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Report No.
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Behavior of radium in Ningyo-toge Environmental Engineering Center

Kuribara, Yuichi  ; Yamaguchi, Akiko*  ; Higaki, Shogo*; Ohara, Yoshiyuki; Takahashi, Yoshio*

In order to investigate the behavior of radium (Ra) in the Ningyo-toge Environmental Engineering Center, $$^{226}$$Ra/$$^{238}$$U activity ratio in two boring core samples in the center was analyzed with HPGe semiconductor detector. The $$^{226}$$Ra/$$^{238}$$U ratio was below 1 and over 1 in the U enriched and contained clay mineral layers, respectively. Based on the radioactive equilibrium and mass balance calculation, it was suggested that Ra and U eluted to groundwater migrated from the U enriched layer to the contained clay minerals layer when Ra was selectivity fixed on the contained clay mineral layer. EXAFS and micro-XRF-XANES-XRD for Ba, used as an analog of Ra, confirmed that Ba$$^{2+}$$ was adsorbed on clay minerals as IS complex, and Ra was expected to show similar behavior. Therefore, it was indicated that Ra migrated from U concentrated layer was adsorbed and fixed on clay minerals in the environment of the Ningyo-toge Environmental Engineering Center.

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