富士山周辺における湧水中の栄養塩特性

萩原 直樹

doi:10.14862/geochemproc.62.0_261

Abstracts of Annual Meeting of the Geochemical Society of Japan

Session ID : 3C08

DOI https://doi.org/10.14862/geochemproc.62.0_261

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Host: Abstracts of Annual Meeting of the Geochemical Society of Japan

Nutorient charecteristics of spring waters around Fuji Volcano

*Hagiwara Naoki

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Keywords: Fuji Volcano, spring waters, basalt, Nutrient

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Abstract

　Fuji Volcano began to form at ca.100,000 y B.P.and contiued to erupt basaltic labas. The ner stage 'shin Fuji'on the weathering old Fuji mudflow is eruptions of basaltic lavas ca.10,000 y B.P. Ther are many springs on the foot around Fuji Volcano.The following representative springs were analyzed about Nutrient.1.East area:Gotenba420～490μM,Kakitagawa 620～660μM 2.Oshinohakkai：Wakuike650μM,Shoubuike 690μM、Kagamiike 660μM

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