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Projected loss of soil organic carbon in temperate agricultural soils in the 21st century: effects of climate change and carbon input trends

机译:预计21世纪温带农业土壤中有机碳的损失:气候变化和碳输入趋势的影响

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摘要

Climate change and stagnating crop yields may cause a decline of SOC stocks in agricultural soils leading to considerable CO2 emissions and reduced agricultural productivity. Regional model-based SOC projections are needed to evaluate these potential risks. In this study, we simulated the future SOC development in cropland and grassland soils of Bavaria in the 21st century. Soils from 51 study sites representing the most important soil classes of Central Europe were fractionated and derived SOC pools were used to initialize the RothC soil carbon model. For each site, long-term C inputs were determined using the C allocation method. Model runs were performed for three different C input scenarios as a realistic range of projected yield development. Our modelling approach revealed substantial SOC decreases of 11–16% under an expected mean temperature increase of 3.3 °C assuming unchanged C inputs. For the scenario of 20% reduced C inputs, agricultural SOC stocks are projected to decline by 19–24%. Remarkably, even the optimistic scenario of 20% increased C inputs led to SOC decreases of 3–8%. Projected SOC changes largely differed among investigated soil classes. Our results indicated that C inputs have to increase by 29% to maintain present SOC stocks in agricultural soils.
机译:气候变化和作物单产停滞可能导致农业土壤中SOC数量下降,从而导致大量CO2排放并降低农业生产率。需要基于区域模型的SOC预测来评估这些潜在风险。在这项研究中,我们模拟了21世纪巴伐利亚州农田和草地土壤中SOC的未来发展。对代表中欧最重要土壤类别的51个研究地点的土壤进行了分级,并使用衍生的SOC库初始化RothC土壤碳模型。对于每个站点,使用C分配方法确定长期C输入。针对三种不同的C输入方案执行了模型运行,这是预计的产量发展的实际范围。我们的建模方法表明,假设C输入不变,在预期平均温度升高3.3 C的情况下,SOC会大幅降低11-16%。在碳输入减少20%的情况下,预计农业SOC存量将减少19-24%。值得注意的是,即使乐观的设想是增加20%的C输入量,也会导致SOC降低3–8%。预计的SOC变化在调查的土壤类别之间差异很大。我们的结果表明,碳投入必须增加29%,才能维持当前农业土壤中的SOC存量。

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