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  1. F300 宇宙地球環境研究所
  2. F300b 紀要
  3. 名古屋大学加速器質量分析計業績報告書
  4. 13

雲仙周辺における土壌CO_2を利用した火山活動の影響範囲の推定に関する研究

https://doi.org/10.18999/sumrua.13.105
https://doi.org/10.18999/sumrua.13.105
6da8f2e8-101d-400f-9df6-3d5ad85f4bb5
名前 / ファイル ライセンス アクション
KJ00000187441.pdf KJ00000187441.pdf (230.5 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-06-01
タイトル
タイトル 雲仙周辺における土壌CO_2を利用した火山活動の影響範囲の推定に関する研究
その他のタイトル
その他のタイトル Spatial estimation of volcanic effect using soil air CO_2 around the Unzen volcano
著者 高橋, 浩

× 高橋, 浩

WEKO 81294

高橋, 浩

Search repository
Takahashi, Hiroshi A.

× Takahashi, Hiroshi A.

WEKO 81295

Takahashi, Hiroshi A.

Search repository
風早, 康平

× 風早, 康平

WEKO 81296

風早, 康平

Search repository
Kazahaya, Kohei

× Kazahaya, Kohei

WEKO 81297

Kazahaya, Kohei

Search repository
篠原, 宏志

× 篠原, 宏志

WEKO 81298

篠原, 宏志

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Shinohara, Hiroshi

× Shinohara, Hiroshi

WEKO 81299

Shinohara, Hiroshi

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中村, 俊夫

× 中村, 俊夫

WEKO 81300

中村, 俊夫

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Nakamura, Toshio

× Nakamura, Toshio

WEKO 81301

Nakamura, Toshio

Search repository
権利
権利情報 名古屋大学年代測定資料研究センター
権利
権利情報 本文データは学協会の許諾に基づきCiNiiから複製したものである
抄録
内容記述 In the present study, the carbon isotopic approach was used for identification of magmatic contribution in soil air CO_2. Here we represent the CO_2 concentration and carbon isotopic composition in soil air in order to estimate the effect from Unzen Volcano in the Shimabara Peninsula. We took soil air through a sampling tube pricked at 30cm depth below the land surface, and measured concentration of carbon dioxide by the GASTEC tube. For the isotopic analysis, soil air was sampled in a glass reservoir (100ml : for stable carbon isotopic measurement) or an aluminized plastic bag (3 litters : for radiocarbon measurement). CO_2 was collected from the sampled soil air under the vacuum at the laboratory, and its stable carbon isotopic composition was measured by the IR-MS. Some samples measured radiocarbon concentration by the accelerator mass spectrometry at the Nagoya University. The filed observations were carried out in September 2001. We had two traverses (500-600m) across the fault near the USDP-2 site and embouchure of the Waren River. We also took bubbles in the spring water at the Waren River and the smoke air of Heiseishin-zan volcano. We found that several points had the high CO_2 concentration in the two traverses of the USDP-2 and the Waren River. Some of them showed the relatively higher value of stable carbon isotopic ratio. This indicates that the magmatic CO_2 might be brought to the land surface in the area of Unzen Graven. Moreover, radiocarbon technique tells us the stable carbon isotopic ratio of magmatic CO_2 and contributions of magmatic, biogenic and atmospheric CO_2. The value of stable carbon isotopic ratio was estimated to be -5.4per-mil. The proportions of respective contributions were 75 : 0 : 25 for smoke air, 60 : 40 : 0 in soil air nearby the Waren River spring and 0 : 30 : 70 in soil air at 500m away from the Waren River.
内容記述タイプ Abstract
内容記述
内容記述 第14回名古屋大学タンデトロン加速器質量分析計シンポジウム(平成13 (2001)年度)報告
内容記述タイプ Other
出版者
出版者 名古屋大学年代測定資料研究センター
言語
言語 jpn
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
ID登録
ID登録 10.18999/sumrua.13.105
ID登録タイプ JaLC
関連情報
関連タイプ isVersionOf
識別子タイプ URI
関連識別子 http://ci.nii.ac.jp/naid/110000475717/
書誌情報 名古屋大学加速器質量分析計業績報告書

巻 13, p. 105-109, 発行日 2002-03
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