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Simulation and prediction of soil organic carbon spatial change in arable lands based on DNDC model

机译:基于DNDC模型的耕地土壤有机碳空间变化的仿真与预测

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Soil organic carbon (SOC) change not only affects soil fertility and productivity, but also plays an important role to clarify the potential for regional soil carbon sequestration and the impact of global climate change. The method of predicting the SOC trends based on model is superior to methods of long-term experiment and soil sample collecting on the time scale. Because of the spatial and regional variability of climate, soil and farming system, SOC change simulation and prediction on the spatial scale has defect in terms of regional representation and simulation accuracy if using several points or county as modeling unit. In order to improve the accuracy of SOC change prediction on regional and spatial scale, this study simulated the effects of 4 fertilizer application treatments of past 16 years (1990–2005) on SOC change based on DNDC model using data from the long-term experiment station of Gongzhuling of Jilin province in China, and validated the DNDC model. Then the modeling units of Jilin province was divided according to the spatial variability characteristics of climate, soil by using geographic information system (GIS) technology. SOC spatial change trends of Jilin in next 60 years (2011–2070) were simulated and predicted by 3 kinds of scenarios designation on future climate changes (climate repeat, Precis B2 and Precis A2) and spring corn planning. The results showed: (1) DNDC model can be used for SOC simulation and predictions for the study area. The root mean square error (RMSE) were less than 10% comparing SOC measured values to simulated values for 4 fertilizer application treatments. (2) SOC spatial changes simulation and prediction of Jilin based on DNDC model indicated that 60% areas of arable land SOC trended to increase from 2011–2070 under the scenario of climate repeat and spring corn plant, 28% trended to decrease. Under the climate scenario of Precis A2, the area of SOC increase and decrease kept balance. Under th- climate scenario of Precis B2, 60% areas of arable land SOC trended to decrease. (3) Under modeling units division by using spatial heterogeneity of climate and soil, the results of SOC simulation and prediction in regional scale are more reasonable as opposed to a few typical points or the county unit as modeling unit.
机译:土壤有机碳(SOC)变化不仅影响土壤肥力和生产力,而且还发挥着重要作用,以澄清区域土壤碳封存的潜力和全球气候变化的影响。基于模型预测SOC趋势的方法优于时间尺度的长期实验和土壤样品的方法。由于气候的空间和区域变异,土壤和农业系统的可变性,如果使用几个点或县作为建模单元,则空间尺度的SOC变化模拟和空间尺度的预测具有缺陷。为了提高区域和空间尺度对SoC变化预测的准确性,本研究模拟了使用来自长期实验的数据的DNDC模型对过去16岁(1990-2005)对SoC变化的影响的影响中国吉林省公区的驻地,验证了DNDC模型。然后,吉林省建模单位根据气候变化特征,采用地理信息系统(GIS)技术分割。在未来气候变化的3种情景指定(气候重复,Precis B2和Precis A2)和春季玉米规划中,模拟并预测了吉林的SoC空间变化趋势(2011-2070)的模拟和预测。结果显示:(1)DNDC模型可用于研究区域的SOC模拟和预测。均方根误差(RMSE)小于10%,将SOC测量值与模拟值进行比较,以进行4种肥料应用处理。 (2)基于DNDC模型的吉林的SoC空间变化模拟与预测表明,耕地SoC的60%面积从2011 - 2070年在气候重复和春玉米厂的情况下增加,28%趋势减少。根据PRECIS A2的气候情景,SOC的面积增加和减少保持平衡。根据PRECIS B2的气候情景,耕地SOC的60%地区趋势下降。 (3)根据使用气候和土壤的空间异质性在建模单元划分中,SoC模拟和区域规模预测的结果更合理,而不是几个典型点或县单位作为建模单元。

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