Articles | Volume 10, issue 2
https://doi.org/10.5194/soil-10-873-2024
© Author(s) 2024. This work is distributed under the Creative Commons Attribution 4.0 License.
Soil is a major contributor to global greenhouse gas emissions and climate change
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- Final revised paper (published on 06 Dec 2024)
- Preprint (discussion started on 15 Jul 2024)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on egusphere-2024-1782', Anonymous Referee #1, 13 Aug 2024
- AC1: 'Reply on RC1', Peter M. Kopittke, 03 Sep 2024
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RC2: 'Comment on egusphere-2024-1782', Anonymous Referee #2, 22 Aug 2024
- AC2: 'Reply on RC2', Peter M. Kopittke, 03 Sep 2024
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (20 Sep 2024) by Ngonidzashe Chirinda
AR by Peter M. Kopittke on behalf of the Authors (27 Sep 2024)
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ED: Publish as is (16 Oct 2024) by Ngonidzashe Chirinda
ED: Publish as is (19 Oct 2024) by Rémi Cardinael (Executive editor)
AR by Peter M. Kopittke on behalf of the Authors (20 Oct 2024)
General Comments
The manuscript titled ‘Soil is a major contributor to global greenhouse gas emissions and climate change’ takes a broad view of the role of anthropogenic land use change, especially with regard to agricultural lands used to grow food, in global soil GHG emissions and soil carbon loss. The authors base their analysis on the previous studies of Sanderman et al. (2017) for CO2, Tian et al. (2019 and 2020) for N2O, and data from FAO (2021) for CH4 emissions. This is a valuable global analysis and synthesis that finds that net anthropogenic emissions from soil alone account for 15% of the entire global increase in radiative forcing caused by well-mixed greenhouse gases, with CO2 being the most important gas emitted from soil (74% of total soil-derived warming) followed by N2O (17%) and CH4 (9%). The authors suggest that there’s an urgent need to prevent land use change to the best of our ability and to specifically take action to prevent further thawing of permafrost, to decrease rice paddy methane emissions, and to increase N fertilizer efficiency.
However, there are a number of concerns regarding mismatch between study findings and recommendations.The authors have not fully considered other important soil C loss mitigation strategies or a more targeted approach for the most vulnerable regions given their capacity for soil C gains or GHG emissions. Current frameworks for soil carbon management are not fully explored. The authors discuss the reason for excluding uncertainty estimates, but I am not convinced that this wasn’t possible given that the main data they reference does include confidence bounds. They suggest a multifaceted approach to land management to grow the food needed to support the global population, but have failed to enumerate any innovative or targeted approaches and instead suggest a few broad, sweeping needs that were not investigated by the present study and that have not been critically assessed for their feasibility of implementation.
Specific Comments
Abstract should include a statement about the data sources used for this analysis.
Regarding study methods: See Crow & Sierra (2022): The climate benefit of sequestration in soils for warming mitigation. Biogeochemistry, 161(1), 71-84. for an alternative, potentially more robust, computational framework that assesses the contribution of simultaneous emissions and uptake on radiative forcing as the ‘climate benefit of sequestration’.
Sanderman (2017) reports uncertainty estimates, so why not use those in the current modeling effort? There is, potentially, substantial uncertainty in these estimates given the mismatch between model estimates (Sanderman 2017) and measured SOC given known spatial and temporal complexity of SOC and GHG pools and processes.
L165: C outputs as CO2 efflux only or outputs to biomass vegetation too?
L178-180: Clarification needed regarding land-use change decreasing in terms of acreage of land affected globally or intensity of the change? Thinking about rainforest deforestation and extreme ecosystem effects relative to other types of land use changes, for example.
Fig. 2: Add to the figure caption a brief note of the ecosystem/vegetation and features that each panel represents or label them below each panel. Figure takes up a lot of space and it’s not strictly necessary to show the entire soil profile, since the C and other GHGs are mainly being lost from the top of the profile.
L280 suggests that a multifaceted approach is needed that includes landowner incentives and points to Fig 3, but the figure does not include any description of how these changes might be accomplished. They are very broad recommendations and do not include any novel or innovative approaches.
L 286: Regarding the recommendation to cease land-use change, including for bioenergy production. Is there enough evidence from the current study to support this recommendation? I only see one older reference to support this statement (Fargione et al., 2008) and this is not something that the present study measured, so it is not appropriate to conjecture about. Blanket statements such as this should be made with caution, since there is a body of evidence which supports targeted use of certain marginal lands for biofuel production (but of course not something like clearing rainforests to grow biofuel feedstocks). I recommend a more measured argument based on evidence from the present study.
Fig 3. For the recommendation to reduce waterlogging, how feasible is this in rice paddy production systems? Is it more feasible in some than others? Explore this idea more fully using support from other studies if needed. I don’t understand the arrow connecting thawing of permafrost to the set of recommendations. Wouldn’t it instead make sense to connect ‘reduce total GHGs’ to the set of other recommendations? Otherwise it would make sense to connect more of the boxes to each other in perhaps three tiers instead of 2, since thawing of permafrost is caused by the increased GHGs that result from the other land management actions listed as causes.
L 310-311: Consider also referencing the publication: Bailey, V. L., Pries, C. H., & Lajtha, K. (2019). What do we know about soil carbon destabilization?. Environmental Research Letters, 14(8), 083004.
L 316: This argument about intensifying agricultural production has been made frequently before, but what are the bounds we can reasonably do this within? How does increasing the intensity of land use, rotation frequency, planting density, etc. influence the balance between C losses and gains? How much does this depend on the system, ecology, environment, and previous land use conditions? In my mind these two statements should be considered separately.
What about studies that have considered the diversion of food waste and argue that we already produce enough food globally; we just waste some large amounts?
What about arguments that a portfolio of approaches are necessary to address the magnitude of our current problem? Locally produced food, reducing emissions from importing food (food miles), addressing food waste, incentivizing agricultural and land management practices that build soil carbon and lessen emissions, simultaneously increasing N-use efficiency through precision agricultural technologies, reducing barriers to access to healthy food for marginalized communities, etc.
L418-422: I appreciate this perspective, but given the spatiotemporal variability of soil C losses and gains, it is important to consider the inputs and outputs when possible. What about the Sanderman (2017) perspective that there are identifiable regions that should be targets for soil C restoration efforts? Managing soil C effectively requires taking its differences into account - in terms of past and current land use, climatic differences, land management goals and potential land use, state of degradation, current ecosystem function and services, benefits, vulnerability to C loss, etc.
Technical Corrections
L170. Remove error message: (Figure 1Error! Reference source not found.)
L 235. “considering the atmospheric life of N2O is 109 y”