313 results on '"Cardinael, Rémi"'
Search Results
2. Priority science can accelerate agroforestry as a natural climate solution
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Terasaki Hart, Drew E., Yeo, Samantha, Almaraz, Maya, Beillouin, Damien, Cardinael, Rémi, Garcia, Edenise, Kay, Sonja, Lovell, Sarah Taylor, Rosenstock, Todd S., Sprenkle-Hyppolite, Starry, Stolle, Fred, Suber, Marta, Thapa, Bhuwan, Wood, Stephen, and Cook-Patton, Susan C.
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- 2023
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3. Current NPP cannot predict future soil organic carbon sequestration potential. Comment on “Photosynthetic limits on carbon sequestration in croplands”
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Minasny, Budiman, Arrouays, Dominique, Cardinael, Rémi, Chabbi, Abad, Farrell, Mark, Henry, Beverley, Koutika, Lydie-Stella, Ladha, Jagdish K, McBratney, Alex B, Padarian, Jose, Dobarco, Mercedes Román, Rumpel, Cornelia, Smith, Pete, and Soussana, Jean-François
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Life on Land ,Environmental Sciences ,Biological Sciences ,Agricultural and Veterinary Sciences ,Agronomy & Agriculture - Published
- 2022
4. Multivariate regional deep learning prediction of soil properties from near-infrared, mid-infrared and their combined spectra
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Nyawasha, Rumbidzai W., Wadoux, Alexandre M.J.-C., Todoroff, Pierre, Chikowo, Regis, Falconnier, Gatien N., Lagorsse, Maeva, Corbeels, Marc, and Cardinael, Rémi
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- 2024
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5. A global meta-analysis of soil organic carbon in the Anthropocene
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Beillouin, Damien, Corbeels, Marc, Demenois, Julien, Berre, David, Boyer, Annie, Fallot, Abigail, Feder, Frédéric, and Cardinael, Rémi
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- 2023
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6. Soil organic carbon models need independent time-series validation for reliable prediction
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Le Noë, Julia, Manzoni, Stefano, Abramoff, Rose, Bölscher, Tobias, Bruni, Elisa, Cardinael, Rémi, Ciais, Philippe, Chenu, Claire, Clivot, Hugues, Derrien, Delphine, Ferchaud, Fabien, Garnier, Patricia, Goll, Daniel, Lashermes, Gwenaëlle, Martin, Manuel, Rasse, Daniel, Rees, Frédéric, Sainte-Marie, Julien, Salmon, Elodie, Schiedung, Marcus, Schimel, Josh, Wieder, William, Abiven, Samuel, Barré, Pierre, Cécillon, Lauric, and Guenet, Bertrand
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- 2023
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7. Long-term soil organic carbon and crop yield feedbacks differ between 16 soil-crop models in sub-Saharan Africa
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Couëdel, Antoine, Falconnier, Gatien N., Adam, Myriam, Cardinael, Rémi, Boote, Kenneth, Justes, Eric, Smith, Ward N., Whitbread, Anthony M., Affholder, François, Balkovic, Juraj, Basso, Bruno, Bhatia, Arti, Chakrabarti, Bidisha, Chikowo, Regis, Christina, Mathias, Faye, Babacar, Ferchaud, Fabien, Folberth, Christian, Akinseye, Folorunso M., Gaiser, Thomas, Galdos, Marcelo V., Gayler, Sebastian, Gorooei, Aram, Grant, Brian, Guibert, Hervé, Hoogenboom, Gerrit, Kamali, Bahareh, Laub, Moritz, Maureira, Fidel, Mequanint, Fasil, Nendel, Claas, Porter, Cheryl H., Ripoche, Dominique, Ruane, Alex C., Rusinamhodzi, Leonard, Sharma, Shikha, Singh, Upendra, Six, Johan, Srivastava, Amit, Vanlauwe, Bernard, Versini, Antoine, Vianna, Murilo, Webber, Heidi, Weber, Tobias K.D., Zhang, Congmu, and Corbeels, Marc
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- 2024
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8. Initial soil carbon losses may offset decades of biomass carbon accumulation in Mediterranean afforestation
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Renna, Valeria, Martín-Gallego, Pilar, Julián, Federico, Six, Johan, Cardinael, Rémi, and Laub, Moritz
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- 2024
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9. Do intercropping and mineral nitrogen fertilizer affect weed community structures in low-input maize-based cropping systems?
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Namatsheve, Talent, Cardinael, Rémi, Chikowo, Regis, Corbeels, Marc, Rugare, Joyful Tatenda, Mabasa, Stanford, and Ripoche, Aude
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- 2024
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10. Multivariate deep learning prediction of regional soil properties from near-infrared, mid-infrared and their combined spectra
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Nyawasha, Rumbidzai W., primary, Wadoux, Alexandre M.J.-C., additional, Todoroff, Pierre, additional, Chikowo, Regis, additional, Falconnier, Gatien N., additional, Lagorsse, Maeva, additional, Corbeels, Marc, additional, and Cardinael, Rémi, additional
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- 2024
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11. A global database of land management, land-use change and climate change effects on soil organic carbon
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Beillouin, Damien, Demenois, Julien, Cardinael, Rémi, Berre, David, Corbeels, Marc, Fallot, Abigail, Boyer, Annie, and Feder, Frédéric
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- 2022
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12. Interaction between soil type and cropping system on albedo dynamics leads to contrasted impact on climate mitigation
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Diop, Souleymane, primary, Cardinael, Rémi, additional, Lauerwald, Ronny, additional, Ferlicoq, Morgan, additional, Thierfelder, Christian, additional, Chikowo, Regis, additional, Corbeels, Marc, additional, and Ceschia, Eric, additional
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- 2024
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13. A novel approach to use the DayCent model for simulating agroforestry systems with multiple components
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Laub, Moritz, primary, Goff, Ulysse Le, additional, Prébandier, Marc, additional, Six, Johan, additional, and Cardinael, Rémi, additional
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- 2024
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14. Belowground functioning of agroforestry systems : recent advances and perspectives
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Cardinael, Rémi, Mao, Zhun, Chenu, Claire, and Hinsinger, Philippe
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- 2020
15. Reductions in water, soil and nutrient losses and pesticide pollution in agroforestry practices : a review of evidence and processes
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Zhu, Xiai, Liu, Wenjie, Chen, Jin, Bruijnzeel, L. Adrian, Mao, Zhun, Yang, Xiaodong, Cardinael, Rémi, Meng, Fan-Rui, Sidle, Roy C., Seitz, Steffen, Nair, Vimala D., Nanko, Kazuki, Zou, Xin, Chen, Chunfeng, and Jiang, Xiao Jin
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- 2020
16. Pathways to persistence : plant root traits alter carbon accumulation in different soil carbon pools
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Rossi, Lorenzo M. W., Mao, Zhun, Merino-Martín, Luis, Roumet, Catherine, Fort, Florian, Taugourdeau, Olivier, Boukcim, Hassan, Fourtier, Stéphane, Del Rey-Granado, Maria, Chevallier, Tiphaine, Cardinael, Rémi, Fromin, Nathalie, and Stokes, Alexia
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- 2020
17. Soil-crop long-term feedback matters to assess climate change impact on maize yield in Sub-Saharan Africa
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Couedel, Antoine, Falconnier, Gatien, Adam, Myriam, Cardinael, Rémi, Boote, Kenneth J., Justes, Eric, Ruane, Alex C., Smith, Ward N., Whitbread, Anthony M., Corbeels, Marc, Couedel, Antoine, Falconnier, Gatien, Adam, Myriam, Cardinael, Rémi, Boote, Kenneth J., Justes, Eric, Ruane, Alex C., Smith, Ward N., Whitbread, Anthony M., and Corbeels, Marc
- Abstract
Sub-Saharan Africa (SSA) faces significant food security risks, primarily due to low soil fertility leading to low crop yields. Climate change is expected to worsen food security issues in SSA due to a combined negative impact on crop yield and soil fertility. A common omission from climate change impact studies in SSA is the interaction between change in soil fertility and crop yield. Integrated soil fertility management (ISFM), which includes the combined use of mineral and organic fertilizers, is expected to increase crop yield but it is uncertain how this advantage is maintained with climate change. We explored the impact of scenarios of change in soil fertility and climate variables (temperature, rainfall, and CO2) on rainfed maize yield in four representative sites in SSA with no input and ISFM management. To do so, we used an ensemble of 15 calibrated soil-crop models. Reset and continuous simulations were performed to assess the impact of soil fertility vs climate change on crop yield. In reset simulations, SOC, soil N and soil water were reinitialized each year with the same initial conditions. In continuous simulations, SOC, soil N and soil water values of a given year were obtained from the simulation of the previous year, allowing cumulative effects on SOC and crop yields. Most models agreed that with current baseline (no input) management, yield changed by a much larger order of magnitude when considering declining soil fertility with baseline climate (-39%), compared with considering constant soil fertility but changes in temperature, rainfall and CO2 (from -12% to +5% depending on the climate variable considered). The interaction between change in soil fertility and climate variables only marginally influenced maize yield (high agreement between models). The model ensemble indicated that when accounting for soil fertility change, the benefits of ISFM systems over no-input systems increased over time (+190%). This increase in ISFM benefits was greater
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- 2024
18. Storing additional carbon in soil: different practices, different stabilities of the organic matter?
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Chenu, Claire, Kpemoua, Kossi, Cardinael, Rémi, Houot, Sabine, Baudin, François, Chevallier, Tiphaine, Barré, Pierre, Chenu, Claire, Kpemoua, Kossi, Cardinael, Rémi, Houot, Sabine, Baudin, François, Chevallier, Tiphaine, and Barré, Pierre
- Abstract
A diversity of agricultural practices and systems enable the accrual of soil organic C (SOC) stocks, with variable efficiencies. These C-storing practices increase SOC stocks, either by increasing the inputs of plant biomass or exogenous organic matter, or by decreasing the outputs of SOC reducing SOC mineralisation rates, or both. In the perspective of contributing to climate change mitigation, the temporal stability of the additional SOC stored is critical. Different approaches can be used to assess the stability of soil organic matter, such as physical fractionation of soil organic matter, chemical extractions, long term incubations and analysis of the thermal behaviour of the organic matter using RockEval© pyrolysis. These address contrasting residence times, such as of months to years (long term incubations), to several decades and centuries (particle size fractionation, RockEval© pyrolysis coupled with PARTYSOC model) We used the literature and long-term agricultural experiments in which management options (application of exogenous organic matter, conservation agriculture, organic agriculture, agroforestry) result in increased SOC stocks. We investigated the stability of the additional SOC stored, compared to the reference management option. Methods currently used in the literature to assess the temporal stability of soil organic matter do not address the same SOC kinetic pools. Care must be taken to specify which range of residence times is considered when using any method intending to evaluate the biogeochemical stability of soil organic matter, as well as when using the terms stable or labile. Management options result in slightly contrasted stability of the additional organic carbon, the application of exogenous organic matter resulting in the most stable additional carbon, compared to management options that increase belowground plant biomass inputs to soil. Carbon storing agricultural management options mobilize different stabilization processes of soil
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- 2024
19. Mulch application as the overarching factor explaining increase in soil organic carbon stocks under conservation agriculture in two 8-year-old experiments in Zimbabwe
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Shumba, Armwell, Chikowo, Régis, Thierfelder, Christian, Corbeels, Marc, Six, Johan, Cardinael, Rémi, Shumba, Armwell, Chikowo, Régis, Thierfelder, Christian, Corbeels, Marc, Six, Johan, and Cardinael, Rémi
- Abstract
Conservation agriculture (CA), combining reduced or no tillage, permanent soil cover, and improved rotations, is often promoted as a climate-smart practice. However, our understanding of the impact of CA and its respective three principles on top- and subsoil organic carbon stocks in the low-input cropping systems of sub-Saharan Africa is rather limited. This study was conducted at two long-term experimental sites established in Zimbabwe in 2013. The soil types were abruptic Lixisols at Domboshava Training Centre (DTC) and xanthic Ferralsol at the University of Zimbabwe farm (UZF). The following six treatments, which were replicated four times, were investigated: conventional tillage (CT), conventional tillage with rotation (CTR), no tillage (NT), no tillage with mulch (NTM), no tillage with rotation (NTR), and no tillage with mulch and rotation (NTMR). Maize (Zea mays L.) was the main crop, and treatments with rotation included cowpea (Vigna unguiculata L. Walp.). The soil organic carbon (SOC) concentration and soil bulk density were determined for samples taken from depths of 0–5, 5–10, 10–15, 15–20, 20–30, 30–40, 40–50, 50–75 and 75–100 cm. Cumulative organic inputs to the soil were also estimated for all treatments. SOC stocks at equivalent soil mass were significantly (p<0.05) higher in the NTM, NTR and NTMR treatments compared with the NT and CT treatments in the top 5 cm and top 10 cm layers at UZF, while SOC stocks were only significantly higher in the NTM and NTMR treatments compared with the NT and CT treatments in the top 5 cm at DTC. NT alone had a slightly negative impact on the top SOC stocks. Cumulative SOC stocks were not significantly different between treatments when considering the whole 100 cm soil profile. Our results show the overarching role of crop residue mulching in CA cropping systems with respect to enhancing SOC stocks but also that this effect is limited to the topsoil. The highest cumulative organic carbon inputs to the soil were obser
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- 2024
20. Sécurité alimentaire et ressources naturelles : stratégies de diversification
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Cardinael, Rémi, Deheuvels, Olivier, Leroux, Louise, Subervie, Julie, Suwa-Eisenmann, Akiko, Bessou, Cécile, Bouquet, Emmanuelle, Catry, Thibault, Chikowo, Régis, Corbeels, Marc, Demarchi, Gabriela, Diouf, Abdoul Aziz, Falconnier, Gatien, Faye, Ndeye Fatou, Gignoux, Jérémie, Icard-Vernière, Christèle, Jahel, Camille, Katic, Pamela, Libois, François, Mercier, Sabine, Mouquet-Rivier, Claire, Namatsheve, Talent, Renk, Andréa, Sirdey, Ninon, Tritsch, Isabelle, Verger, Eric O., Cardinael, Rémi, Deheuvels, Olivier, Leroux, Louise, Subervie, Julie, Suwa-Eisenmann, Akiko, Bessou, Cécile, Bouquet, Emmanuelle, Catry, Thibault, Chikowo, Régis, Corbeels, Marc, Demarchi, Gabriela, Diouf, Abdoul Aziz, Falconnier, Gatien, Faye, Ndeye Fatou, Gignoux, Jérémie, Icard-Vernière, Christèle, Jahel, Camille, Katic, Pamela, Libois, François, Mercier, Sabine, Mouquet-Rivier, Claire, Namatsheve, Talent, Renk, Andréa, Sirdey, Ninon, Tritsch, Isabelle, and Verger, Eric O.
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- 2024
21. Interaction between soil type and cropping system on albedo dynamics leads to contrasted impact on climate mitigation
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Diop, Souleymane, Cardinael, Rémi, Lauerwald, Ronny, Ferlicoq, Morgan, Thierfelder, Christian, Chikowo, Régis, Corbeels, Marc, Ceschia, Eric, Diop, Souleymane, Cardinael, Rémi, Lauerwald, Ronny, Ferlicoq, Morgan, Thierfelder, Christian, Chikowo, Régis, Corbeels, Marc, and Ceschia, Eric
- Abstract
The biogeochemical effects of conservation agriculture (CA), such as soil organic carbon storage and greenhouse gas emissions, have been extensively studied. However, recent research has shown that management practices also have biogeophysical effects on both local and global climates by altering surface albedo and energy partitioning. We assessed the biogeophysical impacts of CA in maize fields during two successive seasons (2021/22-2022/23) at two long-term experimental sites in Zimbabwe with contrasting soil properties: Domboshawa Training Center (DTC) with a light abruptic Lixisol (sandy soil) and the University of Zimbabwe Farm (UZF) with a dark xanthic Ferralsol (clayey soil). We monitored surface albedo, longwave radiation, leaf area index (LAI), and soil moisture/temperature under three treatments: conventional tillage (CT), notillage (NT), and no-tillage with mulch (NTM). Our findings reveal that, across all treatments during the two monitored seasons, the average surface albedo of the xanthic Ferralsol at UZF was consistently lower than that of the abruptic Lixisol at DTC. It results a cooling effect in both NT and NTM treatments compared to CT in the clayey soil at UZF. During the 2021/22 season, the mean annual radiative forcing (RF) of NT and NTM were -0.83 W.m-² and -0.43 W.m-2 respectively, while during the second season (2022/23) the annual mean RF was -1.43 W.m-2 for NT and -1.03 W.m-2 for NTM.On the sandy soil at DTC, a warming effect was observed due to soil darkening induced by mulching. The mean annual RF of NT in this site was -3.34 W.m-2 during the first season and -2.78 W.m-2 during the second. In contrast, NTM showed a warming effect with an RF of 1.2 W.m-2 in 2021/22, and 2.77 W.m-2 during the 2022/23 season. The RF induced by albedo change were converted into CO2-equivalents in order to compare it with biogeochemical effects of CA through changes in soil N2O emissions and SOC storage. The results demonstrated an opposite effect on RF and o
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- 2024
22. Cover crops do increase soil organic carbon stocks—A critical comment on Chaplot and Smith (2023)
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Poeplau, Christopher, primary, Liang, Zhi, additional, Don, Axel, additional, Seitz, Daria, additional, De Notaris, Chiara, additional, Angers, Denis, additional, Barré, Pierre, additional, Beillouin, Damien, additional, Cardinael, Rémi, additional, Ceschia, Eric, additional, Chenu, Claire, additional, Constantin, Julie, additional, Demenois, Julien, additional, Mary, Bruno, additional, Pellerin, Sylvain, additional, Plaza‐Bonilla, Daniel, additional, Quemada, Miguel, additional, and Justes, Eric, additional
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- 2024
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23. The 4 per 1000 goal and soil carbon storage under agroforestry and conservation agriculture systems in sub-Saharan Africa
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Corbeels, Marc, Cardinael, Rémi, Naudin, Krishna, Guibert, Hervé, and Torquebiau, Emmanuel
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- 2019
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24. Diachronic assessment of soil organic C and N dynamics under long-term no-till cropping systems in the tropical upland of Cambodia.
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Leng, Vira, Cardinael, Rémi, Tivet, Florent, Seng, Vang, Mark, Phearum, Lienhard, Pascal, Filloux, Titouan, Six, Johan, Hok, Lyda, Boulakia, Stéphane, Briedis, Clever, Sá, João Carlos de Moraes, and Thuriès, Laurent
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CROPPING systems ,NO-tillage ,TROPICAL crops ,CROP rotation ,UPLANDS ,SOIL degradation ,COVER crops - Abstract
No-till (NT) cropping systems have been proposed as a potential strategy to combat soil degradation and global warming by storing soil organic carbon (SOC) and nitrogen (N). Yet, there are ongoing debates about the real benefits of NT systems and factors influencing SOC and N accumulation. Assessing the dynamics of SOC and N on the long-term is needed to fill knowledge gaps and provide robust scientific evidence for potential additional SOC storage. We quantified the changes in SOC and N stocks and fractions down to 100 cm depth from three 13-year-old experiments in a tropical red Oxisol in Cambodia, comparing conventional tillage (CT) to NT monocropping and NT crop rotation systems using a diachronic and equivalent soil mass (ESM) approach. The three experiments comprised maize-, soybean-, and cassava-based cropping system trials, hereafter called MaiEx, SoyEx, and CasEx, respectively. Soil samples were collected in 2021, 10 years after the first sampling in 2011, at 7 depths: 0–5, 5–10, 10–20, 20–40, 40–60, 60–80, and 80–100 cm. Over the 10-year period (2011–2021), significant impacts on SOC stock and its vertical distribution differed among the NT systems and in the three experiments. In MaiEx and CasEx, the soils under all the NT systems significantly (P > 0.05) accumulated SOC stock across the soil depths, with the accumulation ranging from 6.97 to 14.71 Mg C ha
-1 in the whole profile (0–100 cm). In SoyEx, significant increase in SOC stock was limited to the top 0–20 cm under NT monocropping, whereas NT crop rotation systems had significantly accumulating SOC stock from 0 to 80 cm depths. When considering 0–100 cm as a single stratum, the annual SOC cumulative rate in NT systems ranged from 0.86–1.47, 0.65–1.00, and 0.70–1.07 Mg C ha-1 yr-1 in MaiEx, SoyEx, and CasEx, respectively. In the top 0–10 cm, NT systems significantly increased C concentration in particulate organic matter (POM) by 115 %, 118 %, in MaiEx and SoyEx, respectively, and by 37 % in CasEx although not significantly. Similarly, at 0–10 cm depth, NT systems significantly enhanced C concentration in the mineral-associated organic matter (MAOM) by 33 %, 21 %, in MaiEx and SoyEx, respectively. Significant increase of C in MAOM was also observed from 0 to 40 cm in CasEx. In contrast, total N stock in NT systems increased in the surface 0–5 cm depth but decreased below 10 cm and in the whole profile (0–100 cm), particularly under NT monocropping with an annual loss rate of -0.10 and -0.17 Mg N ha-1 yr-1 in SoyEx and CasEx, respectively. Although NT systems increased N concentration in POM in the top 0–10 cm of MaiEx and SoyEx, a decreasing trend was observed below 10 cm depth. The N concentration in POM under NT systems in CasEx also decreased with soil depth. From 2011 to 2021, N concentration in MAOM under NT systems remained stable in MaiEx and SoyEx in the top 0–5 cm, but significant decreases in MaiEx and CasEx below 5 cm. Our findings suggest that adopting NT cropping systems with diverse crop and cover crop species and high biomass C inputs in the long-term leads to SOC accumulation not only in the surface but also in deeper layers, by increasing both the C pools in the POM and MAOM size fractions, even on the cassava-based system, which is believed to be an annual crop that could cause serious soil fertility depletion. This study highlights the potential of NT cropping systems to store SOC over time, but raises questions about soil N dynamics. [ABSTRACT FROM AUTHOR]- Published
- 2024
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25. The input reduction principle of agroecology is wrong when it comes to mineral fertilizer use in sub-Saharan Africa
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Falconnier, Gatien N, primary, Cardinael, Rémi, additional, Corbeels, Marc, additional, Baudron, Frédéric, additional, Chivenge, Pauline, additional, Couëdel, Antoine, additional, Ripoche, Aude, additional, Affholder, François, additional, Naudin, Krishna, additional, Benaillon, Emilie, additional, Rusinamhodzi, Leonard, additional, Leroux, Louise, additional, Vanlauwe, Bernard, additional, and Giller, Ken E, additional
- Published
- 2023
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26. Soil N2O emissions during dry fallow periods.
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Cardinael, Rémi, Barton, Louise, Corbeels, Marc, Six, Johan, Rowlings, David, Shumba, Armwell, Chikowo, Regis, and Farrell, Mark
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ARID regions , *NITROUS oxide , *FALLOWING , *FARMS , *SOILS - Abstract
Shang et al. (2024) recently suggested to include nitrous oxide (N2O) emissions during the fallow period to better estimate N2O emission factors (EFs). We however highlighted several pitfalls of the proposed adjusted EFs for croplands in the specific case of dry subhumid, semiarid, and arid regions with dry fallow periods, these regions covering about 47% of the Earth's terrestrial area. [ABSTRACT FROM AUTHOR]
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- 2024
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27. Spatial variation of earthworm communities and soil organic carbon in temperate agroforestry
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Cardinael, Rémi, Hoeffner, Kevin, Chenu, Claire, Chevallier, Tiphaine, Béral, Camille, Dewisme, Antoine, and Cluzeau, Daniel
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- 2019
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28. Conservation agriculture increases soil organic carbon stocks but not soil CO2 efflux in two 8-year-old experiments in Zimbabwe
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Shumba, Armwell, primary, Chikowo, Regis, additional, Thierfelder, Christian, additional, Corbeels, Marc, additional, Six, Johan, additional, and Cardinael, Rémi, additional
- Published
- 2023
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29. Supplementary material to "Conservation agriculture increases soil organic carbon stocks but not soil CO2 efflux in two 8-year-old experiments in Zimbabwe"
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Shumba, Armwell, primary, Chikowo, Regis, additional, Thierfelder, Christian, additional, Corbeels, Marc, additional, Six, Johan, additional, and Cardinael, Rémi, additional
- Published
- 2023
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30. Productivity and biological N2-fixation in cereal-cowpea intercropping systems in sub-Saharan Africa. A review
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Namatsheve, Talent, Cardinael, Rémi, Corbeels, Marc, and Chikowo, Regis
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- 2020
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31. Conservation agriculture increases soil organic carbon stocks but not soil CO2 efflux in two 8-year-old experiments in Zimbabwe
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Shumba, Armwell, Chikowo, Regis, Thierfelder, Christian, Corbeels, Marc, Six, Johan, and Cardinael, Rémi
- Abstract
Conservation agriculture (CA), combining reduced or no tillage, permanent soil cover and improved rotations, is often promoted as a climate-smart practice. However, our understanding about the impact of CA and its respective three principles on top and sub-soil organic carbon (SOC) stocks and on soil CO2 efflux in low input cropping systems of sub-Saharan Africa is rather limited. The study was conducted at two long-term experimental sites established in 2013 in Zimbabwe. The soil types were abruptic Lixisols at Domboshava Training Centre (DTC) and xanthic Ferralsol at the University of Zimbabwe farm (UZF). Six treatments, replicated four times were investigated: conventional tillage (CT), conventional tillage with rotation (CTR), NT, no-tillage with mulch (NTM), no-tillage with rotation (NTR), no-tillage with mulch and rotation (NTMR). Maize (Zea mays L.) was the main crop and treatments with rotation included cowpea (Vigna unguiculata L. Walp.). SOC concentration and bulk density were determined for samples taken from the 0–5, 5–10, 10–15, 15–20, 20–30, 30–40, 40–50, 50–75 and 75–100 cm depths. Gas samples were regularly collected using the static chamber method during the 2019/20 and 2020/21 cropping seasons and during the 2020/21 dry season. SOC stocks were significantly (p < 0.05) higher under NTM, NTR and NTMR compared to NT and CT in top 5 and 10 cm layers at UZF, while SOC stocks were only significantly higher under NTM and NTMR compared to NT and CT in top 5 cm at DTC. NT alone had a slightly negative impact on top SOC stock. Cumulative SOC stocks were not significantly different between treatments when considering the whole 100 cm soil profile. Regardless of larger organic carbon inputs in mulch treatments, there were no significant differences in CO2 efflux between treatments, but it was higher in maize rows than in inter-rows as a result of autotrophic respiration from maize roots. Our results show the overarching role of crop residue mulching in CA cropping systems in enhancing SOC storage but that this effect is limited to the topsoil.
- Published
- 2023
32. Semantics about soil organic carbon storage: DATA4C+, a comprehensive thesaurus and classification of management practices in agriculture and forestry
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Fujisaki, Kenji, primary, Chevallier, Tiphaine, additional, Bispo, Antonio, additional, Laurent, Jean-Baptiste, additional, Thevenin, François, additional, Chapuis-Lardy, Lydie, additional, Cardinael, Rémi, additional, Le Bas, Christine, additional, Freycon, Vincent, additional, Bénédet, Fabrice, additional, Blanfort, Vincent, additional, Brossard, Michel, additional, Tella, Marie, additional, and Demenois, Julien, additional
- Published
- 2023
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33. Healthy soils sustain food system transformations to contribute to the net zero CO2 emission target by 2050
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Chotte, Jean-Luc, Barot, Sébastien, Blanchart, Eric, Blanfort, Vincent, Brauman, Alain, Cardinael, Rémi, Demenois, Julien, Lardy, Lydie, Luu, Paul, Masse, Dominique, Chevalier, Tiphaine, Trap, Jean, Wadoux, Alexandre M. J. C., Chotte, Jean-Luc, Barot, Sébastien, Blanchart, Eric, Blanfort, Vincent, Brauman, Alain, Cardinael, Rémi, Demenois, Julien, Lardy, Lydie, Luu, Paul, Masse, Dominique, Chevalier, Tiphaine, Trap, Jean, and Wadoux, Alexandre M. J. C.
- Published
- 2023
34. Modelling albedo and the energy budget using the STICS soil-crop model - Application to two Sub-Saharan sites
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Diop, Souleymane, Cardinael, Rémi, Falconnier, Gatien, Lauerwald, Ronny, Felicoq, Morgan, Thierfelder, Christian, Affholder, François, Chikowo, Régis, Ceschia, Eric, Diop, Souleymane, Cardinael, Rémi, Falconnier, Gatien, Lauerwald, Ronny, Felicoq, Morgan, Thierfelder, Christian, Affholder, François, Chikowo, Régis, and Ceschia, Eric
- Abstract
Introduction - Climate impacts of agricultural management practices such as mulching and no-tillage are usually evaluated with regard to soil organic carbon stock changes or greenhouse emissions. However, albedo effects of these practices that have been found to be of similar importance for climate change mitigation are usually ignored in this kind of assessment. This is even true for agricultural systems in Africa, which are less studied than temperate systems. In this study, we aim to assess the effect of land management on albedo dynamics and Radiative Forcing (i.e. climatic impact) in two long-term experiments established in Zimbabwe in 2013 with contrasting soil types. The Radiative Forcing (RF), is a metric used to quantify the change in Earth energy budget (radiation absorbed and emitted by the Earth) relative to an assumed default state (Betts 2000; Forster et al. 2007). The albedo of a cropland depends on soil properties, surface rugosity, soil moisture and coverage by plant litter, but also on plant density, phenology, architecture and spectral properties. Note that the latter may change for instance with phenology. The RFs resulting from land management changes are determined by their effects on the surface albedo dynamics but also by the solar radiation and atmospheric transmittance dynamics. Using a soil-crop model such as STICS coupled with a spatialization method that allows to represent changes in vegetation and soil properties is a promising solution to upscale RF related to albedo effects associated to land management changes at regional to global scales. 1. Modelling albedo using STICS Surface albedo is the fraction of solar radiation reflected by Earth surface back to the space. Currently, STICS estimates surface albedo as a function of soil and vegetation albedo (Brisson et al., 2008). Soil albedo is a function of soil colour and moisture and also depends on the presence of mulch at the surface. Current formalism considers total leaf area index
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- 2023
35. Modeling agroecological intensification in the tropics with the Stics model - lessons learned and way forward
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Couedel, Antoine, Affholder, François, Adam, Myriam, Balde, Alpha Bocar, Cardinael, Rémi, Christina, Mathias, Civil, Jean Alain, De Freitas, Mathilde, Diop, Souleymane, Gamene, Aminata, Giner, Michel, Justes, Eric, Kwenda, Illiana, Midingoyi, Cyrille Ahmed, Pierre, Caroline, Pret, Valentin, Ranaivoson, Lalaina Bakotiana, Ripoche, Aude, Senghor, Yolande, Sow, Sidy, Traore, Amadou, Falconnier, Gatien, Couedel, Antoine, Affholder, François, Adam, Myriam, Balde, Alpha Bocar, Cardinael, Rémi, Christina, Mathias, Civil, Jean Alain, De Freitas, Mathilde, Diop, Souleymane, Gamene, Aminata, Giner, Michel, Justes, Eric, Kwenda, Illiana, Midingoyi, Cyrille Ahmed, Pierre, Caroline, Pret, Valentin, Ranaivoson, Lalaina Bakotiana, Ripoche, Aude, Senghor, Yolande, Sow, Sidy, Traore, Amadou, and Falconnier, Gatien
- Abstract
The year 2023 will likely be the hottest ever recorded on our planet. Adapting to climate change and climate extremes is increasingly becoming a day-to-day concern for African farmers, along with food security and income issues. Agricultural adaptations like varietal choice and fertilizer doses have deserved great attention from the crop modeling community, and are overall well accounted for by crop models. Agroecological practices, for example residue mulching, rotation and intercropping with legumes and application of organic amendments offer great potential to adapt to climate change. Yet, they have deserved less attention when it comes to the modeling of their performance in tropical context. In this abstract, we describe a collective research effort to update and test the Stics soil-crop model to account for the impact of agroecological practices on cropping system performance in the tropics. We built on multiple years of measurements in contrasting experimental sites from cool to warm, semi-arid to sub-humid subtropical environments, in Senegal, Zimbabwe, Mali, Burkina Faso, Kenya, Brazil and Madagascar. We assessed the skills and pitfalls of the model to simulate i) new cereal and legume crops ii) cereal-legume intercropping, iii) crop residue decomposition and feedbacks on crop growth and iv) crop residue mulching. We calibrated a new set of parameters for tropical maize (Falconnier et al., 2020), sorghum (Traoré et al., 2022, Ganeme et al., in revision), millet (Sow et al., forthcoming), rice (Ranaivoson et al., 2022), and legumes like cowpea (Traoré et al., 2022, Ganeme et al., in revision) and groundnut (Civil, 2022). Model accuracy (rRMSE) for end-of-season variables like aboveground biomass and grain yield was in the range of 20 to 50%. The scrutiny of in-season soil water and plant leaf area index (LAI) indicated that water stress was often underestimated, possibly because of underestimation of soil evaporation, and underestimation of the impact of wat
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- 2023
36. The input reduction principle of agroecology is wrong when it comes to mineral fertilizer use in sub-Saharan Africa
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Falconnier, Gatien N., Cardinael, Rémi, Corbeels, Marc, Baudron, Frédéric, Chivenge, Pauline, Couëdel, Antoine, Ripoche, Aude, Affholder, François, Naudin, Krishna, Benaillon, Emilie, Rusinamhodzi, Leonard, Leroux, Louise, Vanlauwe, Bernard, Giller, Ken E., Falconnier, Gatien N., Cardinael, Rémi, Corbeels, Marc, Baudron, Frédéric, Chivenge, Pauline, Couëdel, Antoine, Ripoche, Aude, Affholder, François, Naudin, Krishna, Benaillon, Emilie, Rusinamhodzi, Leonard, Leroux, Louise, Vanlauwe, Bernard, and Giller, Ken E.
- Abstract
Can farmers in sub-Saharan Africa (SSA) boost crop yields and improve food availability without using more mineral fertilizer? This question has been at the center of lively debates among the civil society, policy-makers, and in academic editorials. Proponents of the “yes” answer have put forward the “input reduction” principle of agroecology, i.e. by relying on agrobiodiversity, recycling and better efficiency, agroecological practices such as the use of legumes and manure can increase crop productivity without the need for more mineral fertilizer. We reviewed decades of scientific literature on nutrient balances in SSA, biological nitrogen fixation of tropical legumes, manure production and use in smallholder farming systems, and the environmental impact of mineral fertilizer. Our analyses show that more mineral fertilizer is needed in SSA for five reasons: (i) the starting point in SSA is that agricultural production is “agroecological” by default, that is, very low mineral fertilizer use, widespread mixed crop-livestock systems and large crop diversity including legumes, but leading to poor soil fertility as a result of widespread soil nutrient mining, (ii) the nitrogen needs of crops cannot be adequately met solely through biological nitrogen fixation by legumes and recycling of animal manure, (iii) other nutrients like phosphorus and potassium need to be replaced continuously, (iv) mineral fertilizers, if used appropriately, cause little harm to the environment, and (v) reducing the use of mineral fertilizers would hamper productivity gains and contribute indirectly to agricultural expansion and to deforestation. Yet, the agroecological principles directly related to soil fertility—recycling, efficiency, diversity—remain key in improving soil health and nutrient-use efficiency, and are critical to sustaining crop productivity in the long run. We argue for a nuanced position that acknowledges the critical need for more mineral fertilizers in SSA, in combination
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- 2023
37. An interactive global review of practices for increasing soil carbon
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Demenois, Julien, Beillouin, Damien, Cardinael, Rémi, Corbeels, Marc, Laurent, Jean-Baptiste, Berre, David, Boyer, Annie, Fallot, Abigail, Feder, Frédéric, Thévenin, François, Demenois, Julien, Beillouin, Damien, Cardinael, Rémi, Corbeels, Marc, Laurent, Jean-Baptiste, Berre, David, Boyer, Annie, Fallot, Abigail, Feder, Frédéric, and Thévenin, François
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- 2023
38. The input reduction principle of agroecology is wrong when it comes to mineral fertilizer use in sub-Saharan Africa
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Falconnier, Gatien, Cardinael, Rémi, Corbeels, Marc, Baudron, Frédéric, Chivenge, Pauline, Couedel, Antoine, Ripoche, Aude, Affholder, François, Naudin, Krishna, Benaillon, Emilie, Rusinamhodzi, Léonard, Leroux, Louise, Vanlauwe, Bernard, Giller, Ken E., Falconnier, Gatien, Cardinael, Rémi, Corbeels, Marc, Baudron, Frédéric, Chivenge, Pauline, Couedel, Antoine, Ripoche, Aude, Affholder, François, Naudin, Krishna, Benaillon, Emilie, Rusinamhodzi, Léonard, Leroux, Louise, Vanlauwe, Bernard, and Giller, Ken E.
- Abstract
Can farmers in sub-Saharan Africa (SSA) boost crop yields and improve food availability without using more mineral fertilizer? This question has been at the center of lively debates among the civil society, policy-makers, and in academic editorials. Proponents of the “yes” answer have put forward the “input reduction” principle of agroecology, i.e. by relying on agrobiodiversity, recycling and better efficiency, agroecological practices such as the use of legumes and manure can increase crop productivity without the need for more mineral fertilizer. We reviewed decades of scientific literature on nutrient balances in SSA, biological nitrogen fixation of tropical legumes, manure production and use in smallholder farming systems, and the environmental impact of mineral fertilizer. Our analyses show that more mineral fertilizer is needed in SSA for five reasons: (i) the starting point in SSA is that agricultural production is “agroecological” by default, that is, very low mineral fertilizer use, widespread mixed crop-livestock systems and large crop diversity including legumes, but leading to poor soil fertility as a result of widespread soil nutrient mining, (ii) the nitrogen needs of crops cannot be adequately met solely through biological nitrogen fixation by legumes and recycling of animal manure, (iii) other nutrients like phosphorus and potassium need to be replaced continuously, (iv) mineral fertilizers, if used appropriately, cause little harm to the environment, and (v) reducing the use of mineral fertilizers would hamper productivity gains and contribute indirectly to agricultural expansion and to deforestation. Yet, the agroecological principles directly related to soil fertility—recycling, efficiency, diversity—remain key in improving soil health and nutrient-use efficiency, and are critical to sustaining crop productivity in the long run. We argue for a nuanced position that acknowledges the critical need for more mineral fertilizers in SSA, in combination
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- 2023
39. Soil organic carbon models need independent time-series validation for reliable prediction
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Le Noë, Juia, Manzoni, Stefano, Abramoff, Rose, Bölscher, Tobias, Bruni, Elisa, Cardinael, Rémi, Ciais, Philippe, Chenu, Claire, Clivot, Hugues, Derrien, Delphine, Ferchaud, Fabien, Garnier, Patricia, Goll, Daniel, Lashermes, Gwenaëlle, Martin, Manuel, Rasse, Daniel, Rees, Frédéric, Sainte-Marie, Julien, Salmon, Elodie, Schiedung, Marcus, Schimel, Josh, Wieder, William, Abiven, Samuel, Barré, Pierre, Cécillon, Lauric, Guenet, Bertrand, Le Noë, Juia, Manzoni, Stefano, Abramoff, Rose, Bölscher, Tobias, Bruni, Elisa, Cardinael, Rémi, Ciais, Philippe, Chenu, Claire, Clivot, Hugues, Derrien, Delphine, Ferchaud, Fabien, Garnier, Patricia, Goll, Daniel, Lashermes, Gwenaëlle, Martin, Manuel, Rasse, Daniel, Rees, Frédéric, Sainte-Marie, Julien, Salmon, Elodie, Schiedung, Marcus, Schimel, Josh, Wieder, William, Abiven, Samuel, Barré, Pierre, Cécillon, Lauric, and Guenet, Bertrand
- Abstract
Numerical models are crucial to understand and/or predict past and future soil organic carbon dynamics. For those models aiming at prediction, validation is a critical step to gain confidence in projections. With a comprehensive review of ~250 models, we assess how models are validated depending on their objectives and features, discuss how validation of predictive models can be improved. We find a critical lack of independent validation using observed time series. Conducting such validations should be a priority to improve the model reliability. Approximately 60% of the models we analysed are not designed for predictions, but rather for conceptual understanding of soil processes. These models provide important insights by identifying key processes and alternative formalisms that can be relevant for predictive models. We argue that combining independent validation based on observed time series and improved information flow between predictive and conceptual models will increase reliability in predictions.
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- 2023
40. Fertilizer and soil health in Africa: The role of fertilizer in building soil health to sustain farming and address climate change
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Vanlauwe, Bernard, Amede, Tilahun, Bationo, André, Bindraban, Prem, Breman, Henk, Cardinael, Rémi, Couedel, Antoine, Chivenge, Pauline, Corbeels, Marc, Dobermann, Achim, Falconnier, Gatien, Fatunbi, Wole, Giller, Ken E., Harawa, Rebbie, Kamau, Mercy, Merckx, Roel, Palm, Cheryl, Powlson, David, Rusinamhodzi, Léonard, Six, Johan, Singh, Upendra, Stewart, Zachary, van Ittersum, Martin, Witt, Christian, Zingore, Shamie, Groot, Rob, Vanlauwe, Bernard, Amede, Tilahun, Bationo, André, Bindraban, Prem, Breman, Henk, Cardinael, Rémi, Couedel, Antoine, Chivenge, Pauline, Corbeels, Marc, Dobermann, Achim, Falconnier, Gatien, Fatunbi, Wole, Giller, Ken E., Harawa, Rebbie, Kamau, Mercy, Merckx, Roel, Palm, Cheryl, Powlson, David, Rusinamhodzi, Léonard, Six, Johan, Singh, Upendra, Stewart, Zachary, van Ittersum, Martin, Witt, Christian, Zingore, Shamie, and Groot, Rob
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- 2023
41. Semantics about soil organic carbon storage: DATA4C+, a comprehensive thesaurus and classification of management practices in agriculture and forestry
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Fujisaki, Kenji, Chevallier, Tiphaine, Bispo, Antonio, Laurent, Jean-Baptiste, Thévenin, François, Chapuis-Lardy, Lydie, Cardinael, Rémi, Le Bas, Christine, Freycon, Vincent, Bénédet, Fabrice, Blanfort, Vincent, Brossard, Michel, Tella, Marie, Demenois, Julien, Fujisaki, Kenji, Chevallier, Tiphaine, Bispo, Antonio, Laurent, Jean-Baptiste, Thévenin, François, Chapuis-Lardy, Lydie, Cardinael, Rémi, Le Bas, Christine, Freycon, Vincent, Bénédet, Fabrice, Blanfort, Vincent, Brossard, Michel, Tella, Marie, and Demenois, Julien
- Abstract
Identifying the drivers of soil organic carbon (SOC) stock changes is of the utmost importance to contribute to global challenges like climate change, land degradation, biodiversity loss, or food security. Evaluating the impacts of land use and management practices in agriculture and forestry on SOC is still challenging. Merging datasets or making databases interoperable is a promising way, but still has several semantic challenges. So far, a comprehensive thesaurus and classification of management practices in agriculture and forestry has been lacking, especially while focusing on SOC storage. Therefore, the aim of this paper is to present a first comprehensive thesaurus for management practices driving SOC storage (DATA4C+). The DATA4C+ thesaurus contains 224 classified and defined terms related to land management practices in agriculture and forestry. It is organized as a hierarchical tree reflecting the drivers of SOC storage. It is oriented to be used by scientists in agronomy, forestry, and soil sciences with the aim of uniformizing the description of practices influencing SOC in their original research. It is accessible in Agroportal (http://agroportal.lirmm.fr/ontologies/DATA4CPLUS, last access: 24 March 2022) to enhance its findability, accessibility, interoperability, and reuse by scientists and others such as laboratories or land managers. Future uses of the DATA4C+ thesaurus will be crucial to improve and enrich it, but also to raise the quality of meta-analyses on SOC, and ultimately help policymakers to identify efficient agricultural and forest management practices to enhance SOC storage.
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- 2023
42. Prediction of soil organic carbon stock using visible and near infrared reflectance spectroscopy (VNIRS) in the field
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Cambou, Aurélie, Cardinael, Rémi, Kouakoua, Ernest, Villeneuve, Manon, Durand, Céline, and Barthès, Bernard G.
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- 2016
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43. Unexpected phenology and lifespan of shallow and deep fine roots of walnut trees grown in a silvoarable Mediterranean agroforestry system
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Germon, Amandine, Cardinael, Rémi, Prieto, Iván, Mao, Zhun, Kim, John, Stokes, Alexia, Dupraz, Christian, Laclau, Jean-Paul, and Jourdan, Christophe
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- 2016
44. Impact of alley cropping agroforestry on stocks, forms and spatial distribution of soil organic carbon — A case study in a Mediterranean context
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Cardinael, Rémi, Chevallier, Tiphaine, Barthès, Bernard G., Saby, Nicolas P.A., Parent, Théophile, Dupraz, Christian, Bernoux, Martial, and Chenu, Claire
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- 2015
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45. Long-term tillage, residue management and crop rotation impacts on N2O and CH4 emissions from two contrasting soils in sub-humid Zimbabwe
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Shumba, Armwell, primary, Chikowo, Regis, additional, Corbeels, Marc, additional, Six, Johan, additional, Thierfelder, Christian, additional, and Cardinael, Rémi, additional
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- 2023
- Full Text
- View/download PDF
46. A marginal abatement cost curve for greenhouse gases attenuation by additional carbon storage in French agricultural land
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Bamiere, Laure, Bellassen, Valentin, Angers, Denis, Cardinael, Rémi, Ceschia, Eric, Chenu, Claire, Constantin, Julie, Delame, Nathalie, Diallo, A., Graux, Anne-Isabelle, Houot, Sabine, Klumpp, Katja, Launay, Camille, Letort, Elodie, Martin, Raphael, Meziere, Delphine, Mosnier, Claire, Réchauchère, Olivier, Schiavo, Michele, Thérond, Olivier, Pellerin, Sylvain, Paris-Saclay Applied Economics (UMR PSAE), AgroParisTech-Université Paris-Saclay-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Centre d'Economie et de Sociologie Rurales Appliquées à l'Agriculture et aux Espaces Ruraux (CESAER), Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut Agro Dijon, Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro), Centre de recherche et de développement sur les aliments, Agriculture et Agroalimentaire Canada [Saint Hyacinte, Québec, Canada], Agroécologie et Intensification Durables des cultures annuelles (UPR AIDA), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad), Direction du département Performances des systèmes de production et de transformation tropicaux (Direction Persyst), University of Zimbabwe (UZ), Centre d'études spatiales de la biosphère (CESBIO), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Ecologie fonctionnelle et écotoxicologie des agroécosystèmes (ECOSYS), AGroécologie, Innovations, teRritoires (AGIR), Institut National Polytechnique (Toulouse) (Toulouse INP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Physiologie, Environnement et Génétique pour l'Animal et les Systèmes d'Elevage [Rennes] (PEGASE), Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut Agro Rennes Angers, Unité Mixte de Recherche sur l'Ecosystème Prairial - UMR (UREP), VetAgro Sup - Institut national d'enseignement supérieur et de recherche en alimentation, santé animale, sciences agronomiques et de l'environnement (VAS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Structures et Marché Agricoles, Ressources et Territoires (SMART), Agrosystèmes Biodiversifiés (UMR ABSys), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre International de Hautes Etudes Agronomiques Méditerranéennes - Institut Agronomique Méditerranéen de Montpellier (CIHEAM-IAMM), Centre International de Hautes Études Agronomiques Méditerranéennes (CIHEAM)-Centre International de Hautes Études Agronomiques Méditerranéennes (CIHEAM)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut Agro Montpellier, Unité Mixte de Recherche sur les Herbivores - UMR 1213 (UMRH), Agronomie, Direction de l'Expertise scientifique collective, de la Prospective et des Etudes, Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Institut du Développement Durable et des Relations Internationales (IDDRI), Institut d'Études Politiques [IEP] - Paris, Laboratoire Agronomie et Environnement - Antenne Colmar (LAE-Colmar ), Laboratoire Agronomie et Environnement (LAE), Université de Lorraine (UL)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université de Lorraine (UL)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Interactions Sol Plante Atmosphère (UMR ISPA), Ecole Nationale Supérieure des Sciences Agronomiques de Bordeaux-Aquitaine (Bordeaux Sciences Agro)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), This work was supported by the French National Research Institute for Agriculture, Food, and environment (INRAE), the French Agency for Ecological Transition (ADEME), and the French Ministry of Agriculture (MAA) (convention n.1660C0020). The Secure Data Access Centre (CASD) of the French Ministry of Agriculture provided access to the French Farm Accountancy Data Network (FADN) and this work was indirectly supported by a public grant of the French National Research Agency as part of the 'Investissements d'avenir' program (ANR-10-EQPX-0017, Centre d'acces securise aux donnees - CASD). Authors acknowledges support from the Horizon 2020 European Joint Programme SOIL (EJP-SOIL, grant agreement: 862695). L. Bamière, C. Chenu, N. Delame, and S. Houot acknowledges support from CLAND and benefited from the French state aid managed by the ANR under the 'Investissements d'avenir' programme with the reference ANR-16-CONV-0003., ANR-10-EQPX-0017,CASD,Développement et construction d'un Centre d'Accès Sécurisé Distant aux données confidentielles (CASD) pour la recherche française en sciences sociales et en économie.(2010), ANR-16-CONV-0003,CLAND,CLAND : Changement climatique et usage des terres(2016), and European Project: 862695,H2020,H2020-SFS-2019-1,EJP SOIL(2020)
- Subjects
Terre agricole ,P40 - Météorologie et climatologie ,F08 - Systèmes et modes de culture ,Carbone organique du sol ,Abatement cost ,[SDV.SA.AGRO]Life Sciences [q-bio]/Agricultural sciences/Agronomy ,[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study ,Greenhouse gas ,Carbon neutrality ,Climate change mitigation ,atténuation des effets du changement climatique ,JEL: Q - Agricultural and Natural Resource Economics • Environmental and Ecological Economics/Q.Q1 - Agriculture ,émission de gaz ,Coût marginal ,Agriculture ,[SDV.SA.AEP]Life Sciences [q-bio]/Agricultural sciences/Agriculture, economy and politics ,JEL: Q - Agricultural and Natural Resource Economics • Environmental and Ecological Economics/Q.Q5 - Environmental Economics/Q.Q5.Q54 - Climate • Natural Disasters and Their Management • Global Warming ,[SHS.ECO]Humanities and Social Sciences/Economics and Finance ,séquestration du carbone ,réduction des émissions ,JEL: Q - Agricultural and Natural Resource Economics • Environmental and Ecological Economics ,France ,Gaz à effet de serre ,Soil organic carbon sequestration - Abstract
International audience; Highlights:• Additional carbon storage, net GHG budget, and cost of 8 agricultural practices.• MACC shows abatement potential of 40–60 MtCO2e.yr−1 for carbon price 55–250 €.tCO2e−1.• Key practices: agroforestry, hedges, cover crops, grasslands in crop sequences.• No “one size fits all strategy” due to heterogeneity across regions and practices.• French agricultural carbon sink potential is 5 times higher than anticipated by the government.Abstract:Following the Paris agreement in 2015, the European Union (EU) set a carbon neutrality objective by 2050, and so did France. The French agricultural sector can contribute as a carbon sink through carbon storage in biomass and soil, in addition to reducing GHG emissions. The objective of this study is to quantitatively assess the additional storage potential and cost of a set of eight carbon-storing practices. The impacts of these agricultural practices on soil organic carbon storage and crop production are assessed at a very fine spatial scale, using crop and grassland models. The associated area base, GHG budget, and implementation costs are assessed and aggregated at the region level. The economic model BANCO uses this information to derive the marginal abatement cost curve for France and identify the combination of carbon storing practices that minimizes the total cost of achieving a given national net GHG mitigation target. We find that a substantial amount of carbon, 36.2 to 52.9 MtCO2e yr-1, can be stored in soil and biomass for reasonable carbon prices of 55 and 250 € tCO2e-1, respectively (corresponding to current and 2030 French carbon value for climate action), mainly by developing agroforestry and hedges, generalising cover crops, and introducing or extending temporary grasslands in crop sequences. This finding questions the 3-5 times lower target of 10 MtCO2e.yr-1 retained for the agricultural carbon sink by the French climate neutrality strategy. Overall, this would decrease total French GHG emissions by 9.2 to 13.8%, respectively (reference year 2019).; Suite aux accords de Paris en 2015, l'Union européenne (UE) s'est fixé un objectif de neutralité carbone d'ici à 2050, tout comme la France. En plus de réduire les émissions de GES, le secteur agricole français peut contribuer à la neutralité carbone en tant que puits de carbone, par le stockage de carbone dans le sol et la biomasse. L'objectif de cette étude est de quantifier le potentiel de stockage additionnel et le coût d'un ensemble de huit pratiques stockantes. Les impacts de ces pratiques agricoles sur le stockage du carbone organique du sol et les rendements des cultures sont évalués à une échelle spatiale très fine, à l'aide de modèles de cultures et de prairies. L'assiette, le bilan GES net et le coût de mise en œuvre associés à chaque pratique sont également évalués et agrégés au niveau régional. Le modèle économique BANCO utilise ces informations pour générer la courbe de coût marginal d'abattement pour la France, et identifier la combinaison de pratiques stockantes qui minimise le coût total pour atteindre un objectif national donné d'atténuation des émissions de GES nettes. Nous montrons qu'une quantité non négligeable de carbone, de 36,2 à 52,9 MtCO2e an-1, peut être stockée dans le sol et la biomasse pour des prix du carbone raisonnables de 55 et 250 € tCO2e-1, respectivement (correspondant à la "valeur de l'action pour le climat" actuelle et 2030, fixée par le gouvernement français), et cela principalement par le développement de l'agroforesterie et des haies, la généralisation des cultures intermédiaires, l'introduction ou l'extension des prairies temporaires dans les séquences de culture. Ce résultat remet en cause l'objectif 3 à 5 fois inférieur retenu pour le puits de carbone agricole (10 MtCO2e.an-1) par la stratégie nationale bas carbone. Globalement, ce stockage additionnel de carbone permettrait de réduire les émissions totales de GES de la France de 9,2 à 13,8 %, respectivement (année de référence 2019).
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- 2023
47. Terrestrial carbon removal activities, standards, certifications, and their expected durations
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Sprenkle-Hyppolite, Starry, Arcusa, S., Hagood, E., Cardinael, Rémi, Funk, J., and Roopsind, Anand
- Abstract
Carbon Dioxide Removal (CDR) is a mitigation activity that captures carbon dioxide from the atmosphere and stores it in reservoirs or products, and proof of storage is given through carbon accounting methodologies embodied in standards. We review nature- and engineering-based terrestrial CDR activities, certifications and standards and explore their expected durations. Using a mapping exercise, we find a complex ecosystem with 23 standard developing organizations certifying carbon removal from 15 different terrestrial CDR activities resulting in the availability of 17 different certification instruments. More standards exist for nature-based compared to engineering-based activities. The process revealed ambiguity on what constitutes CDR and highlights potential reforms to CDR certification. Furthermore, we conducted a literature review of the expected storage durations, risks, and process times for mineral and geologic formations, long-lived products, soil carbon, and above & belowground biomass carbon reservoir types (13 terrestrial CDR activities). We find variations in the expected storage durations that span multiple orders of magnitude between reservoir types and within estimates for the same reservoir type. We discuss the implications of the scaling of terrestrial CDR, of different durations, in relation to the Exponential Roadmap for Natural Climate Solutions and perspectives for future terrestrial carbon storage.
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- 2023
48. Sustaining maize yields and soil carbon following land clearing in the forest-savannah transition zone of West Africa: Results from a 20-year experiment
- Author
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Cardinael, Rémi, Guibert, Hervé, Kouassi Bredoumy, Soumaïla T., Gigou, Jacques, and N'Goran, Kouadio Emmanuel
- Abstract
Sustainable alternatives to slash-and-burn shifting cultivation in the (sub)humid tropics often rely on the use of external nutrient inputs to address soil fertility decline. The objective of this study was to investigate whether maize productivity and SOC can be sustained under permanent cropping with sole and combined use of compost and mineral nitrogen (N) fertilizer. Here, we report results from a long-term experiment carried out in Gagnoa, Ivory Coast, from 1971 to 1990. The experiment followed a randomized block design comprising eight replicates of 12 treatments. The two studied factors were compost (0 or 10 t DM ha−1 yr−1) and mineral N (0, 40, 80, 120, 160 or 200 kg N ha−1 yr−1) additions. Average maize grain yields of the first cropping cycles were significantly lower without compost (5.05 ± 1.57 t ha−1) than with compost addition (6.07 ± 1.31 t ha−1). The annual yield variability as shown by the standard deviation of the mean was reduced by 20% with compost addition. Without compost, 53% of the initial SOC stock in the 0–20 cm soil layer was lost, resulting in a SOC loss rate of − 0.62 t C ha−1 yr−1 compared to 21% with compost (−0.27 t C ha−1 yr−1). Compost addition therefore reduced SOC loss with an apparent SOC storage rate of 0.35 t C ha−1 yr−1. The conversion rate of organic carbon (OC) inputs to SOC was about 12%. The Introductory Carbon Balance Model (ICBM) reproduced well SOC dynamics, especially without compost. Without mineral N and without compost, maize grain yield decreased with decreasing SOC concentration until the introduction of leguminous crops in the second cropping cycle. We conclude that combined application of compost with mineral N fertilizers was effective at maintaining maize productivity but inadequate to prevent the decline of SOC stocks, despite large additions.
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- 2023
49. Don't put all your eggs in one basket: legumes diversification to improve resilience of rainfed cropping systems in sub-humid Zimbabwe
- Author
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Pret, Valentin, Couedel, Antoine, Diop, Souleymane, Affholder, François, Descheemaeker, Katrien, Chikowo, Régis, Cardinael, Rémi, and Falconnier, Gatien
- Abstract
Climate variability is predicted to increase in sub-Saharan Africa. This will impact the food security of the populations who rely on rainfed cereal production. Sustainable intensification of cropping systems aims at increasing food production while adapting to future climate and mitigating environmental impacts. The opportunity to diversify cereal-based cropping systems with legumes to increase resilience has not been quantitively assessed so far. In this study, we explored the impact of interannual climate variability for a set of cropland allocations, going from maize only to various share and number of legume crops. We explored the hypotheses that maize and legumes inter-annual performances are not correlated, so that mixing the two crops will increase the resilience of the cropland allocation. We calibrated the STICS soil-crop model for maize, cowpea, groundnut and pigeon pea, with data from on-farm trials in Murehwa district in sub-humid Zimbabwe, conducted in the 2021- 2022 and 2022-2023 growing seasons. Crop performance in terms of average yield and its variability was simulated with the calibrated crop model for the historical climate (1996-2016), on red-clay and granitic sandy soils, for more fertile homefields and less fertile outfields. Two planting dates (early-late) and three levels of fertilization (0-80-160 kg N/ha), brought by mineral fertiliser only, manure only, or by a combination of 30% manure and 70% mineral fertiliser, were investigated. The simulated crop performance was used to compute for each land allocation the agricultural productivity, the economic profitability and the environmental performance. From the on-going simulation results, we will draw critical insights on the complementarities between maize and legumes. More specifically, we expect smaller but more stable groundnut yield compared with fertilized maize, so that diversification with groundnut will increase production stability and food security in terms of proteins. With regard to crop management, we foresee that a mix of mineral and organic fertilization will limit nitrogen leaching compared with mineral fertilization only, the first strategy giving similar energy production but greater environmental performance and gross margin. Under favourable rainy seasons, early planting is expected to increase productivity of both cereals and legumes and thus land allocation resilience, while late planting might be more detrimental to the cereal. These results can help inform the current research agenda around the benefits of cereal-based systems integrating legumes and trade-offs between intensification and diversification of rainfed cropping systems in sub-Saharan Africa.
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- 2023
50. Climatic effect of no-tillage and mulch due to albedo change differs with soil type: a field study in Zimbabwe
- Author
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Diop, Souleymane, Cardinael, Rémi, Lauerwald, Ronny, Ferlicoq, Morgan, Thierfelder, Christian, Chikowo, Régis, Corbeels, Marc, and Ceschia, Eric
- Abstract
Biogeochemical effects of conservation agriculture (CA), i.e. soil organic carbon storage and greenhouse gas emissions have been investigated in numerous studies. Recent ones suggest that management practices also have significant biogeophysical impacts on local and global climate through changes in surface albedo and energy partitioning. For Africa, relevant studies are scarce. In this study, we assessed the biogeophysical effects of CA in maize fields over the 2021/22 and 2022/23 seasons at two sites established in 2013 in Zimbabwe on an abruptic Lixisol at Domboshawa Training Center (DTC) and on a xanthic Ferralsol at the University of Zimbabwe Farm (UZF). We hypothesised that CA would have different effects on albedo dynamics and radiative forcing (RF) depending on 1) the presence/absence of crop residues at soil surface, 2) soil type/colour. We monitored dynamics of albedo, longwave radiation, LAI, soil moisture/temperature under three different treatments: conventional tillage (CT), no-tillage (NT) and no-tillage with mulch (NTM). Our results showed that NT and NTM induced a RF cooling effect (higher albedo compared to CT) in the clayey soil at UZF but the mean annual RF of NT was higher than that under NTM with -0.83 W.m-2 and -0.43 W.m-2 respectively. In sandy soil (at DTC), we observed a warming effect due to the soil darkening effect induced by mulching. The mean annual RF of NT was -3.4 W.m-2 (cooling effect compare to CT treatment) against 1.2 W.m-2 for NTM (warming effect). Next step is to compare the albedo induced RF induced by NT and NTM with the other biogeophysical effects and the biogeochemical effects on climate of those treatments. These results suggest that application of mulch or crop residues on sandy soils might not be relevant for a climate change mitigation perspective, even if it provides benefits for soil health and adaptation to climate change.
- Published
- 2023
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