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Accounting for long-term soil fertility effects when assessing the climate impact of crop cultivation

机译:评估作物培养气候影响时的长期土壤肥力效应

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摘要

Soil organic carbon (SOC) dynamics influence the climate impact of crop cultivation, both through affecting net carbon exchange between the soil and the atmosphere and through affecting soil fertility. Higher soil fertility can enhance yield, and consequently make more plant residues available for carbon sequestration in the soil. This feedback mechanism between SOC and yield is commonly not included when assessing the environmental impact of crop production using system analysis tools like life cycle assessment (LCA). Therefore, this study developed a modelling framework where the SOC-yield feedback mechanism is included in climate impact assessment of crop cultivation, and which could be applied in LCAs. The framework was constructed by combining a model for SOC dynamics, yield response to SOC changes in a Swedish long-term field experiment and climate impact assessment. The framework employs a dynamic approach, with a time-distributed emissions inventory and a time-dependent climate impact assessment model, complemented by the most common climate metric, global warming potential (GWP). A case study applying the framework to barley cultivation was performed to explore the quantitative effect of including the feedback mechanism on the calculated climate impact. The case study involved simulating a fertiliser-induced 10% yield increase during one year and assessing the climate impact over 60 years. In this specific case, the effect of solely including SOC dynamics without the yield response to SOC decreased climate impact per kg barley by about three-fold more than only accounting for the 10% temporary yield increase. When the feedback mechanism was included, the estimated climate impact decreased five-fold more than when SOC changes were not included. These results show that SOC changes can affect the climate impact of cultivation, not only through affecting net CO2 exchanges between soil and atmosphere, as previously acknowledged by other studies, but also through changing the system performance. The quantitative results obtained in this study show that this could be an important aspect to include in order to avoid introducing systematic error when assessing the long-term climate impact of crop management changes that affect yield or SOC dynamics.
机译:土壤有机碳(SOC)动力学影响作物培养的气候影响,无论是通过影响土壤和大气之间的净碳交换,通过影响土壤肥力。土壤肥力较高可提高产量,因此制造更多的植物残留物可用于土壤中的碳封存。在使用寿命周期评估(LCA)等系统分析工具评估作物生产的环境影响时,SoC和产量之间的这种反馈机制通常不包括在内。因此,本研究开发了一种建模框架,其中SoC-产量反馈机制包括在气候影响评估作物培养中,可应用于LCAS。该框架是通过组合SOC动态的模型来构建的,在瑞典的长期现场实验和气候影响评估中对SoC变化的产生响应。该框架采用动态方法,具有时间分布式排放库存和时间依赖的气候影响评估模型,由最常见的气候公制,全球变暖潜力(GWP)补充。采用将框架应用于大麦培养的案例研究,探讨包括对计算的气候影响的反馈机制的定量效果。案例研究涉及模拟肥料诱导的肥料10%的产量增加,并评估了60多年的气候影响。在这种特定情况下,仅包括SoC动态的效果,没有对SoC的产量反应,每千克大麦的气候影响降低了大约三倍,而不是仅占10%临时产量增加。当包括反馈机制时,估计的气候影响比不包括SOC变化时减少五倍。这些结果表明,SOC变化可能影响培养的气候影响,而不仅通过影响土壤和大气之间的净二氧化碳交换,如前所述,还通过改变系统性能。本研究中获得的定量结果表明,这可能是包括在评估影响产量或SOC动态的作物管理变化的长期气候影响时避免引入系统误差的重要方面。

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