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Moinet GYK, Amundson R, Galdos MV, Grace PR, Haefele SM, Hijbeek R, Van Groenigen JW, Van Groenigen KJ, Powlson DS. Climate change mitigation through soil carbon sequestration in working lands: A reality check. Glob Chang Biol 2024; 30:e17010. [PMID: 37965790 DOI: 10.1111/gcb.17010] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/07/2023] [Accepted: 10/17/2023] [Indexed: 11/16/2023]
Affiliation(s)
| | - Ronald Amundson
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, California, USA
| | - Marcelo V Galdos
- Department of Sustainable Soils and Crops, Rothamsted Research, Harpenden, UK
| | - Peter R Grace
- Queensland University of Technology, Brisbane, Queensland, Australia
| | - Stephan M Haefele
- Department of Sustainable Soils and Crops, Rothamsted Research, Harpenden, UK
| | - Renske Hijbeek
- Plant Production Systems, Wageningen University, Wageningen, The Netherlands
| | | | | | - David S Powlson
- Department of Sustainable Soils and Crops, Rothamsted Research, Harpenden, UK
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Garsia A, Moinet A, Vazquez C, Creamer RE, Moinet GYK. The challenge of selecting an appropriate soil organic carbon simulation model: A comprehensive global review and validation assessment. Glob Chang Biol 2023; 29:5760-5774. [PMID: 37571868 DOI: 10.1111/gcb.16896] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/06/2023] [Accepted: 06/21/2023] [Indexed: 08/13/2023]
Abstract
Promotion of soil organic carbon (SOC) sequestration as a potential solution to support climate change mitigation as well as more sustainable farming systems is rising steeply. As a result, voluntary carbon markets are rapidly expanding in which farmers get paid per tons of carbon dioxide sequestered. This market relies on protocols using simulation models to certify that increases in SOC stocks do indeed occur and generate tradable carbon credits. This puts tremendous pressure on SOC simulation models, which are now expected to provide the foundation for a reliable global carbon credit generation system. There exist an incredibly large number SOC simulation models which vary considerably in their applicability and sensitivity. This confronts practitioners and certificate providers with the critical challenge of selecting the models that are appropriate to the specific conditions in which they will be applied. Model validation and the context of said validation define the boundaries of applicability of the model, and are critical therefore to model selection. To date, however, guidelines for model selection are lacking. In this review, we present a comprehensive review of existing SOC models and a classification of their validation contexts. We found that most models are not validated (71%), and out of those validated, validation contexts are overall limited. Validation studies so far largely focus on the global north. Therefore, countries of the global south, the least emitting countries that are already facing the most drastic consequences of climate change, are the most poorly supported. In addition, we found a general lack of clear reporting, numerous flaws in model performance evaluation, and a poor overall coverage of land use types across countries and pedoclimatic conditions. We conclude that, to date, SOC simulation does not represent an adequate tool for globally ensuring effectiveness of SOC sequestration effort and ensuring reliable carbon crediting.
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Affiliation(s)
- Agata Garsia
- Soil Biology Group, Wageningen University, Wageningen, The Netherlands
| | - Antoine Moinet
- Soil Biology Group, Wageningen University, Wageningen, The Netherlands
| | - Carmen Vazquez
- Soil Biology Group, Wageningen University, Wageningen, The Netherlands
| | - Rachel E Creamer
- Soil Biology Group, Wageningen University, Wageningen, The Netherlands
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Moinet GYK, Hijbeek R, van Vuuren DP, Giller KE. Carbon for soils, not soils for carbon. Glob Chang Biol 2023; 29:2384-2398. [PMID: 36644803 DOI: 10.1111/gcb.16570] [Citation(s) in RCA: 10] [Impact Index Per Article: 10.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/07/2022] [Accepted: 11/17/2022] [Indexed: 05/28/2023]
Abstract
The role of soil organic carbon (SOC) sequestration as a 'win-win' solution to both climate change and food insecurity receives an increasing promotion. The opportunity may be too good to be missed! Yet the tremendous complexity of the two issues at stake calls for a detailed and nuanced examination of any potential solution, no matter how appealing. Here, we critically re-examine the benefits of global SOC sequestration strategies on both climate change mitigation and food production. While estimated contributions of SOC sequestration to climate change vary, almost none take SOC saturation into account. Here, we show that including saturation in estimations decreases any potential contribution of SOC sequestration to climate change mitigation by 53%-81% towards 2100. In addition, reviewing more than 21 meta-analyses, we found that observed yield effects of increasing SOC are inconsistent, ranging from negative to neutral to positive. We find that the promise of a win-win outcome is confirmed only when specific land management practices are applied under specific conditions. Therefore, we argue that the existing knowledge base does not justify the current trend to set global agendas focusing first and foremost on SOC sequestration. Away from climate-smart soils, we need a shift towards soil-smart agriculture, adaptative and adapted to each local context, and where multiple soil functions are quantified concurrently. Only such comprehensive assessments will allow synergies for land sustainability to be maximised and agronomic requirements for food security to be fulfilled. This implies moving away from global targets for SOC in agricultural soils. SOC sequestration may occur along this pathway and contribute to climate change mitigation and should be regarded as a co-benefit.
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Affiliation(s)
| | - Renske Hijbeek
- Plant Production Systems, Wageningen University, Wageningen, The Netherlands
| | - Detlef P van Vuuren
- PBL Netherlands Environmental Assessment Agency, The Hague, The Netherlands
- Copernicus Institute of Sustainable Development, Utrecht University, Utrecht, The Netherlands
| | - Ken E Giller
- Plant Production Systems, Wageningen University, Wageningen, The Netherlands
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Li Y, Moinet GYK, Clough TJ, Whitehead D. Organic matter contributions to nitrous oxide emissions following nitrate addition are not proportional to substrate-induced soil carbon priming. Sci Total Environ 2022; 851:158274. [PMID: 36030860 DOI: 10.1016/j.scitotenv.2022.158274] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/17/2022] [Revised: 08/16/2022] [Accepted: 08/21/2022] [Indexed: 06/15/2023]
Abstract
The addition of carbon (C) substrate often modifies the rate of soil organic matter (SOM) decomposition. This is known as the priming effect. Nitrous oxide (N2O) emissions from soil are also linked to C substrate dynamics; however, the relationship between the priming effect and N2O emissions from soil is not understood. This study aimed to investigate the effects of C and N substrate addition on the linkages between SOM priming and N2O emissions. We applied 13C-labelled substrates (acetate, butyrate, glucose; 80 μg C g-1), with water as a control, and 15N-labelled N (300 μg N g-1 soil, potassium nitrate) to three different soils, and, after 3 days, we measured the effects on the priming of SOM and sources of N2O emission. Carbon substrate addition increased both CO2- and SOM-derived N2O emissions in the presence of exogenous N. Emissions of CO2 and N2O from soils with added glucose (mean ± standard deviation, 0.73 ± 0.13 μmol m-2 s-1 and 21.4 ± 12.1 mg N m-2 h-1) were higher (p < 0.05) than those from soils treated with acetate (0.64 ± 0.11 μmol m-2 s-1 and 10.9 ± 6.5 mg N m-2 h-1) or butyrate (0.61 ± 0.11 μmol m-2 s-1 and 11.0 ± 6.6 mg N m-2 h-1), respectively. Acetate addition induced a stronger (p < 0.05) priming effect on soil C (0.07 ± 0.09 μmol C m-2 s-1) than that for glucose (0.02 ± 0.10 μmol C m-2 s-1), while butyrate addition resulted in negative priming (-0.09 ± 0.05 μmol C m-2 s-1). SOM-derived N2O emissions were relatively low from soils with butyrate addition (1.4 ± 1.5 mg N m-2 h-1) compared with acetate (2.9 ± 2.3 mg N m-2 h-1) or glucose (9.2 ± 4.5 mg N m-2 h-1). There was no clear relationship between the priming effect and SOM-derived N2O emissions. The observed priming effect related to the potential electron donor supply of the C substrates was not observed. There is a need to further examine the role of soil priming in relation to soil N2O emissions.
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Affiliation(s)
- Yuan Li
- Department of Soil and Physical Sciences, PO Box 85084, Lincoln University, Lincoln 7647, New Zealand; Manaaki Whenua - Landcare Research, PO Box 69040, Lincoln 7640, New Zealand.
| | - Gabriel Y K Moinet
- Manaaki Whenua - Landcare Research, PO Box 69040, Lincoln 7640, New Zealand
| | - Timothy J Clough
- Department of Soil and Physical Sciences, PO Box 85084, Lincoln University, Lincoln 7647, New Zealand
| | - David Whitehead
- Manaaki Whenua - Landcare Research, PO Box 69040, Lincoln 7640, New Zealand
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Moinet GYK, Dhami MK, Hunt JE, Podolyan A, Liáng LL, Schipper LA, Whitehead D, Nuñez J, Nascente A, Millard P. Soil microbial sensitivity to temperature remains unchanged despite community compositional shifts along geothermal gradients. Glob Chang Biol 2021; 27:6217-6231. [PMID: 34585498 PMCID: PMC9293425 DOI: 10.1111/gcb.15878] [Citation(s) in RCA: 10] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/10/2021] [Accepted: 08/24/2021] [Indexed: 05/29/2023]
Abstract
Climate warming may be exacerbated if rising temperatures stimulate losses of soil carbon to the atmosphere. The direction and magnitude of this carbon-climate feedback are uncertain, largely due to lack of knowledge of the thermal adaptation of the physiology and composition of soil microbial communities. Here, we applied the macromolecular rate theory (MMRT) to describe the temperature response of the microbial decomposition of soil organic matter (SOM) in a natural long-term warming experiment in a geothermally active area in New Zealand. Our objective was to test whether microbial communities adapt to long-term warming with a shift in their composition and their temperature response that are consistent with evolutionary theory of trade-offs between enzyme structure and function. We characterized the microbial community composition (using metabarcoding) and the temperature response of microbial decomposition of SOM (using MMRT) of soils sampled along transects of increasing distance from a geothermally active zone comprising two biomes (a shrubland and a grassland) and sampled at two depths (0-50 and 50-100 mm), such that ambient soil temperature and soil carbon concentration varied widely and independently. We found that the different environments were hosting microbial communities with distinct compositions, with thermophile and thermotolerant genera increasing in relative abundance with increasing ambient temperature. However, the ambient temperature had no detectable influence on the MMRT parameters or the relative temperature sensitivity of decomposition (Q10 ). MMRT parameters were, however, strongly correlated with soil carbon concentration and carbon:nitrogen ratio. Our findings suggest that, while long-term warming selects for warm-adapted taxa, substrate quality and quantity exert a stronger influence than temperature in selecting for distinct thermal traits. The results have major implications for our understanding of the role of soil microbial processes in the long-term effects of climate warming on soil carbon dynamics and will help increase confidence in carbon-climate feedback projections.
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Affiliation(s)
- Gabriel Y. K. Moinet
- Soil Biology GroupWageningen University and ResearchWageningenThe Netherlands
- Manaaki Whenua – Landcare ResearchLincolnNew Zealand
| | | | - John E. Hunt
- Manaaki Whenua – Landcare ResearchLincolnNew Zealand
| | | | - Liyĭn L. Liáng
- Manaaki Whenua – Landcare ResearchPalmerston NorthNew Zealand
| | | | | | | | | | - Peter Millard
- Manaaki Whenua – Landcare ResearchLincolnNew Zealand
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Moinet GYK, Moinet M, Hunt JE, Rumpel C, Chabbi A, Millard P. Temperature sensitivity of decomposition decreases with increasing soil organic matter stability. Sci Total Environ 2020; 704:135460. [PMID: 31812385 DOI: 10.1016/j.scitotenv.2019.135460] [Citation(s) in RCA: 15] [Impact Index Per Article: 3.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/05/2019] [Revised: 10/17/2019] [Accepted: 11/08/2019] [Indexed: 05/14/2023]
Abstract
Evaluation of the temperature sensitivity of soil organic matter (SOM) decomposition is critical for forecasting whether soils in a warming world will lose or gain carbon and, therefore, accelerate or mitigate climate warming. It is usually described, using Arrhenius kinetics, as increasing with the stability of the substrate in laboratory conditions, where substrate availability is non-limiting and where chemical recalcitrance, therefore, predominantly regulates stability. However, conditions of non-limiting subtrate availability are rare in the undisturbed soil, where physicochemical protection of substrates may control their stability. The aim of this study was to assess the temperature sensitivity of decomposition of SOM with contrasting stability in the field. Our conceptual approach was based on in situ measurements of soil CO2 efflux at a range of temperatures from root exclusion plots of increasing age (1 month and three decades) and, therefore, with SOM of increasing stability. From a set of short-term measurements in spring, using diurnal temperature variation, the relative temperature sensitivity of SOM decomposition decreased significantly (p < 0.0001) with increasing SOM stability, and was weak (Q10 < 1.3) in long-term root exclusion plots. This result was confirmed in a similar set of short-term measurements repeated later in the year, in summer, as well as from an analysis perfomed at the seasonal timscale. We provide direct field evidence that the temperature sensitivity of SOM decomposition decreases with increasing stability, in direct contrast with Arrhenius kinetics prediction, and therefore show that stability of SOM in the field cannot be the sole result of chemical recalcitrance. We conclude that the physicochemical protection of SOM, which controls SOM stability in the field, constrains the temperature sensitivity of SOM decomposition under field conditions.
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Affiliation(s)
- Gabriel Y K Moinet
- Manaaki Whenua - Landcare Research, PO Box 69040, Lincoln 7640, New Zealand; Wageningen University & Research, Department of Environmental Sciences, PO Box 47, Wageningen 6700AA, the Netherlands.
| | - Matthias Moinet
- Manaaki Whenua - Landcare Research, PO Box 69040, Lincoln 7640, New Zealand; CNRS, Institute for Ecology and Environmental Sciences (IEES), UMR 7618, Batiment EGER, F-78850 Thiverval Grignon, France
| | - John E Hunt
- Manaaki Whenua - Landcare Research, PO Box 69040, Lincoln 7640, New Zealand
| | - Cornelia Rumpel
- CNRS, Institute for Ecology and Environmental Sciences (IEES), UMR 7618, Batiment EGER, F-78850 Thiverval Grignon, France
| | - Abad Chabbi
- AgroParisTech, French Natl Inst Agr Res INRA, UMR ECOSYS, F-78850 Thiverval Grignon, France; French Natl Inst Agr Res INRA, URP3F, F-86600 Lusignan, France
| | - Peter Millard
- Manaaki Whenua - Landcare Research, PO Box 69040, Lincoln 7640, New Zealand
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Moinet GYK, Cieraad E, Turnbull MH, Whitehead D. Effects of irrigation and addition of nitrogen fertiliser on net ecosystem carbon balance for a grassland. Sci Total Environ 2017; 579:1715-1725. [PMID: 27923580 DOI: 10.1016/j.scitotenv.2016.11.199] [Citation(s) in RCA: 6] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/10/2016] [Revised: 11/27/2016] [Accepted: 11/27/2016] [Indexed: 05/27/2023]
Abstract
The ability to quantify the impacts of changing management practices on the components of net ecosystem carbon balance (NB) is required to forecast future changes in soil carbon stocks and potential feedbacks on atmospheric CO2 concentrations. In this study we investigated seasonal changes on the components of net ecosystem carbon balance resulting from the application of irrigation and nitrogen fertiliser to a temperate grassland in New Zealand where we simulated grazing events. We made seasonal measurements of the components of NB using chamber measurements in field plots with and without irrigation and addition of nitrogen fertiliser. We developed models to determine the physiological responses of gross canopy photosynthesis (A), leaf respiration (RL) and soil respiration (RS) to soil and air temperature, soil water content and irradiance and we estimated annual NB for the first year after treatments were applied. Overall, irrigation and nitrogen addition had a synergistic effect to increase annual estimates of above-ground components of carbon balance (A, RL and carbon exported through simulated grazing, Fexport), but there was no effect from adding nitrogen alone. Annual RS remained unchanged between treatments. The treatments resulted in increases in above-ground biomass production, but, with the high intensity of simulated grazing, these were not sufficient to offset ecosystem carbon losses, so all treatments remained a net source of carbon. There were no significant differences between treatments and annual NB ranged from -540gCm-2y-1 for the treatment with no irrigation and no nitrogen addition and -284gCm-2y-1 for the treatment with irrigation and nitrogen addition. Our findings from the first year of the treatments quantify the net benefits of addition of irrigation and nitrogen on increasing above-ground production for animal feed but show that this did not lead to a net increase carbon input to the soil.
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Affiliation(s)
- Gabriel Y K Moinet
- Landcare Research, PO Box 69040, Lincoln 7640, New Zealand; Centre for Integrative Ecology, School of Biological Sciences, University of Canterbury, Private Bag 4800, Christchurch 8140, New Zealand.
| | - Ellen Cieraad
- Landcare Research, PO Box 69040, Lincoln 7640, New Zealand; Institute of Environmental Sciences CML, Leiden University, Einsteinweg 2, 2333 CC, Leiden, The Netherlands
| | - Matthew H Turnbull
- Centre for Integrative Ecology, School of Biological Sciences, University of Canterbury, Private Bag 4800, Christchurch 8140, New Zealand
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