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A map of the top-soil organic carbon content of Europe generated by a generalized additive model

机译:广义添加剂模型生成的欧洲表层土壤有机碳含量图

摘要

There is an increasing demand for up-to-date soil organic carbon (OC) data for global environmental andclimatic modelling. The aim of this study was to create a map of topsoil OC content at the European scaleAQ4 by applying digital soil mapping techniques to the first European harmonized geo-referenced topsoil (0–20 cm)database, which arises from the Land use/Cover Area Frame statistical Survey (LUCAS). A map of the associateduncertainty was also produced to support careful use of the predicted OC contents. A generalized additive model(GAM) was fitted on 85% of the dataset (R2 =0.29), using OC content as dependent variable; a backward stepwiseapproach selected slope, land cover, temperature, net primary productivity, latitude and longitude as suitablecovariates. The validation of the model (performed on 15% of the data-set) gave an overall R2 of 0.27 and an R2of 0.21 for mineral soils and 0.06 for organic soils. Organic C content in most organic soils was under-predicted,probably because of the imposed unimodal distribution of our model, whose mean is tilted towards the prevalentmineral soils. This was also confirmed by the poor prediction in Scandinavia (where organic soils are morefrequent), which gave an R2 of 0.09, whilst the prediction performance (R2) in non-Scandinavian countries was0.28. The map of predicted OC content had the smallest values in Mediterranean countries and in croplands acrossEurope, whereas largest OC contents were predicted in wetlands, woodlands and mountainous areas. The mapof the predictions’ standard error had large uncertainty in northern latitudes, wetlands, moors and heathlands,whereas small uncertainty was mostly found in croplands. The map produced gives the most updated generalpicture of topsoil OC content at the European Union scale.
机译:对用于全球环境和气候建模的最新土壤有机碳(OC)数据的需求不断增长。这项研究的目的是通过将数字土壤测绘技术应用到第一个欧洲统一的地理参考表土(0-20厘米)数据库中来创建欧洲规模AQ4的表层土壤OC含量图,该数据库来自土地利用/覆盖面积框架统计调查(LUCAS)。还绘制了相关不确定性的地图,以支持谨慎使用预测的OC含量。使用OC含量作为因变量,对数据集的85%拟合了通用加性模型(GAM)(R2 = 0.29);向后逐步选择选定的坡度,土地覆被,温度,净初级生产力,纬度和经度作为合适的协变量。模型的验证(在数据集的15%上执行)得出,矿质土壤的总体R2为0.27,R2为0.21,有机土壤的R2为0.06。大多数有机土壤中的有机碳含量被低估了,这可能是因为我们模型强加了单峰分布,其均值向普遍的矿质土壤倾斜。斯堪的纳维亚半岛(有机土壤较常见)的预测不佳也证实了这一点,R2为0.09,而非斯堪的纳维亚国家的预测表现为(R2)为0.28。在地中海国家和整个欧洲的农田中,预测的OC含量图的值最小,而在湿地,林地和山区中预测的OC含量最大。预测的标准误差图在北部纬度,湿地,沼泽和荒地中具有较大的不确定性,而在农田中则存在较小的不确定性。生成的地图提供了欧盟范围内表层土壤中OC含量的最新概况。

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