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Vertical Soil Profiling Using a Galvanic Contact Resistivity Scanning Approach

机译:使用电接触电阻率扫描方法进行垂直土壤剖析

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Proximal sensing of soil electromagnetic properties is widely used to map spatial land heterogeneity. The mapping instruments use galvanic contact, capacitive coupling or electromagnetic induction. Regardless of the type of instrument, the geometrical configuration between signal transmitting and receiving elements typically defines the shape of the depth response function. To assess vertical soil profiles, many modern instruments use multiple transmitter-receiver pairs. Alternatively, vertical electrical sounding can be used to measure changes in apparent soil electrical conductivity with depth at a specific location. This paper examines the possibility for the assessment of soil profiles using a dynamic surface galvanic contact resistivity scanning approach, with transmitting and receiving electrodes configured in an equatorial dipole-dipole array. An automated scanner system was developed and tested in agricultural fields with different soil profiles. While operating in the field, the distance between current injecting and measuring pairs of rolling electrodes was varied continuously from 40 to 190 cm. The preliminary evaluation included a comparison of scan results from 20 locations to shallow (less than 1.2 m deep) soil profiles and to a two-layer soil profile model defined using an electromagnetic induction instrument.
机译:对土壤电磁特性的近距离感应被广泛用于绘制空间土地异质性图。测绘仪器使用电流接触,电容耦合或电磁感应。无论仪器的类型如何,信号发送和接收元件之间的几何配置通常都会定义深度响应函数的形状。为了评估垂直土壤剖面,许多现代仪器使用了多个收发器对。或者,可以使用垂直电测深来测量特定位置的表观土壤电导率随深度的变化。本文研究了使用动态表面电接触电阻率扫描方法评估土壤剖面的可能性,发射和接收电极配置为赤道偶极-偶极阵列。开发了自动扫描仪系统,并在具有不同土壤剖面的农田中进行了测试。在现场操作时,电流注入和测量成对的滚动电极之间的距离从40到190 cm连续变化。初步评估包括将20个位置的扫描结果与浅(小于1.2 m深)土壤剖面和使用电磁感应仪定义的两层土壤剖面模型进行比较。

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