1966年の火山活動による蔵王濁川水系のpH異変について

書誌事項

タイトル別名
  • The pH Change of the Nigori-gawa River caused by the Volcanic Activity of the Zaô Volcano in 1966
  • 1966ネン ノ カザン カツドウ ニ ヨル ザオウ ダク カワミズケイ ノ pH イヘン ニ ツイテ

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抄録

In the Zaô valcano, the crater lake “Okama” has been famous as an active center in the historic time. Soon after the cease of the last activity in 1939 at the entrance of the Jigoku-sawa, several fumaroles were suddenly opened, in which the steady state has since been maintained for thirty years. In the early spring of 1966, the activity suddenly, occurred in the vicinity of Kamoshika Spa. Especially, near the junction of the Nigori-gawa and the Furiko-sawa, a new hot-spring started to gush out. Supplied with the acid water of the spring, the pH value of the river water became much lower than ever in its middle and lower course. Therefore, since 1966 the river water has not been used for the irrigation.

収録刊行物

  • 東北地理

    東北地理 21 (3), 160-160, 1969

    東北地理学会

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