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温暖積雪地域における融雪水の化学特性
http://hdl.handle.net/10091/17177
http://hdl.handle.net/10091/1717770897811-b85a-4adf-b14a-a76fd4c947a9
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
BGR20P15.pdf (255.0 kB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2013-10-04 | |||||
| タイトル | ||||||
| タイトル | Chemical property of snow meltwater in a snowy temperate area | |||||
| タイトル | ||||||
| タイトル | 温暖積雪地域における融雪水の化学特性 | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| 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 | journal article | |||||
| 著者 |
鈴木, 啓助
× 鈴木, 啓助 |
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| 信州大学研究者総覧へのリンク | ||||||
| 表示名 | SUZUKl, Keisuke | |||||
| URL | http://soar-rd.shinshu-u.ac.jp/profile/ja.upTmOUkh.html | |||||
| 出版者 | ||||||
| 出版者 | Japanese Society of Snow and Ice | |||||
| 引用 | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | Bulletin of Glaciological Research. 20:15-20 (2003) | |||||
| 書誌情報 |
Bulletin of Glaciological Research 巻 20, p. 15-20, 発行日 2003 |
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| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | We studied the chemical properties of snow meltwater in a snowy temperate area, where air temperature above the freezing point and rainfall are observed even in mid-winter. The amount of bottom-melt beneath the snow cover in the snowy temperate area we studied was below 1mm day-1, which is similar to the amount in a snowy cold area. However, in the case of winter melting, the pH of the meltwater decreased and its electric conductivity increased correspondingly. As the snowmelt progressed, the oxygen-18(.DELTA.18O) of the snow cover increased gradually, and as a result, the .DELTA.18O of the meltwater also increased accordingly. We conducted a multiple regression analysis with four species of acidifying ions(NO-3 and nss-SO2-4) and neutralizing ions(NH+4 and nss-Ca2+) in meltwater as independent variables and H+ as a dependent variable. We could explain 86% of the H+ concentration fluctuation in meltwater based on the concentrations of these four ion species. A clear diurnal variation is observed in anion concentrations in meltwater at the peak melt season. The anion enrichment factors in meltwater are higher in the order of NO-3, nss-SO2-4 and Cl-, with values of 7.7, 7.2 and 4.0, respectively. | |||||
| 資源タイプ（コンテンツの種類） | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | Article | |||||
| ISSN | ||||||
| 収録物識別子タイプ | PISSN | |||||
| 収録物識別子 | 1345-3807 | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AA11582242 | |||||
| 権利 | ||||||
| 権利情報 | Copyright© 2003 Japanese Society of Snow and Ice | |||||
| 出版タイプ | ||||||
| 出版タイプ | VoR | |||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
