日本地球惑星科学連合2024年大会

講演情報

[J] 口頭発表

セッション記号 P (宇宙惑星科学) » P-PS 惑星科学

[P-PS09] 月の科学と探査

2024年5月27日(月) 09:00 〜 10:30 101 (幕張メッセ国際会議場)

コンビーナ:西野 真木(宇宙航空研究開発機構宇宙科学研究所)、鹿山 雅裕(東京大学大学院総合文化研究科広域科学専攻広域システム科学系)、仲内 悠祐(立命館大学)、小野寺 圭祐(東京大学地震研究所)、座長:大竹 真紀子(会津大学)、西野 真木(宇宙航空研究開発機構宇宙科学研究所)


10:10 〜 10:30

[PPS09-05] Lunar subsurface investigations through permittivity measurements

★Invited Papers

*小林 真輝人1宮本 英昭1孫 辰浩1 (1.東京大学)

キーワード:月、誘電率、地下探査、地中レーダー

The lunar regolith not only holds information about the evolution of the lunar surface but also serves as a crucial reservoir for volatiles such as water ice. While direct observations are essential for obtaining information about the regolith, radar exploration is one of the valuable tools for obtaining subsurface information over a wide area down to the thickness of the regolith. Radar exploration provides the permittivity information of the subsurface, which can contribute to a comprehensive understanding of the state of the lunar subsurface.
Permittivity is associated with the bulk density and chemical composition, particularly FeO+TiO2, on the Moon. Recently, we found that another parameter, temperature, is also significant in determining the bulk permittivity of the lunar regolith based on laboratory measurements (Kobayashi et al., 2023). In addition, we pointed out that the temperature may alter the radar data, which has been ignored (Sun et al., submitted).
In this talk, we will present the importance of the temperature dependence of the permittivity for the interpretation of radar data. We will also introduce the ongoing radar exploration methods and permittivity instruments that we are currently employing, and present our strategy for obtaining the information about the subsurface of celestial bodies.