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Spatial Changes in the Distribution of Exchangeable Cations in Soils of a Forested Hilly Landscape

机译:森林丘陵景观土壤中交换性阳离子分布的空间变化

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The study quantified spatial variability in exchangeable basic cations in soils of forested hilly terrain in 2006. A transect technique was used in aligning profile pits along three physiographic units of interfluve, colluvial footslope and channel bed. Collected soil samples from the profile pits were analysed using routine and special laboratory techniques. Soil data were subjected to conventional and geostatistical analyses. Exchangeable cations varied spatially and vertically irrespective of physiographic position. Strong degree of spatial dependence was exhibited by these cations in epipedal horizons while moderate degree of spatial dependence dominated in their subsurface distribution using nugget values. Values of coefficient of variation confirm pronounced anisotropy among these attributes in their vertical distribution. Studies in exchange chemistry and other related edaphic properties using other multivariate techniques will enhance knowledge gained in this study.
机译:该研究量化了2006年森林丘陵地带土壤中可交换的碱性阳离子的空间变异性。采用横断面技术对齐沿沟渠,河床底坡和河床床这三个生理单位的剖面坑。使用常规和特殊实验室技术分析了从轮廓坑收集的土壤样品。对土壤数据进行常规和地统计分析。可交换阳离子在空间和垂直方向上均发生变化,与生理位置无关。这些阳离子在足上层位表现出强烈的空间依赖性,而使用金块值,中等程度的空间依赖性在其地下分布中占主导地位。变异系数的值证实了这些属性在垂直分布中的明显各向异性。使用其他多变量技术进行的交换化学和其他相关edaphic性质的研究,将增加本研究中获得的知识。

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