河川結氷時の塩水遡上に関する基礎的研究
This study aimed to clarify the fundamental phenomenon of salinity intrusion in ice covered river. We carried out salinity intrusion experiment to which model ice-sheet floats on the water surface and one-dimensional two-layered unsteady flow calculation. In this experiment, the vertical flow veloci...
Published in: | Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering) |
---|---|
Main Authors: | , , , |
Language: | Japanese |
Published: |
公益社団法人 土木学会
2012
|
Subjects: | |
Online Access: | https://kitami-it.repo.nii.ac.jp/record/7757/files/20012-03_河川結氷時の塩水遡上に関する基礎的研究.pdf https://kitami-it.repo.nii.ac.jp/records/7757 |
_version_ | 1828692565462876160 |
---|---|
author | 吉川, 泰弘 赤堀, 良介 安田, 浩保 平井, 康幸 |
author_facet | 吉川, 泰弘 赤堀, 良介 安田, 浩保 平井, 康幸 |
author_sort | 吉川, 泰弘 |
collection | Kitami Institute of Technology Repository (KIT-R) |
container_issue | 4 |
container_start_page | I_1321 |
container_title | Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering) |
container_volume | 68 |
description | This study aimed to clarify the fundamental phenomenon of salinity intrusion in ice covered river. We carried out salinity intrusion experiment to which model ice-sheet floats on the water surface and one-dimensional two-layered unsteady flow calculation. In this experiment, the vertical flow velocity was measured using particle image velosimetry technique. In the experiment in which ice-sheet exists, the model ice-sheet indirectly attenuated the salinity intrusion because Reynolds number does not become large. Shear stress was computed by having assigned the experiment data to one-dimensional two-layered unsteady flow equation. In both ice and no-ice condition, Interface shear stress has large influence on salinity intrusion. It was shown that the calculation model built by this study can reproduce salinity intrusion experiment. journal article |
genre | Ice Sheet |
genre_facet | Ice Sheet |
id | ftkitamiit:oai:kitami-it.repo.nii.ac.jp:00007757 |
institution | Open Polar |
language | Japanese |
op_collection_id | ftkitamiit |
op_container_end_page | I_1326 |
op_doi | https://doi.org/10.2208/jscejhe.68.I_1321 |
op_relation | http://doi.org/10.2208/jscejhe.68.I_1321 土木学会論文集B1(水工学) 4 68 I_1321 I_1326 |
op_rights | c 2012 公益社団法人 土木学会 open access |
publishDate | 2012 |
publisher | 公益社団法人 土木学会 |
record_format | openpolar |
spelling | ftkitamiit:oai:kitami-it.repo.nii.ac.jp:00007757 2025-04-06T14:55:14+00:00 河川結氷時の塩水遡上に関する基礎的研究 A FUNDAMENTAL STUDY OF SALINITY INTRUSION IN ICE COVERED RIVER 吉川, 泰弘 赤堀, 良介 安田, 浩保 平井, 康幸 2012 application/pdf https://kitami-it.repo.nii.ac.jp/record/7757/files/20012-03_河川結氷時の塩水遡上に関する基礎的研究.pdf https://kitami-it.repo.nii.ac.jp/records/7757 jpn jpn 公益社団法人 土木学会 http://doi.org/10.2208/jscejhe.68.I_1321 土木学会論文集B1(水工学) 4 68 I_1321 I_1326 c 2012 公益社団法人 土木学会 open access Ice covered River Salinity Intrusion Experiment 2012 ftkitamiit https://doi.org/10.2208/jscejhe.68.I_1321 2025-03-10T11:33:07Z This study aimed to clarify the fundamental phenomenon of salinity intrusion in ice covered river. We carried out salinity intrusion experiment to which model ice-sheet floats on the water surface and one-dimensional two-layered unsteady flow calculation. In this experiment, the vertical flow velocity was measured using particle image velosimetry technique. In the experiment in which ice-sheet exists, the model ice-sheet indirectly attenuated the salinity intrusion because Reynolds number does not become large. Shear stress was computed by having assigned the experiment data to one-dimensional two-layered unsteady flow equation. In both ice and no-ice condition, Interface shear stress has large influence on salinity intrusion. It was shown that the calculation model built by this study can reproduce salinity intrusion experiment. journal article Other/Unknown Material Ice Sheet Kitami Institute of Technology Repository (KIT-R) Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering) 68 4 I_1321 I_1326 |
spellingShingle | Ice covered River Salinity Intrusion Experiment 吉川, 泰弘 赤堀, 良介 安田, 浩保 平井, 康幸 河川結氷時の塩水遡上に関する基礎的研究 |
title | 河川結氷時の塩水遡上に関する基礎的研究 |
title_full | 河川結氷時の塩水遡上に関する基礎的研究 |
title_fullStr | 河川結氷時の塩水遡上に関する基礎的研究 |
title_full_unstemmed | 河川結氷時の塩水遡上に関する基礎的研究 |
title_short | 河川結氷時の塩水遡上に関する基礎的研究 |
title_sort | 河川結氷時の塩水遡上に関する基礎的研究 |
topic | Ice covered River Salinity Intrusion Experiment |
topic_facet | Ice covered River Salinity Intrusion Experiment |
url | https://kitami-it.repo.nii.ac.jp/record/7757/files/20012-03_河川結氷時の塩水遡上に関する基礎的研究.pdf https://kitami-it.repo.nii.ac.jp/records/7757 |