Perchlorate Concentration in Water System and its Variation by Water Treatment in Osaka (original) (raw)

2011, Journal of Environmental Chemistry

Summar y Perchlorate concentrations in raw and tap water in Osaka, Japan, were determined by IC-MS/MS. The concentrations of perchlorate in raw water and tap water were in the ranges from <0. 015 to 0. 48 µg/L and from <0. 015 to 0. 82 µg/L, respectively. Except for only a few cases, the perchlorate concentration in each tap water sample was at nearly equivalent level to that in the corresponding raw water. The results indicate that perchlorate in raw water was not removed effectively by the ordinary water treatment methods such as ozonation, granular activated carbon adsorption, rapid and slow sand filtrations. On the other hand, perchlorate was found to be contained in sodium hypochlorite solutions, used in the chlorination process, at wide concentration range between 4. 9 and 5900 µg/L. In the case using disinfectant with the highest perchlorate content, the significant increase in perchlorate concentration in tap water was observed, compared to that in raw water. However, when 2 L of tap water was ingested every day, the corresponding perchlorate intake was estimated to be at most 1. 8 µg/day from the observed perchlorate concentrations in tap water samples. This value was sufficiently lower than the calculated daily intake for a person weighing 50 kg from reference dose value of perchlorate. Therefore, the health risk to humans from perchlorate in tap water in Osaka, Japan, is very low.

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Horizontal distribution of water quality between early and dense water plant seasons in Lake Shirarutoro, Kushiro Wetland

Japanese Journal of Limnology (rikusuigaku Zasshi), 2020

The dense growth of aquatic macrophytes can affect lake water quality. We studied the water chemistry at 40 sites on Lake Shirarutoro when dense beds of water chestnut (Trapa japonica) expanded in 2007-8. The distribution patterns between the early (June) and middle (August) vegetation water plant seasons were compared. In this lake, the dense beds of water chestnut did not necessarily correspond to the lack of dissolved oxygen at the lake bottom. Principal component analyses (PCA) of 20 variables showed that the lake could be divided into two areas: one was a central area from the main inflowing river to the outflow ('area A') and the other was an area adjacent to the southern wetland ('area B'). The factor loadings of the first principal component (PC) showed high positive value for K + , Ca 2+ , Na + , Cl-, Mg 2+ , and D-Si, and high negative for dissolved organic phosphorus (DOP), dissolved organic carbon (DOC), dissolved organic nitrogen (DON), and dissolved iron (D-Fe). 'Area A' was influenced by the high concentration loading of K + , Ca 2+ , Na + , and Clfrom a northern tributary; 'area B' was influenced by the adjacent wetlands. The factor loadings of the second PC showed high negative values for the total phosphorus (TP), total nitrogen (TN), volatile solids (VS), and chlorophyll a, all of which were indicators of eutrophication. The variables whose factor loading in the first PC changed between June and August were only the soluble reactive phosphorus (SRP) and SO 4 2-. Therefore, we concluded that the distribution of the lake water chemistry was more influenced by watershed condition rather than the dense water plant beds.

Continuous Ground Observation of Particulate Matter on Sakurajima, Kyushu, Japan

2014

A continuous ground observation of particulate matter with a dust meter has been made on Sakurajima. In general, coarse particles are dominant in Sakurajima. Particulate matter concentration varied with the amount of volcanic ash emission and the wind direction. It is considered that the major origin of particulate matter observed in Sakurajima is the volcanic ash of Sakurajima volcano.A continuous ground observation of particulate matter with a dust meter has been made on Sakurajima. In general, coarse particles are dominant in Sakurajima. Particulate matter concentration varied with the amount of volcanic ash emission and the wind direction. It is considered that the major origin of particulate matter observed in Sakurajima is the volcanic ash of Sakurajima volcano

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