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Using Soil Apparent Electrical Conductivity to Optimize Sampling of Soil Penetration Resistance and to Improve the Estimations of Spatial Patterns of Soil Compaction

机译:利用土壤表观电导率优化土壤渗透性采样并改善土壤压实的空间格局估算

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摘要

This study presents a combined application of an EM38DD for assessing soil apparent electrical conductivity (ECa) and a dual-sensor vertical penetrometer Veris-3000 for measuring soil electrical conductivity (ECveris) and soil resistance to penetration (PR). The measurements were made at a 6 ha field cropped with forage maize under no-tillage after sowing and located in Northwestern Spain. The objective was to use data from ECa for improving the estimation of soil PR. First, data of ECa were used to determine the optimized sampling scheme of the soil PR in 40 points. Then, correlation analysis showed a significant negative relationship between soil PR and ECa, ranging from −0.36 to −0.70 for the studied soil layers. The spatial dependence of soil PR was best described by spherical models in most soil layers. However, below 0.50 m the spatial pattern of soil PR showed pure nugget effect, which could be due to the limited number of PR data used in these layers as the values of this parameter often were above the range measured by our equipment (5.5 MPa). The use of ECa as secondary variable slightly improved the estimation of PR by universal cokriging, when compared with kriging.
机译:这项研究提出了一种用于评估土壤表观电导率(ECa)的EM38DD和一种用于测量土壤电导率(ECveris)和土壤抗渗透性(PR)的双传感器垂直渗透仪Veris-3000的组合应用。测量是在西班牙西北部一个6公顷的田地上进行的,该田地播种后没有耕种的饲用玉米。目的是使用来自ECa的数据来改善土壤PR的估算。首先,使用ECa数据确定40个土壤PR的最佳采样方案。然后,相关分析表明,土壤PR与ECa之间存在显着的负相关关系,对于所研究的土壤层而言,其范围从-0.36至-0.70。在大多数土壤层中,球形模型最好地描述了土壤PR的空间依赖性。但是,低于0.50 m时,土壤PR的空间格局显示出纯金块效应,这可能是由于这些层中使用的PR数据数量有限,因为此参数的值通常高于我们的设备所测量的范围(5.5 MPa) 。与克里金法相比,将ECa用作次要变量可以稍微改善通过通用共克里金法估算的PR。

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