3:30 PM - 5:00 PM
[PPS06-P03] Numerical Study of the Propagation of Electromagnetic Waves to Detect Putative Water-ice in Complex Permittivity Structures of the Lunar Regolith
Keywords:Relative permittivity, Regolith, Water-ice, Ground Penetrating Radar
We use the FDTD method by assuming that the water-ice containing layer exists in the lunar polar region. We simplify that the regolith is composed exclusively of anorthosite only. The profile of the relative permittivity of the regolith is modeled considering the subsurface structures of both porosity and temperature as proposed by previous works (Feng & Siegler, 2021; Hayne et al., 2017). We find that detection of the water-ice containing layer by UHF-band GPR is possible even assuming a low water-ice content, if the depth of the layer is deep enough than the characteristic depths determined by the frequency band. More detailed results and applications on measurement system will be discussed in the presentation.
References:
Kobayashi et al., Earth, Planets and Space, 75, 8 (2023).
Feng & Siegler, Journal of Geophysical Research-Planets, 126, (2021).
Hayne et al., Journal of Geophysical Research-Planets, 122, 2371-2400 (2017).