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Autoradiography was used to detect  137 Cs-enriched particles in sediment samples. The contributions of  137 Cs-enriched particles to  137 Cs concentrations in sediment samples ranged from 9% to 64%. These experiments revealed that the variability of  137 Cs concentrations was due mainly to the heterogeneous distribution of  137 Cs-enriched particles in the samples. Therefore, the heterogeneous distribution of  137 Cs-enriched particles is probably one of the main factors responsible for the temporal and spatial variations of  137 Cs concentrations in sediment samples.

Contribution of 137Cs-enriched particles to radiocesium concentrations in seafloor sediment: Reconnaissance experiment