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妙高山麓地域の降雪及び積雪中に含まれる主要化学成分
https://niit.repo.nii.ac.jp/records/889
https://niit.repo.nii.ac.jp/records/8894e2ce862-f3b5-40fd-9002-6e585958b3fe
名前 / ファイル | ライセンス | アクション |
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niit2_27_8_118-124.pdf (792.5 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2011-02-28 | |||||
タイトル | ||||||
言語 | ja | |||||
タイトル | 妙高山麓地域の降雪及び積雪中に含まれる主要化学成分 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Major Chemical Constituents in Snowfall and Snowcover on the Piedmont of Mt. Myoko | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
著者 |
福崎, 紀夫
× 福崎, 紀夫× 大泉, 毅× 伊藤, 保子 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Snowfall and core samples of snowcover were collected from two different sites on the southeastern slope of Mt. Myoko in southwestern Niigata Prefecture. One sampling site was the top of Suginohara Ski Grounds and the other, the foot of that Ski Grounds (Suginosawa). Conductivity, pH and major ions in the samples were measured. Precipitation-weighted mean of the concentrations of ions in the snowfall at Suginosawa were higher than that at the top. The total deposition of each ion at Suginosawa exceeded that at the top. The average concentration of each ion in newly fallen snow was lower than that in snowfall, possibly due to the runoff of ions from newly fallen snow by melting. Ion movement from upper to lower layers was confirmed in ion concentration profiles of snowcover collected four times. The nitrate to sulfate ratio, expressed as equivalents, was about 0.3 at both sites. Sulfate may thus possibly be largely responsible for the snow acidity in this region. | |||||
書誌情報 |
新潟県衛生公害研究所年報 巻 8, p. 118-124, 発行日 1993-12 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0913-1671 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN10036850 | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
出版者 | ||||||
出版者 | 新潟県衛生公害研究所 |