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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Spatially-explicit regional-scale prediction of soil organic carbon stocks in cropland using environmental variables and mixed model approaches
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Spatially-explicit regional-scale prediction of soil organic carbon stocks in cropland using environmental variables and mixed model approaches

机译:利用环境变量和混合模型方法对农田土壤有机碳储量进行空间明晰的区域尺度预测

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摘要

The effects of soil redistribution on the carbon (C) cycle and the need for spatially and depth-explicit C estimates at large scales have recently been receiving growing attention. In eroding agricultural landscapes, C gets transported from erosional to depositional landscape elements forming a heterogeneous pattern in quantity and quality of the distributed carbon. At present, methods and research to characterize this horizontal and vertical variability are either limited to local slope scales or, if applied to larger scales, to surface soil horizons with large uncertainties when extrapolated to deeper layers. In this study, we used soil profile data collected in two zones of differing soil texture (loam and clay-rich soils) in Luxembourg, to calibrate a linear mixed-effect model to predict the 3D soil C stock distribution on a regional scale for cropping systems using a set of spatially-explicit hydrologic, climatic, pedologic and geomorphologic variables. We demonstrate that due to a high spatial variability of C stocks it is mandatory to consider various environmental processes to predict C accurately on a regional scale, especially in deeper soil layers, and to avoid simple depth extrapolation of topsoil C data as has been done earlier in flat landscapes. Using estimates of topsoil C contents derived from hyperspectral remote sensing, we predict spatial patterns of C stocks for cropland on a regional scale and provide new insights into the spatial heterogeneity of soil C storage covering a large area. The variability of C stocks in the two texture zones expressed as values larger or smaller than the mean +/- standard deviation is hereby lower in the loam zone (26.2%) than in the clay zone (38.7%). We estimate a mean C stock (to 100 cm soil depth) of 9.4 +/- 3.1 kg/m(2) for the clay-rich soils and 11.3 +/- 2.4 kg/m(2) for loamy soils. This represents the first regional estimate for C stocks for the research area using continuous spatial explicit datasets
机译:最近,土壤重新分布对碳(C)循环的影响以及对空间和深度显式碳估算的需求日益受到关注。在侵蚀农业景观时,碳从侵蚀景观元素迁移到沉积景观元素,从而在分布碳的数量和质量上形成了异质的格局。目前,表征这种水平和垂直变化的方法和研究仅限于局部坡度尺度,或者如果应用于较大尺度,则只能推断出具有较大不确定性的地表土壤层,如果将其外推至较深层。在这项研究中,我们使用了在卢森堡不同土壤质地的两个区域(壤土和富含粘土的土壤)中收集的土壤剖面数据,以校准线性混合效应模型,以预测作物种植区域规模上的3D土壤C储量分布。系统使用一组空间上明确的水文,气候,生态和地貌变量。我们证明,由于碳储量的高度空间变异性,必须考虑各种环境过程以在区域范围内准确预测碳,尤其是在较深的土壤层中,并避免像以前所做的那样简单地对表土碳数据进行深度推断在平坦的风景。利用从高光谱遥感获得的表层土壤碳含量的估算,我们可以预测区域范围内农田的碳储量的空间格局,并对覆盖大面积土壤碳储量的空间异质性提供新的见解。在两个纹理区域中,C储量的变异性表示为大于或小于平均+/-标准偏差的值,因此在壤土区域(26.2%)比粘土区域(38.7%)低。我们估计富含粘土的土壤的平均碳储量(至100 cm土壤深度)为9.4 +/- 3.1 kg / m(2),而壤土的碳储量为11.3 +/- 2.4 kg / m(2)。这是使用连续空间显式数据集的研究区域C储量的第一个区域估计

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