日本地球惑星科学連合2024年大会

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[J] 口頭発表

セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS11] 山の科学

2024年5月27日(月) 13:45 〜 15:00 201B (幕張メッセ国際会議場)

コンビーナ:苅谷 愛彦(専修大学文学部環境地理学科)、佐々木 明彦(国士舘大学文学部史学地理学科 地理・環境コース)、奈良間 千之(新潟大学理学部フィールド科学人材育成プログラム)、西村 基志(信州大学 先鋭領域融合研究群 山岳科学研究拠点)、座長:西村 基志(国立極地研究所 北極観測センター)、苅谷 愛彦(専修大学文学部環境地理学科)

14:15 〜 14:30

[MIS11-03] Preliminarily environmental magnetic results from a snow pit in the Midagahara area of Mt. Tateyama, Toyama, Japan.

*川崎 一雄1、平野 瑠香1堀 雅裕1杉浦 幸之助1谷川 朋範2庭野 匡思2足立 光司2 (1.富山大学、2.気象庁気象研究所)

キーワード:環境磁気、雪、大気汚染、立山

Atmospheric pollution often contains measurable magnetic minerals and environmental magnetic monitoring techniques have been shown to be rapid and cost-effective methods for investigating spatial distribution of air pollution. Although snowpack acts as a seasonal storage of contaminants and is widely used in anthropogenic pollution studies, only a few studies using packed snow have been reported for magnetic monitoring. Here, environmental magnetic studies are reported for the Midagahara area of Mt. Tateyama in Toyama. Snow pit observations at the Midagahara were made on a site ~600 m away from the Tateyama Kurobe sightseeing Alpine route, the only available road in the area, on 16-17 April 2023. Three dust layers, likely caused by Asian dust events, are recognized by in-situ snow observation. The snow depth at the study site was about 241 cm. 99 samples were collected from the top to bottom of the pit wall using 7 cm3 non-magnetic plastic cubes. The collected snow melted to water at room temperature and then it was solidified using a superabsorbent polymer. Rock magnetic measurements indicate that the major magnetic mineral in the snow is partially oxidized magnetite and its composition is nearly the same throughout the snow wall. In addition, high coercivity magnetic minerals such as hematite are also found at the upper part of the wall. The higher saturation isothermal remanent magnetization (SIRM) intensities are observed mostly at the upper part of the wall, suggesting larger amounts of magnetic minerals at the upper part. The continuous higher SIRM intensities at the upper part are most likely from the snow removal vehicles rather than sporadic supplies of Asian Dust-derived magnetic minerals. The results show that environmental magnetic techniques can be applied to packed snow by using a superabsorbent polymer and this could be an effective method for monitoring pollution in mountain areas.