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Geochemical Journal
Geochemical Journal An open access journal for geochemistry
Published for geochemistry community from Geochemical Society of Japan.

Applying an improved method to measure 134Cs, 135Cs, and 137Cs activities and their atom ratios in marine sediments collected close to the Fukushima Daiichi Nuclear Power Plant

Guosheng Yang, Yoshihisa Kato, Hirofumi Tazoe, Masatoshi Yamada
Geochemical Journal, Vol. 52, No. 2, P. 219-226, 2018


The 135Cs/137Cs atom ratio has been proved to be a reliable tracer for radiocesium source identification in the studies on the Fukushima Daiichi Nuclear Power Plant (FDNPP) accident. However, due to the technical challenge to measure 135Cs, no 135Cs data are available for Japanese river or ocean sediments. In the present study, the vertical distributions of 134Cs and 137Cs activities and their ratios in two marine sediment cores, collected offshore from the FDNPP site immediately after the accident, were measured by γ spectrometry. A conventional introduction system was replaced by an APEX-Q system, by which it was possible to get 6.5 times higher Cs intensities and then 135Cs was analyzed by triple-quadrupole inductively coupled plasma-mass spectrometry. From the vertical distributions, it was seen that the deposition of 134Cs and 137Cs presented an increasing trend, which indicated continuous radiocesium input into the ocean and deposition from sea water onto the sea floor up to the collection date. Therefore, the 134Cs/137Cs activity ratios (0.866–1.16) and 135Cs/137Cs atom ratios (0.249–0.343) (all decay-corrected to March 11, 2011) in marine sediment core samples showed the fingerprints of radiocesium in the oceanic environment were mainly derived from the FDNPP.


135Cs/137Cs atom ratio, 134Cs/137Cs activity ratio, Fukushima Daiichi Nuclear Power Plant accident, marine sediment, triple-quadrupole inductively coupled plasma-mass spectrometry

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