# Interaction between soil type and cropping system on albedo dynamics leads to contrasted impact on climate mitigation

Souleymane Diop, Rémi Cardinael, Ronny Lauerwald, Morgan Ferlicoq, Christian Thierfelder, Régis Chikowo, Marc Corbeels, Eric Ceschia

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## ► To cite this version:

Souleymane Diop, Rémi Cardinael, Ronny Lauerwald, Morgan Ferlicoq, Christian Thierfelder, et al. Interaction between soil type and cropping system on albedo dynamics leads to contrasted impact on climate mitigation. EGU General Assembly 2024, EGU, Apr 2024, Vienne, Austria. 1 p., 10.5194/egusphere-egu24-6466. hal-05181912

HAL Id: hal-05181912

https://hal.science/hal-05181912v1

Submitted on 23 Jul 2025

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Interaction between soil type and cropping system on albedo
dynamics leads to contrasted impact on climate mitigation

Souleymane Diop<fnref n="1" />,<fnref n="2" />,<fnref n="3" />, Rémi Cardinalel<fnref n="3" />,<fnref n="4" />,<fnref n="5" />, Ronny Lauerwald<fnref n="1" />, Morgan Ferlicoq<fnref n="2" />, Christian Thierfelder<fnref n="6" />, Regis Chikowo<fnref n="5" />,<fnref n="7" />, Marc Corbeels<fnref n="4" />,<fnref n="8" />, and Eric Ceschia<fnref n="2" />

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), no-tillage (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⁻<fnref n="2" /> and -0.43 W.m⁻<fnref n="2" /> respectively, while during the second season (2022/23) the annual mean RF was -1.43 W.m⁻<fnref n="2" /> for NT and -1.03 W.m⁻<fnref n="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⁻<fnref n="2" /> during the first season and -2.78 W.m⁻<fnref n="2" /> during the second. In contrast, NTM showed a warming effect with an RF of 1.2 W.m⁻<fnref n="2" /> in 2021/22, and 2.77 W.m⁻<fnref n="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 of the same magnitude between albedo and soil organic carbon (SOC) in the NT and NTM treatments at DTC, suggesting that CA might not bring any mitigation benefit if mulch is applied on light coloured soils.

<footnote n="1">¹Université Paris-Saclay, INRAE, AgroParisTech, UMR EcoSys, Palaiseau, France (souleymane.diop@agroparistech.fr)</footnote>

<footnote n="2">²CESBIO-Univ. Toulouse III/CNRS/CNES/IRD/INRAE 18, avenue, Edouard Belin, bpi 2801, 31401 Toulouse Cedex 9, France</footnote>

<footnote n="3">³CIRAD, UPR AIDA, Harare, Zimbabwe</footnote>

<footnote n="4">⁴AIDA, Univ. Montpellier, CIRAD, Montpellier, France</footnote>

<footnote n="5">⁵Department of Plant Production Sciences and Technologies, University of Zimbabwe, Harare, Zimbabwe</footnote>

<footnote n="6">⁶International Maize and Wheat Improvement Center (CIMMYT), P.O. Box MP 163, Mount Pleasant, Harare, Zimbabwe</footnote>

<footnote n="7">⁷Plant, Soil and Microbial Sciences Department, Michigan State University, East Lansing, MI 48824, USA</footnote>

<footnote n="8">⁸IITA, International Institute of Tropical Agriculture, PO Box 30772, Nairobi 00100, Kenya</footnote>
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