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Documenting GlobalSoilMap.net grid cells from legacy measured soil profile and global available covariates in Northern Tunisia

机译:记录Globalsoilmap.net从遗留测量的土壤剖面和突尼斯北部的全球可用协变量

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In many regions of the planet, GlobalSoilMap.net grid cells can only be documented by Digital soil mapping (DSM) procedures using sparse sets of legacy measured soil profiles and landscape covariates available at the global level. This study aimed to test a DSM methodology for mapping from such an input, in the Cap Bon Region, northern Tunisia (2822 km~2), the soil properties according to the GlobalSoilMap.net specifications. Best possible maps of six primary soil properties at six intervals of depth were produced by selecting and applying, for each of the targeted soil properties, an appropriate DSM function among three candidates (linear regression, ordinary kriging and regression kriging). The selection was made from decision criteria that resulted from an exploratory analysis involving statistical tests. Only a small part of soil variability of the study area could be captured and it was at best obtained a decrease of one third of the widths of the 95% confidence intervals that expressed a prediction of soil property. These results could be explained by the low rate of variability of some properties and the predominance of short scale variations that could not be modeled from the sparse set of profiles. The merit of such a DSM approach is to identify the gaps that needs to be filled to provide data that will meet higher expectations, outlying the need for more investment in soil data.
机译:在地球的许多地区,GlobalSOILMAP.NET网格单元只能通过数字土壤映射(DSM)程序记录,使用稀疏的遗产测量的土壤剖面和全球水平可用的景观协变量。本研究旨在从这样的输入测试映射DSM方法,在卡本半岛地区,北方突尼斯(2822公里〜2),根据GlobalSoilMap.net规格土壤性质。通过选择和施加六个深度间隔的六个主要土壤性质的最佳地图是通过选择和施加的每种靶向土壤性质,在三个候选物中适当的DSM功能(线性回归,普通克里格汀和回归克里格)。选择是由决策标准制成的,该标准由涉及统计测试的探索性分析。只能捕获研究区域的土壤变异性的一小部分土壤变异性,并且最多只获得了表达土壤性质预测的95%置信区间宽度的三分之一的减少。这些结果可以通过一些属性的低可变性率和短尺度变化的优势来解释,这是无法从稀疏的曲线集合模拟的短尺度变化。这种DSM方法的优点是识别需要填补的差距,以提供将满足更高期望的数据,偏远偏离土壤数据的更多投资。

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