環境工学研究論文集
Online ISSN : 1884-829X
Print ISSN : 1341-5115
ISSN-L : 1341-5115
猪苗代湖の水質に及ぼす酸性河川長瀬川の水質および底質特性
黒澤 幸二中村 玄正高橋 幸彦松本 順一郎
著者情報
ジャーナル フリー

1997 年 34 巻 p. 111-120

詳細
抄録

From the view point of water supply stability, lakes and reservoirs are expected to be important water resources. Lake Inawashiro is the most important water resource not only for the Aizu districts but also for Koriyama city and the surrounding area. Lake Inawashiro has 104km2 of surface area, 3, 859, 000, 000m3 of volume and is classified as an oligotrophicated but acid-eutrophicated lake. The water quality of Lake Inawashiro has been at very high level. We considerthat the water quality of lake Inawashiro should be effectedby the Nagase river.
Water quality was investigated at fifteen points of the Sukawa river and Nagase river. The pHvalue of the water is about 2-5 because of sulfuric acid flow out from out abandoned mind. As ferric, aluminium and phosphorus concentration decrease with flow down travel, it had been concludedthat the river had been undergoing self purification concerning to phosphorus. Sulfuric acidwater, which flows into Lake Inawashiro from the Nagase River has possibility of dissolving ferricand aluminium which have the ability of the flocculating and sedimenting of phosphorus.
Thus, in the Nagase river, phosphorus concentration which causes eutrophication is very low, comparing to the other rivers which flow into Lake Inawashiro.

著者関連情報
© 社団法人 土木学会
前の記事 次の記事
feedback
Top