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2.10.4: Time Domain Reflectometry

  • Page ID
    44339
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    One soil water measurement technique that takes advantage of the fact that a soil's apparent dielectric permittivity (εa) is dependent on θv is time domain reflectometry (TDR). TDR requires the placement of two parallel rods (wave guides) into the soil. An electromagnetic wave is pulsed along the wave guides. The reflected signal from the tip of the wave guide is captured with a fast oscilloscope, recording voltage as a function of time. The travel time of the recorded wave must be calculated with a graphical interpretation of the waveform (with software) as part of the TDR method (Evett, 2007). The travel time provides a direct measurement of εa. The wave will travel faster in a dry soil than in a wet soil, with a lower travel time and a lower εa. The εa is comprised of the permittivity of the water, the permittivity of the soil, and the permittivity of air, and the water has a much larger influence on εa than the soil or air. Therefore, εa is directly proportional to θv. Because of the strong correlation between εa and θv, TDR is an accurate method for sensing θv (within 2%). Its use was initially limited to research due to high costs, but ongoing technology development is reducing the price of TDR sensors. It has the advantage of not using a radioactive source, so licensing is not required. The measurement volume is approximately cylindrical and is dependent on the length of the rods and the spacing between rods. The diameter of the cylinder is about 1.5 times the spacing between rods.

    Figure 2.16. Calibration curve for a neutron probe.

    callibrationCurve.jpg

    Scatterplot and corresponding linear regression equation for measured volumetric water content (dependent variable) and neutron probe measurement (independent variable). The neutron probe measurement is expressed as the count ratio (soil count divided by standard count)


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