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Figure 5


FIG. 5. Comparison of the measured {varepsilon}r' (real component of relative complex permittivity) and {varepsilon}r'' (imaginary component of relative complex permittivity) temperature (T) response with apparent permittivity, {varepsilon}a, calculated using Eq. [3]. The Ames soil is representative of high {varepsilon}r'' soils, and the Tif5 soil is representative of low {varepsilon}r'' soils. Where {varepsilon}r'' is low, there is little impact on {varepsilon}a, and sensor type is not critical.