Researchers have developed a numerical model for simulating the waveform in soil by using Time Domain Reflectometry (TDR) and a new calibration equation. The results are published in the May/June issue of Soil Science Society of America Journal. Chih-Ping Lin, assistant professor of civil engineering, was the lead scientist on the research, conducted from 1999 to 2001 with support from the National Science Council, Taiwan.
"The TDR waveforms vary not only with the soil water content, but also with the soil types, bulk density, and probe parameters," said Lin. "If these factors can be taken into account in the analysis, we can have a better algorithm for determining the soil water content."
TDR measurement has become a widely adopted method for monitoring soil water content. The article examines the limitations of the traditional data reduction method for determining water content and proposed a new method. The result is a better automatic data reduction algorithm. Previous studies of TDR waveforms used sophisticated probes that were not appropriate for field applications and had limited values to the agronomy and geotechnical engineering community. The new finding connects the gap between the theoretical analysis and the field measurement.
"Now with almost any kind of probe and cable system, one can measure the frequency-dependent dielectric permittivity of the soil in the field," Lin said. "This will not only improve the soil moisture measurements but also have impacts on the characterization of soil-water interaction."
Soil Science Society of America Journal (SSSAJ), http://soil.
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