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Mapping soils using the fuzzy approach and regression-kriging case study from the Pova?sky Inovec Mountains, Slovakia

机译:使用模糊方法对土壤进行制图并从斯洛伐克Pova?sky Inovec山脉进行回归克里格案例研究

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The paper introduces a method of digital mapping of spatial distribution of soil typological units. It implements fuzzy k-means to classify the soil profile data (study area from the Pova?sky Inovec Mountains, Slovakia) and regression-kriging with the selected digital terrain and remote sensing data to draw membership maps of soil typological units. Totally three soil typological units were identified: Haplic Cambisols (Skeletic, Dystric), Albic Stagnic Luvisols, and Haplic Stagnosols (Albic, Dystric). We analysed the membership values to these units with respect to terrain and remote sensing data. The membership values appeared as spatially smoothly dependant on the terrain gradients (linearly or exponentially) whereas the residua showed spatial autocorrelation. Based on regression and kriging analyses, the regression-kriging model was successfully deployed to draw raster membership maps. These maps yield coefficients of determination between R2 = 56% (Albic Stagnic Luvisols) to R2= 79% (Haplic Cambisols (Skeletic, Dystric)) when evaluated by cross validation. The grid-based continuous soil map represents an alternative to the classical polygon soil maps and can offer a wide range of interpretations for landscape studies.
机译:介绍了土壤类型学单位空间分布的数字制图方法。它执行模糊k均值以对土壤剖面数据(来自斯洛伐克Pova?sky Inovec山脉的研究区域)进行分类,并使用选定的数字地形和遥感数据进行回归克里格法绘制土壤类型学单元的隶属关系图。总共确定了三个土壤类型学单元:Haplic Cambisols(Skeletic,Dystric),Albic Stagnic Luvisols和Haplic Stagnosols(Albic,Dystric)。我们针对地形和遥感数据分析了这些单位的隶属度值。隶属度值显示为在空间上平滑地取决于地形梯度(线性或指数),而残差则显示出空间自相关。基于回归和克里格分析,成功地使用了回归克里格模型绘制栅格成员图。这些图通过交叉评估时得出R 2 = 56%(Albic Stagnic Luvisols)到R 2 = 79%(Haplic Cambisols(Skeletic,Dystric))的测定系数验证。基于网格的连续土壤图代表了经典多边形土壤图的替代方法,可以为景观研究提供广泛的解释。

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