Natural attenuation of dissolved uranium within a small stream of central Japan View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2007-08

AUTHORS

Mitsuo Manaka, Yoji Seki, Koichi Okuzawa, Hikari Kamioka, Yoshio Watanabe

ABSTRACT

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 field 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. More... »

PAGES

143-153

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/s10201-007-0199-z

DOI

http://dx.doi.org/10.1007/s10201-007-0199-z

DIMENSIONS

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41 schema:description 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 field 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.
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