in helping explain the impact on soil processes resulting in emissions, for example net N immobilization (line 317). It is a major omission not to include this data. Likewise, I don’t see any measure of CO2 emissions, despite residue addition likely to stimulate microbial activity."
Author's Response: Thank you for the suggestion to include soil mineral N. We did measure this and will add methods and a table with soil inorganic N data at two different time points at each site (on the day after tillage, and 12-13 days later). We will also add this component throughout the discussion. We did not measure CO2 emissions in this study but agree that microbial activity increased with the addition of fresh cover crop residue (e.g., as shown by the release of inorganic N and flux of N2O measured in our experiment).
Section 8: "I may have missed this, but I don’t see data of the chemical characteristics of the clover, rye or weeds?"
Author's Response: In Figure 1 and section 3.2 of the results, we report on litter N and C:N ratio for all cover crop treatments. We did not include other measures of litter chemistry (e.g., lignin) in this study.
Section 9: "It would be helpful to have the daily fluxes of N2O also presented as fluxes per biomass or % C applied basis. I think you give this for cumulative N2O, but not for the daily fluxes."
Author's Response: Thank you for this suggestion. We will add a table to the appendix with daily N2O/aboveground cover crop biomass and biomass N.
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AC1: 'Reply on RC1', Alison Bressler, 31 Mar 2022
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RC2: 'Comment on bg-2022-39', Anonymous Referee #2, 02 Mar 2022
The manuscript is well written and assessing interesting question regarding the effect of cover crop (and mixtures) incorporation on soil nitrous oxide emissions.
At KBS site measurement length seems to be appropriate for the question asked, at the CF site, however, the post-incorporation peak emissions have not finished before the last measurement (e.g. Fig 2). Thus, cumulative emissions calculated for the CF cycle likely underestimated. This problem can be addressed, at least partially by additional analysis of the existing data.
I think that authors should include analysis of post-incorporation emissions from the KBS LTER site since, I guess CF site doesn't have long-term soil N2O emissions data. Within existing data authors can find times of cover-crop incorporation across the KBS dataset. By finding measurements of post-incorporation emissions and compare them to total annual/seasonal emissions, authors can prove that post-incorporation emissions indeed contribute significant amount of N2O emissions. This will improve the manuscript and make it more suitable for publication.
I agree with the first reviewer comments and don't want to repeat them, however, I think that incorporation of additional analysis will make this manuscript suitable for publication, despite limited novelty pointed by the reviewer 1.
Two technical comments: 1. please use appropriate decimal numbers in current version you use non, one, and two decimal numbers sometimes in the same paragraph (L237, section 3.2). 2. Figure 2, please do not use smoothing line or connection line - you have not measured continuously.
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AC2: 'Reply on RC2', Alison Bressler, 31 Mar 2022
Section 1: “The manuscript is well written and assessing interesting question regarding the effect of cover crop (and mixtures) incorporation on soil nitrous oxide emissions. At KBS site measurement length seems to be appropriate for the question asked, at the CF site, however, the post-incorporation peak emissions have not finished before the last measurement (e.g. Fig 2). Thus, cumulative emissions calculated for the CF cycle likely underestimated. This problem can be addressed, at least partially by additional analysis of the existing data.”
Author’s Response: Thank you for your positive feedback on the manuscript, and for this helpful comment regarding the data at CF. We agree this is the case for the clover treatment at CF. We now better acknowledge in the discussion that the estimate for cumulative emissions at CF is likely an underestimate. We will add an analysis in section 4.1 to provide a possible range of cumulative emissions for this treatment had we measured for a longer period: “We likely underestimated cumulative N2O emissions during the first peak following tillage at CF because emissions had not yet returned to baseline, especially for the clover treatment. By extending our empirical measurements using regression models, we estimated the trajectory of N2O emissions to approximately 19 – 26 days after tillage depending on the cover crop treatment and replicate. We estimate that cumulative N2O emissions could have reached 822.8 ± 253.2 g N2O N ha-1 in clover, 461.6 ± 59.2 g N2O N ha-1 in mixture, 340.4 ± 63.4 g N2O N ha-1 in rye, and 355.0 ± 77.4 g N2O N ha-1 in fallow. These higher estimates further increase differences in cumulative N2O emissions between sites.”
Section 2: “I think that authors should include analysis of post-incorporation emissions from the KBS LTER site since, I guess CF site doesn't have long-term soil N2O emissions data. Within existing data authors can find times of cover-crop incorporation across the KBS dataset. By finding measurements of post-incorporation emissions and compare them to total annual/seasonal emissions, authors can prove that post-incorporation emissions indeed contribute significant amount of N2O emissions. This will improve the manuscript and make it more suitable for publication. I agree with the first reviewer comments and don't want to repeat them, however, I think that incorporation of additional analysis will make this manuscript suitable for publication, despite limited novelty pointed by the reviewer 1.”
Author’s Response: Thank you for this great suggestion! Based on historical N2O data at the KBS site, we analyzed N2O emissions when they were measured within four weeks following incorporation of the red clover cover crop in the organically managed treatment at KBS. We will report this to add additional context to our short- measurements in section 4.3 of the discussion: “Additionally, we used long-term measurements of N2O emissions from the biologically-based cropping system at KBS as further context for interpreting our single-season results. Between 2014 and 2020, following the red clover cover crop, we found three instances of N2O being measured roughly two weeks apart within a month of tillage. These two-week periods of N2O emissions after tilling red clover represented 19.9 ± 2.04 % of the annual emissions from this cropping system (Robertson 2020). These N2O measurements from past years at the KBS site were not collected until at least 8 days after tillage, and likely missed the initial flux immediately following soil disturbance, which may explain why we found a slightly higher proportion of annual emissions (26.3%) following clover tillage at KBS. These historical data suggest that we indeed captured the peak N2O flux following soil disturbance by tillage in our one-year experiment.”
Robertson, G.: Trace Gas Fluxes on the Main Cropping System Experiment at the Kellogg Biological Station, Hickory Corners, MI (1991 to 2019) ver 46, Environmental Data Initiative, https://doi.org/10.6073/pasta/b1feb30692eb31b7f8a27615d18e0fa8 (Accessed 2022-02-11), 2020.
Section 3: “Two technical comments: 1. please use appropriate decimal numbers in current version you use non, one, and two decimal numbers sometimes in the same paragraph (L237, section 3.2). 2. Figure 2, please do not use smoothing line or connection line - you have not measured continuously.”
Author’s Response: Thank you for picking up on the inconsistency. We have checked for decimal places to be consistent and made edits. We appreciate this comment about the smoothing line but would also argue there are differing opinions on the acceptability of this approach in the literature on N2O emissions. In this case, the smoothing lines greatly improve the visualization of the patterns between treatments and across sites and we prefer to keep them in. We explain in the methods exactly how we calculated/estimated this curve (see Eq. 2 on line 180). We will also mention the limitation of this approach after the equation in the methods: “In the absence of continuous sampling, this approach allowed us to approximate a total flux over the sampling window and better visualize treatment patterns within and across sites.” We will also add a note to the Figure 2 caption: “The lines connecting the sampling points are intended to aid in visualizing treatment patterns for cumulative N2O and do not indicate continuous data collection (Eq. 2).”
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AC2: 'Reply on RC2', Alison Bressler, 31 Mar 2022
Status: closed
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RC1: 'Comment on bg-2022-39', Anonymous Referee #1, 24 Feb 2022
This manuscript explores short-term N2O emissions after incorporation of cover crops – clover, rye and a clover/rye mix – at two field sites. There are many studies of N2O emissions after incorporation of plant material (cover crops, crop and tree residues), including those that compare legumes vs non-legumes, and so the novelty of the work you present, and the additional knowledge that this provides, are not apparent.
This is confounded by your study being limited in number of spp – legume, non legume and a mix – and only over a two week period, so that relationships between crop characteristics (eg N content, biomass) or functional traits, can not be rigorously determined, and consequently the discussion provides little insight into trait effects on emissions. I don’t consider this limited selection to truly represent ‘functional diversity’. You state that little is known about multiple spp, but you are only using one mixture of two spp, and there have been other studies that have measured emissions from these spp, and more rigorously examined effect of spp mixtures. The magnitude of emissions will depend on the chemical composition of the plant material, and this is well established in the literature. The magnitude of emissions from the mixture will depend on the ratio of the component material, and so I find it disappointing that you only applied one ratio of the mix.
In the introduction text why do you just focus on emissions from the US? This is a global issue, and by focusing just on the US you are limiting the reach and reader interest of your work.
Line 53 – 20 years – do you mean 20 days?
Can you please explain why you measured N2 fixation in the legume, rather than just the total biomass N – above + belowground?
Did you measure changes in soil mineral N after incorporation? I don’t see this data, but it will be essential in helping explain the impact on soil processes resulting in emissions, for example net N immobilisation (line 317). It is a major omission not to include this data. Likewise, I don’t see any measure of CO2 emissions, despite residue addition likely to stimulate microbial activity.
I may have missed this, but I don’t see data of the chemical characteristics of the clover, rye or weeds?
It would be helpful to have the daily fluxes of N2O also presented as fluxes per biomass or % C applied basis. I think you give this for cumulative N2O, but not for the daily fluxes.
-
AC1: 'Reply on RC1', Alison Bressler, 31 Mar 2022
Section 1: "This manuscript explores short-term N2O emissions after incorporation of cover crops – clover, rye and a clover/rye mix – at two field sites. There are many studies of N2O emissions after incorporation of plant material (cover crops, crop and tree residues), including those that compare legumes vs non-legumes, and so the novelty of the work you present, and the additional knowledge that this provides, are not apparent."
Author's Response: Thank you for your comment. The novelty of our study is not in comparing legume and non-legume cover crops, but as we discuss in the paper, to our knowledge only two other studies have measured N2O emissions from fields with legumes as the sole external N input in organically managed grain agroecosystems (lines 306-310). Other studies have measured N2O following legume N inputs + fertilizers/manure, which typically increases overall N inputs compared to our study and does not isolate the effect of legume N sources in organically managed soils. Our study is also one of the first to include measures of labile SOM fractions relevant to internal nutrient cycling processes (i.e., POM) in a study of N2O emissions. We found one other study (Kong et al. 2009) that measured how soil organic matter fractions and N2O change over time after conversion to no-till under irrigation in a Mediterranean climate. Based on our review of the literature, our study thus provides new knowledge about episodic N2O emissions following tillage in agroecosystems with only legume N sources and is also unique for including measurements of SOM fractions.
Section 2: "This is confounded by your study being limited in number of spp – legume, non legume and a mix – and only over a two week period, so that relationships between crop characteristics (eg N content, biomass) or functional traits, can not be rigorously determined, and consequently the discussion provides little insight into trait effects on emissions. I don’t consider this limited selection to truly represent ‘functional diversity’. You state that little is known about multiple spp, but you are only using one mixture of two spp, and there have been other studies that have measured emissions from these spp, and more rigorously examined effect of spp mixtures."
Author's Response: Thank you for this feedback. We have double checked that the manuscript does not claim to draw conclusions about the role of functional traits or functional diversity per se, which was not our intention. In the paper, we simply intend to convey that we increased the functional trait diversity of the main treatment of interest (the two species mixture) by planting a legume and a grass together, which is expected to impact N2O through effects on plant litter quality and soil N availability. We plan to better justify this in the introduction with the following language: “In agroecosystems, even small increases in crop functional diversity (e.g., 2-3 species cover crop mixtures with complementary traits) can substantially impact ecosystem function (e.g., SOC, N cycling processes, microbial biomass, weed suppression) (Drinkwater et al., 1998; McDaniel et al., 2014; Tiemann et al., 2015; Blesh, 2017).” And in the discussion with: “There is growing evidence that small increases in cover crop functional diversity can simultaneously enhance multiple agroecosystem functions, including nutrient retention (Storkey et al., 2015; Blesh 2017; Kaye et al. 2019). For instance, Storkey et al. (2015) found that low to intermediate levels of species richness (1-4 species) provided an optimal balance of multiple ecosystem services when species exhibited contrasting functional traits related to growth habit and phenology.” We also propose to change headings of sections 3.3. and 4.1 to specify that we are discussing a legume-grass mixture and not functional diversity more broadly. Please see the justification for intensively measuring N2O during the weeks following tillage on lines 50-58. We have further supplemented this argument with: “Gomes et al. (2009) found greater N2O emissions during the first 45 days after terminating cover crops with a roller cutter and herbicide compared to the rest of the year.”
Gomes, J., Bayer, C., Costa, F. D., Piccolo, M. D., Zanatta, J. A., Vieira, F. C. B., and Six, J.: Soil nitrous oxide emissions in long-term cover crops-based rotations under subtropical climate. Soil Tillage Res. 106, 35-44, https://doi.org/10.1016/j.still.2009.10.001, 2009.
Section 3: "The magnitude of emissions will depend on the chemical composition of the plant material, and this is well established in the literature. The magnitude of emissions from the mixture will depend on the ratio of the component material, and so I find it disappointing that you only applied one ratio of the mix."
Author's Response: This is an important point, which we plan to expand on in the discussion at the end of section 4.1. We note that findings would likely differ for mixtures of different ratios of legume to grass. We conducted our experiment at two sites with contrasting soil fertility levels and did not have the capacity to increase the number of treatments to also test different ratios of legume to grass. However, the strength of our study is that the mixture had similar ratios at both sites, allowing for better comparison of results across sites, and we also achieved a relatively even mixture with strong legume presence, which allowed us to understand the role of fixed N inputs specifically. A growing literature on mixtures argues that mixture evenness is related to agroecosystem multifunctionality, and evenness is thus an important goal of management with mixtures. We have added this point to the discussion. We also note that testing a range of mixture ratios is an important and interesting future research need (lines 341-344).
Section 4: "In the introduction text why do you just focus on emissions from the US? This is a global issue, and by focusing just on the US you are limiting the reach and reader interest of your work."
Author's Response: Thank you for this suggestion. We plan to add the global context to the beginning of the introduction with: “Globally, N2O emissions from agricultural soils increased by 11% from 1990 to 2005 and are projected to increase by another 35% between 2005 and 2030 (USEPA, 2012).”
Section 5: "Line 53 – 20 years – do you mean 20 days?"
Author's Response: Gelfand et al.’s paper reporting on a long-term study at KBS measured N2O emissions over 20 years. The point we are making here is that by measuring N2O over 20 years, the authors found that differences in emissions between years were driven by the episodic emissions immediately following tillage every year, which we use to justify the timing of our sampling to address our research question focused on this particular emissions event following overwintering cover crops.
Section 6: "Can you please explain why you measured N2 fixation in the legume, rather than just the total biomass N – above + belowground?"
Author's Response: Yes, we will better explain why N2 fixation is an important aspect of our study to address our question about the role of legume N sources by adding the following to the first paragraph of the introduction: “Generally, total N inputs are correlated with N losses (Robertson and Vitousek 2009). However, diversified grain rotations with legume N sources which add biologically fixed N2 to fields, better balance N inputs with harvested exports and have lower potential for N losses compared with synthetic fertilizer inputs (Drinkwater et al., 1998; Blesh and Drinkwater, 2013; Robertson et al., 2014).”
From an ecosystem perspective, total N inputs to an agroecosystem (regardless of source) are correlated with N losses through leaching or as a gas. For instance, a meta-analysis on N2O emissions in agroecosystems found that higher total N inputs drive higher N2O losses by increasing N mineralization (Han et al. 2017) (lines 292-294). Legume cover crops add a new N source to soil by fixing atmospheric N2. It is therefore important to partition the legume N into the “new” N, which represents an external input (and is, in principle, more likely to explain loss pathways), compared to N that is assimilated from soil N mineralization and recycled. We also recognize that cover crops (including non-legumes) can increase internal nutrient cycling over time by scavenging and accumulating N and other nutrients in biomass and returning them to soil in relatively labile forms. This dynamic also seems to be a factor in our study and we discuss these processes in the discussion in section 4.2.
Section 7: "Did you measure changes in soil mineral N after incorporation? I don’t see this data, but it will be essential in helping explain the impact on soil processes resulting in emissions, for example net N immobilization (line 317). It is a major omission not to include this data. Likewise, I don’t see any measure of CO2 emissions, despite residue addition likely to stimulate microbial activity."
Author's Response: Thank you for the suggestion to include soil mineral N. We did measure this and will add methods and a table with soil inorganic N data at two different time points at each site (on the day after tillage, and 12-13 days later). We will also add this component throughout the discussion. We did not measure CO2 emissions in this study but agree that microbial activity increased with the addition of fresh cover crop residue (e.g., as shown by the release of inorganic N and flux of N2O measured in our experiment).
Section 8: "I may have missed this, but I don’t see data of the chemical characteristics of the clover, rye or weeds?"
Author's Response: In Figure 1 and section 3.2 of the results, we report on litter N and C:N ratio for all cover crop treatments. We did not include other measures of litter chemistry (e.g., lignin) in this study.
Section 9: "It would be helpful to have the daily fluxes of N2O also presented as fluxes per biomass or % C applied basis. I think you give this for cumulative N2O, but not for the daily fluxes."
Author's Response: Thank you for this suggestion. We will add a table to the appendix with daily N2O/aboveground cover crop biomass and biomass N.
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AC1: 'Reply on RC1', Alison Bressler, 31 Mar 2022
-
RC2: 'Comment on bg-2022-39', Anonymous Referee #2, 02 Mar 2022
The manuscript is well written and assessing interesting question regarding the effect of cover crop (and mixtures) incorporation on soil nitrous oxide emissions.
At KBS site measurement length seems to be appropriate for the question asked, at the CF site, however, the post-incorporation peak emissions have not finished before the last measurement (e.g. Fig 2). Thus, cumulative emissions calculated for the CF cycle likely underestimated. This problem can be addressed, at least partially by additional analysis of the existing data.
I think that authors should include analysis of post-incorporation emissions from the KBS LTER site since, I guess CF site doesn't have long-term soil N2O emissions data. Within existing data authors can find times of cover-crop incorporation across the KBS dataset. By finding measurements of post-incorporation emissions and compare them to total annual/seasonal emissions, authors can prove that post-incorporation emissions indeed contribute significant amount of N2O emissions. This will improve the manuscript and make it more suitable for publication.
I agree with the first reviewer comments and don't want to repeat them, however, I think that incorporation of additional analysis will make this manuscript suitable for publication, despite limited novelty pointed by the reviewer 1.
Two technical comments: 1. please use appropriate decimal numbers in current version you use non, one, and two decimal numbers sometimes in the same paragraph (L237, section 3.2). 2. Figure 2, please do not use smoothing line or connection line - you have not measured continuously.
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AC2: 'Reply on RC2', Alison Bressler, 31 Mar 2022
Section 1: “The manuscript is well written and assessing interesting question regarding the effect of cover crop (and mixtures) incorporation on soil nitrous oxide emissions. At KBS site measurement length seems to be appropriate for the question asked, at the CF site, however, the post-incorporation peak emissions have not finished before the last measurement (e.g. Fig 2). Thus, cumulative emissions calculated for the CF cycle likely underestimated. This problem can be addressed, at least partially by additional analysis of the existing data.”
Author’s Response: Thank you for your positive feedback on the manuscript, and for this helpful comment regarding the data at CF. We agree this is the case for the clover treatment at CF. We now better acknowledge in the discussion that the estimate for cumulative emissions at CF is likely an underestimate. We will add an analysis in section 4.1 to provide a possible range of cumulative emissions for this treatment had we measured for a longer period: “We likely underestimated cumulative N2O emissions during the first peak following tillage at CF because emissions had not yet returned to baseline, especially for the clover treatment. By extending our empirical measurements using regression models, we estimated the trajectory of N2O emissions to approximately 19 – 26 days after tillage depending on the cover crop treatment and replicate. We estimate that cumulative N2O emissions could have reached 822.8 ± 253.2 g N2O N ha-1 in clover, 461.6 ± 59.2 g N2O N ha-1 in mixture, 340.4 ± 63.4 g N2O N ha-1 in rye, and 355.0 ± 77.4 g N2O N ha-1 in fallow. These higher estimates further increase differences in cumulative N2O emissions between sites.”
Section 2: “I think that authors should include analysis of post-incorporation emissions from the KBS LTER site since, I guess CF site doesn't have long-term soil N2O emissions data. Within existing data authors can find times of cover-crop incorporation across the KBS dataset. By finding measurements of post-incorporation emissions and compare them to total annual/seasonal emissions, authors can prove that post-incorporation emissions indeed contribute significant amount of N2O emissions. This will improve the manuscript and make it more suitable for publication. I agree with the first reviewer comments and don't want to repeat them, however, I think that incorporation of additional analysis will make this manuscript suitable for publication, despite limited novelty pointed by the reviewer 1.”
Author’s Response: Thank you for this great suggestion! Based on historical N2O data at the KBS site, we analyzed N2O emissions when they were measured within four weeks following incorporation of the red clover cover crop in the organically managed treatment at KBS. We will report this to add additional context to our short- measurements in section 4.3 of the discussion: “Additionally, we used long-term measurements of N2O emissions from the biologically-based cropping system at KBS as further context for interpreting our single-season results. Between 2014 and 2020, following the red clover cover crop, we found three instances of N2O being measured roughly two weeks apart within a month of tillage. These two-week periods of N2O emissions after tilling red clover represented 19.9 ± 2.04 % of the annual emissions from this cropping system (Robertson 2020). These N2O measurements from past years at the KBS site were not collected until at least 8 days after tillage, and likely missed the initial flux immediately following soil disturbance, which may explain why we found a slightly higher proportion of annual emissions (26.3%) following clover tillage at KBS. These historical data suggest that we indeed captured the peak N2O flux following soil disturbance by tillage in our one-year experiment.”
Robertson, G.: Trace Gas Fluxes on the Main Cropping System Experiment at the Kellogg Biological Station, Hickory Corners, MI (1991 to 2019) ver 46, Environmental Data Initiative, https://doi.org/10.6073/pasta/b1feb30692eb31b7f8a27615d18e0fa8 (Accessed 2022-02-11), 2020.
Section 3: “Two technical comments: 1. please use appropriate decimal numbers in current version you use non, one, and two decimal numbers sometimes in the same paragraph (L237, section 3.2). 2. Figure 2, please do not use smoothing line or connection line - you have not measured continuously.”
Author’s Response: Thank you for picking up on the inconsistency. We have checked for decimal places to be consistent and made edits. We appreciate this comment about the smoothing line but would also argue there are differing opinions on the acceptability of this approach in the literature on N2O emissions. In this case, the smoothing lines greatly improve the visualization of the patterns between treatments and across sites and we prefer to keep them in. We explain in the methods exactly how we calculated/estimated this curve (see Eq. 2 on line 180). We will also mention the limitation of this approach after the equation in the methods: “In the absence of continuous sampling, this approach allowed us to approximate a total flux over the sampling window and better visualize treatment patterns within and across sites.” We will also add a note to the Figure 2 caption: “The lines connecting the sampling points are intended to aid in visualizing treatment patterns for cumulative N2O and do not indicate continuous data collection (Eq. 2).”
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AC2: 'Reply on RC2', Alison Bressler, 31 Mar 2022
Alison Bressler and Jennifer Blesh
Alison Bressler and Jennifer Blesh
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