環境工学研究論文集
Online ISSN : 1884-829X
Print ISSN : 1341-5115
ISSN-L : 1341-5115
豊平川におけるヒ素の降雨時流出特性
辰巳 健一中埜渡 丈嘉三浦 勝巳成田 隆広神 和夫眞柄 泰基橘 治国
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ジャーナル フリー

2002 年 39 巻 p. 257-266

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The Toyohira River, the source for Sapporo's waterworks, receives inflow discharged from mines and hot springs. The concentration of potentially hazardous substances in such inflow is high for some flow regimes, which raises concerns related to water quality management. We conducted a water quality survey during and after rainfall (Aug. 21-24, 2001). Rainfall totaled 79 mm. This report reviews the movement of arsenic identified from its runoff characteristics based on continuous observation of water quality during the rainfall. Dissolved arsenic was found to showpoint-type discharge (distilled) whereby the concentration decreased according to the increase in discharge. Suspended arsenic was found to show a non-point-type (outflow) discharge, as was true for suspended solids. Arsenic stored in thesilt and clay of bottom sediment at normal times is tracted by the turbulent flow that occurs during rainfall, becomes suspended, and flows down in high concentration.

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