In this study, we investigated the natural attenuation of the uranium (U) load in the surface water within a humid forest in Japan. Surface water and sediments that had accumulated behind dams in the area were investigated in terms of their mineralogy and chemistry. The chemistry of the surface water was analyzed by fi eld measurements of pH, dissolved oxygen (DO) concentration, and electrical conductivity (EC), as well as laboratory analyses via inductively coupled plasma mass spectrometry and ion chromatography. We determined U levels in the surface water; the distribution of U in phases within the sediment was estimated using a sequential extraction procedure. The results of this investigation indicate that U, which within the study area is derived from pegmatites at a mine, is attenuated by uptake onto the surface of organic material and uptake by amorphous material that forms over time within the dammed sediments. The U concentration within the sediment was as great as 8 mg kg −1 , whereas the downstream U concentrations and loads in surface water decreased from 1.69 µg l −1 and 11.0 mg min −1 to 0.115 µg l −1 and 2.31 mg min −1 , respectively.

In this study, we surveyed the uranium (U) load in stream water within a humid forest in Japan, and clarified the fact that changes in U load depended on the amount of sediment accumulated behind dams constructed along the stream. To elucidate the relationship between U and the accumulated sediments, we conducted U sorption experiments in the laboratory using stream water and sampled sediments. The chemistry of the stream water was analyzed in the field for pH, electrical conductivity (EC), and temperature, as well as laboratory analyses via inductively coupled plasma mass spectrometry (ICP-MS). We determined the amount of organic material, amorphous material, and total U contents in the sediments. Following the sorption experiments, we analyzed the pH and U concentrations in experimental solutions and determined the distribution coefficients of U for the sediments. The logarithm value of the distribution coefficients of U for amorphous material shows a positive correlation with pH, while the logarithm value of the distribution coefficients of U for organic material is independent of pH (4.7-6.9). Although the logarithm value of the distribution coefficient of U for amorphous material was 0.1-0.5 units larger than the value for organic material, U was effectively removed from the stream water by sorption onto organic material (humic substances and decomposing leaves), because the amount of organic material exceeded that of amorphous material.

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