Modelling CO2 and N2O emissions from soils in silvopastoral systems of the West African Sahelian band

Yélognissè Agbohessou, C. Delon, M. Grippa, Eric Mougin, D. Ngom, E. Gaglo, Ousmane Ndiaye, Paulo Salgado, O. Roupsard
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Abstract

Abstract. Silvopastoral systems (SPSs) have been shown to improve ecosystem resilience and provide sustainable land management solutions in the Sahel. However, accurately estimating the contribution of Sahelian ecosystems to the overall greenhouse gas (GHG) balance is a challenge, in particular regarding the magnitude of carbon dioxide (CO2) and nitrous oxide (N2O) emissions from soils. In this work, we spatialized and applied the process-based model Sahelian Transpiration Evaporation and Productivity – GENeral model of litter DEComposition – N2O (STEP–GENDEC-N2O) to investigate the magnitude and spatial and temporal patterns of herbaceous mass, as well as CO2 and N2O emissions from soil (not net emissions) in Sahelian SPSs. Our results show that over the last decade (2012–2022), there was a heterogeneous spatial distribution of herbaceous mass production and of soil CO2 and N2O emissions in Sahelian SPSs. Spatial variations in soil CO2 emissions are primarily controlled by soil carbon content, temperature, herbaceous mass, and animal load, while soil nitrogen content, soil water content, and animal load are the main factors driving the spatial variations in N2O emissions from soil. The estimated CO2 and N2O emissions from soil in Sahelian SPSs over the 2012–2022 period were equal to 58.79 ± 4.83 Tg CO2-C yr−1 (1 Tg = 1012 g) and 21.59 ± 3.91 Gg N2O-N yr−1 (1 Gg = 109 g), respectively. These values are generally lower than estimates reported in the literature for tropical areas and croplands. Furthermore, our simulations indicated a significant annual rising trend of soil CO2 and N2O emissions between 2012 and 2020 as herbaceous mass increased, making more C and N available for the nitrification, denitrification, and decomposition processes. By mapping soil CO2 and N2O emissions, we provide crucial insights into the localization of emission hotspots in Sahelian SPSs, thereby offering valuable information that can be used to devise and implement effective strategies aimed at fostering carbon sequestration in the Sahel.
西非萨赫勒地带林牧系统土壤二氧化碳和一氧化二氮排放建模
摘要事实证明,在萨赫勒地区,林牧系统(SPSs)可提高生态系统的恢复能力,并提供可持续的土地管理解决方案。然而,准确估算萨赫勒生态系统对整个温室气体(GHG)平衡的贡献是一项挑战,尤其是土壤中二氧化碳(CO2)和氧化亚氮(N2O)的排放量。在这项工作中,我们将基于过程的萨赫勒蒸腾蒸发和生产力模型--枯落物分解基因模型--N2O(STEP-GENDEC-N2O)空间化并加以应用,以研究萨赫勒SPS中草本植物质量的大小和时空模式,以及土壤中二氧化碳和一氧化二氮的排放量(非净排放量)。我们的研究结果表明,在过去十年(2012-2022 年)中,萨赫勒小流域的草本植物产量以及土壤二氧化碳和一氧化二氮排放量的空间分布是不均匀的。土壤二氧化碳排放量的空间变化主要受土壤含碳量、温度、草本植物质量和动物负荷的控制,而土壤含氮量、土壤含水量和动物负荷是驱动土壤一氧化二氮排放量空间变化的主要因素。据估计,2012-2022 年期间萨赫勒小流域土壤的二氧化碳和一氧化二氮排放量分别为:58.79 ± 4.83 Tg CO2-C yr-1(1 Tg = 1012 g)和 21.59 ± 3.91 Gg N2O-N yr-1(1 Gg = 109 g)。这些数值总体上低于文献报道的热带地区和耕地的估计值。此外,我们的模拟结果表明,2012 年至 2020 年期间,随着草本植物数量的增加,土壤二氧化碳和一氧化二氮排放量呈显著的逐年上升趋势,从而使更多的碳和氮可用于硝化、反硝化和分解过程。通过绘制土壤二氧化碳和一氧化二氮排放图,我们对萨赫勒地区SPSs排放热点的定位有了重要的认识,从而提供了宝贵的信息,可用于制定和实施旨在促进萨赫勒地区碳固存的有效战略。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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