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Soil penetration resistance analysis by multivariate and geostatistical methods

机译:多元和地统计方法土壤渗透性分析

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The penetration resistance (PR) is a soil attribute that allows identifies areas with restrictions due to compaction, which results in mechanical impedance for root growth and reduced crop yield. The aim of this study was to characterize the PR of an agricultural soil by geostatistical and multivariate analysis. Sampling was done randomly in 90 points up to 0.60 m depth. It was determined spatial distribution models of PR, and defined areas with mechanical impedance for roots growth. The PR showed a random distribution to 0.55 and 0.60 m depth. PR in other depths analyzed showed spatial dependence, with adjustments to exponential and spherical models. The cluster analysis that considered sampling points allowed establishing areas with compaction problem identified in the maps by kriging interpolation. The analysis with main components identified three soil layers, where the middle layer showed the highest values of PR.
机译:渗透性(PR)是一种土地属性,允许识别由于压实而具有限制的区域,这导致机械阻抗进行根生长和减少的作物产量。本研究的目的是通过地统计和多变量分析表征农业土壤的公关。取样随机完成,在90点到0.60米深度。它是确定PR的空间分布模型,以及具有机械阻抗的定义区域,用于根生长。 PR显示随机分布至0.55和0.60米深度。在其他深度中分析出现空间依赖,调整指数和球形模型。群集分析,考虑采样点允许通过Kriging插值在地图中标识的压缩问题建立区域。主要成分的分析确定了三层土层,其中中间层显示了Pr的最高值。

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