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首页> 外文期刊>Soil Science Society of America Journal >Considerations for Improving the Accuracy of Permittivity Measurement using Time Domain Reflectometry: Air-Water Calibration, Effects of Cable Length
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Considerations for Improving the Accuracy of Permittivity Measurement using Time Domain Reflectometry: Air-Water Calibration, Effects of Cable Length

机译:使用时域反射法提高介电常数测量精度的注意事项:空气-水校准,电缆长度的影响

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摘要

In a paper presented by Heimovaara (1993) a method of calibrating TDR sensors was presented using air and water. Time has moved on but time domain reflectometry (TDR) sensors are still calibrated in a number of different ways. In this article we present a rigorous investigation of the method proposed by Heimovaara and demonstrate its accuracy. We demonstrate that the placement of a starting point in any place other than the one determined using Heimovaara's method results in erroneous permittivity measurement. This will be most significant at low values of permittivity. We propose that Heimovaara's method be adopted as a standard method for calibrating TDR sensors for measuring permittivity. The discussion centers on the placement of the first time marker used to measure the signal travel time from which permittivity is measured. Our modeling results suggest that this point is slightly forward of the apex of the bump on the waveform which corresponds to the impedance increase as the wave travels from the cable into the TDR sensor head. We also demonstrate that using the apex of this bump as a starting point reference can lead to erroneous measurements of travel time in layered dielectric media. Finally we examine the use of long cables to connect sensors to the TDR. We demonstrate that the travel time in the cable changes as a function of temperature and that fixed travel time markers based on cable length cause error in the measurement of travel time. For a 2.6-m cable the error was 1.6% at 50°C, and 4.7% for a 10.3-m cable, relative to calibration at 25°C. Software that tracks the sensor head either through the impedance mismatch caused by the head or using an electrical marker eliminates this source of error.
机译:在Heimovaara(1993)发表的一篇论文中,提出了一种使用空气和水校准 TDR传感器的方法。时间已经过去,但是时域反射法(TDR)传感器仍然可以通过许多不同方式进行校准。在本文中,我们对Heimovaara 提出的方法进行了 的严格研究,并证明了其准确性。我们证明,在使用Heimovaara方法确定的起点以外的任何地方,起点的放置 都会导致错误的介电常数 测量。这在 介电常数低的情况下最为明显。我们建议采用Heimovaara的方法 作为校准用于测量 介电常数的TDR传感器的标准方法。讨论的重点是 第一次标记的放置,该标记用于测量 的信号传播时间,该时间用于测量介电常数。我们的建模结果表明 该点在波形上的凸点 的顶点稍微向前,与波传播时的阻抗增加 相对应。从电缆到TDR传感器头。 我们还演示了使用此凸点的顶点作为起始 点参考会导致错误的行程 将传感器连接到TDR。我们证明 电缆的传播时间随温度变化 ,并且基于电缆长度的固定传播时间标记会导致 错误行程时间的测量。对于2.6米电缆, 误差在50°C下为1.6%,对于10.3米电缆,其相对于校准在25°C下的 误差为4.7%。通过由磁头 引起的阻抗失配或使用电子标记来跟踪传感器 磁头的软件消除了这种错误源。

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  • 来源
    《Soil Science Society of America Journal》 |2003年第1期|62-70|共9页
  • 作者单位

    George E. Brown Jr Salinity Laboratory USDA-ARS, 450 W. Big Springs Road, Riverside, CA 92507,Jesus College, University of Oxford, Oxford OX1 3DW, UK;

    Dep. Plants, Soils and Biometeorology, Ag. Sci Building-Old Main Hill 4820, Utah State University, Logan, UT 84322S,Jesus College, University of Oxford, Oxford OX1 3DW, UK;

    The Institute of Soil, Water and Environmental Science, (ARO) The Volcani Center, Bet Dagan, Israel,Jesus College, University of Oxford, Oxford OX1 3DW, UK;

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