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  1. 学術雑誌掲載済論文
  2. 和雑誌

河川水位上昇による空気湧出時における堤体と堤内地盤の内部構造の把握

https://kitami-it.repo.nii.ac.jp/records/2000003
2d8544df-7d45-47a9-9eca-0d2a71eafafb
名前 / ファイル ライセンス アクション
dobokuB1_73,4,I_1261-1266.pdf 土木学会論文集B1(水工学) 73, 4, I_1261-1266 (1.9 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2021-03-31
タイトル
言語 ja
タイトル 河川水位上昇による空気湧出時における堤体と堤内地盤の内部構造の把握
タイトル
言語 en
タイトル EVALUATION OF LEVEE AND AROUND GROUND INNER STRUCTURE ON AIR-BLOW PHENOMENON
言語
言語 jpn
キーワード
言語 en
主題Scheme Other
主題 air blow
キーワード
言語 en
主題Scheme Other
主題 levee
キーワード
言語 en
主題Scheme Other
主題 landside
キーワード
言語 en
主題Scheme Other
主題 inner structure
キーワード
言語 en
主題Scheme Other
主題 surface wave method
キーワード
言語 en
主題Scheme Other
主題 shear wave velocity
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
著者 川尻, 峻三

× 川尻, 峻三

WEKO 39273

ja 川尻, 峻三

en KAWAJIRI, Shunzo

Search repository
川口, 貴之

× 川口, 貴之

WEKO 285

ja 川口, 貴之

en KAWAGUCHI, Takayuki

Search repository
早川, 博

× 早川, 博

WEKO 157

ja 早川, 博

ja-Kana ハヤカワ, ヒロシ

Search repository
中村, 大

× 中村, 大

WEKO 237

ja 中村, 大

en NAKAMURA, Dai

Search repository
渡邊, 康玄

× 渡邊, 康玄

WEKO 214
CiNii ID 9000411228257
KAKEN - 研究者検索 00344424

ja 渡邊, 康玄

ja-Kana ワタナベ, ヤスハル

en Watanabe, Yasuhau

Search repository
森田, 大詩

× 森田, 大詩

ja 森田, 大詩

en MORITA, Taishi

Search repository
田中, 悠暉

× 田中, 悠暉

ja 田中, 悠暉

en TANAKA, Yuki

Search repository
抄録
内容記述タイプ Abstract
内容記述 堤防周辺における空気湧出の発生は,高水位作用を受けた堤防の安全性低下に関する予兆と考えられるため,その発生要因や発生時の堤体内の状況を理解することは工学的に重要である.本研究では,裏のり尻で空気湧出が確認された堤体に対して,堤体内部構造を把握するために表面波探査を行った.また,土質構成を確認するため,空気湧出発生箇所で試掘を行った.その結果,空気湧出が確認された付近では,高水位前後でS波速度は低い値を維持していた.土質構成は層厚1m程度の乾燥したシルト層の下部に湿潤状態の砂層が分布しており,砂層からは湧水が発生していた.このことから,S波速度の低速度領域では飽和状態かつ間隙水圧が作用していると考えられ,砂層からの水が不飽和状態にあるシルト層へ浸透する際に空気湧出が発生したと推定される.
言語 ja
抄録
内容記述タイプ Abstract
内容記述 In this research, when detecting an air blow at the slope toe of the levee, we made a survey with surface waves method to evaluate the inner structure of the levee before and after high water. Moreover, to check the soil profile, we dug the air-blow occurrence place. We have concluded that the area where shear waves velocity at low speed is saturated and subjected to pore water pressure, resulting in the occurrence of the air blow when water moves from the sand layer to the upper part of the silt layer.
言語 en
書誌情報 ja : 土木学会論文集B1(水工学)

巻 73, 号 4, p. I_1261-I_1266, 発行日 2017
ISSN
収録物識別子タイプ EISSN
収録物識別子 2185-467X
DOI
関連識別子
識別子タイプ DOI
関連識別子 https://doi.org/10.2208/jscejhe.73.I_1261
論文ID(NAID)
関連識別子
識別子タイプ NAID
関連識別子 130006406164
出版者
言語 ja
出版者 土木学会
著者版フラグ
値 publisher
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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