Time extraction method for time domain reflectometry measurements

Mangesh Gurav, S. Sarik, M. Baghini
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引用次数: 1

Abstract

Determination and monitoring of moisture content in the soil is a requirement in many agricultural and civil engineering applications. Time domain reflectometry (TDR) is a well-known technique for its accuracy and applicability in the field. A typical TDR system consists of three units: A signal generation unit, a signal acquisition and encoding/decoding unit and a signal processing unit. The signal generation unit sends the electromagnetic waves in the form of pulses on a transmission line (probe), inserted in the soil. Based on the traveling time of the wave along the probe and characteristics of the reflected waves the dielectric constant of the soil is derived. This moisture content of soil is related to the dielectric constant using Topp's equation. Several TDR waveform interpretation methods have been reported. Though, many reported methods process the entire cycle of the TDR signal, the useful information is only available in 10-20% of the signal period, called the region of interest (ROI). Some of the methods extract this ROI manually. Some existing method describe the results by analyzing a single pulse of the TDR signal. This can lead to erroneous results as the single pulse may have been corrupted by either internal or external noise or by the jitter of the sampling clock. This paper presents a TDR waveform interpretation method. In this method, the ROI of 20 cycles is calculated automatically and averaged with the proper averaging technique. To study the effect of non-linearities added by the system on the TDR signal we have modeled the signal acquisition and encoding/decoding unit. We have also presented an error detection technique to detect the corrupted regions of a captured signal. The error detection technique is able to detect error level as low as 0.2% in the signal. The model has been tested with real TDR signals transmitted through air and water and then captured on a sampling oscilloscope, with different jitter levels and different number of bits in DAC. The TDR waveform interpretation method has been tested successfully with 5 different materials.
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时域反射测量的时间提取方法
测定和监测土壤中的水分含量是许多农业和土木工程应用的要求。时域反射法(TDR)以其精度和适用性而闻名于世。典型的TDR系统由三个单元组成:信号产生单元、信号采集和编码/解码单元以及信号处理单元。信号产生装置通过插入土壤的传输线(探头)以脉冲的形式发送电磁波。根据波沿探针的传播时间和反射波的特性,导出了土壤的介电常数。根据托普方程,土壤的水分含量与介电常数有关。已经报道了几种TDR波形解释方法。虽然,许多报道的方法处理TDR信号的整个周期,但有用的信息仅在10-20%的信号周期内可用,称为感兴趣区域(ROI)。有些方法手动提取ROI。现有的一些方法通过分析TDR信号的单个脉冲来描述结果。这可能导致错误的结果,因为单个脉冲可能被内部或外部噪声或采样时钟的抖动损坏。本文提出了一种TDR波形解释方法。该方法自动计算20个周期的ROI,并采用适当的平均技术进行平均。为了研究系统所增加的非线性对TDR信号的影响,我们对信号采集和编解码单元进行了建模。我们还提出了一种错误检测技术来检测捕获信号的损坏区域。误差检测技术能够检测到信号中低至0.2%的误差水平。该模型通过空气和水传输的真实TDR信号进行了测试,然后在采样示波器上捕获了不同抖动电平和DAC中不同位数的TDR信号。TDR波形解释方法已在5种不同的材料上进行了成功的测试。
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