“…To extend the applicability of the derived dielectric properties to frequencies between 10 and 89 GHz, a simple parameterization of the imaginary part of the permittivity is proposed.
has been described as an inverse function of the frequency for dry rocks (Ulaby et al.,
1990), or with a Debye‐type model dependent on multiple parameters such as the sand fraction (Dobson et al.,
1985; Gupta & Jangid,
2011; Peplinski et al.,
1995), and soil moisture contents above 5%. For very dry soil, we suggest an empirical approach, only retaining the inverse relationship of
with frequency:
with a and b coefficients to represent the spatial variation of the dielectric properties.…”