JpGU-AGU Joint Meeting 2017

講演情報

[JJ] 口頭発表

セッション記号 H (地球人間圏科学) » H-TT 計測技術・研究手法

[H-TT26] [JJ] 浅層物理探査

2017年5月24日(水) 13:45 〜 15:15 105 (国際会議場 1F)

コンビーナ:尾西 恭亮(国立研究開発法人土木研究所)、高橋 亨(公益財団法人深田地質研究所)、青池 邦夫(応用地質株式会社)、井上 敬資(国立研究開発法人 農業・食品産業技術総合研究機構)、座長:高橋 亨(公益財団法人深田地質研究所)、座長:青池 邦夫(応用地質株式会社)、座長:井上 敬資(国立研究開発法人 農業・食品産業技術総合研究機構)

14:00 〜 14:15

[HTT26-02] 電磁波を用いた1次元誘電率分布の推定手法の開発

*古川 陽1高木 勘多1廣瀬 壮一1山中 義彰2今井 博2 (1.東京工業大学、2.サンコーコンサルタント株式会社)

キーワード:電磁波、誘電率分布、アンセンテッドカルマンフィルタ

It is important to monitor water distribution under the ground near repository sites of radioactive waste. Water content in the ground and rocks can be evaluated via electromagnetic wave analysis. Electromagnetic wave analysis has advantages to evaluate water content for the following reasons: (1) The existence of pore water provides significant change in dielectric constant. (2) There is a relation between dielectric constant and degree of saturation. However, it is difficult to evaluate the distribution of dielectric constant in wave propagation direction by existing methods which are based on information of arrival time and amplitude of electromagnetic waves reflected from gap of dielectric constant.
This study presents a method to estimate the distribution of dielectric constant via electromagnetic wave analysis. The proposed method consists of an unscented Kalman filter and a finite element method. The unscented Kalman filter is a nonlinear Kalman filter which can evaluate state values of a nonlinear system from observation signals with zero-mean Gaussian noise. In the estimation process, the nonlinear Kalman filter requires computation of nonlinear transform. In this study, the computation of a nonlinear transform corresponds to the FEM analysis of reflected electromagnetic waves for arbitrary distribution of dielectric constant.
The validity and performance of our proposed method have been confirmed by numerical and laboratory experiments. In numerical experiments, reflected electromagnetic waves computed by FEM are used as observed signals. The estimated distribution of dielectric constant is in good agreement with the correct distribution. In laboratory experiments, reflected waves measured by a ground penetrating radar (GPR) are used as observed signals. The estimation results are not well fitted with the distributions expected. One of the reasons is that finite element analysis doesn’t consider the effects of wave attenuation, and this problem is a future task of this study.