Updated on 2024/08/20

写真a

 
Yoshiharu Takemura
 
Organization
Research and Development Initiative Institute Associate Professor
Contact information
The inquiry by e-mail is 《here
External link

Degree

  • 博士(工学) ( 中央大学 )

Education

  • 2012.3
     

    Chuo University   doctor course   completed

Research History

  • 2019.4 - Now

    Chuo University   Research and Development Initiative   Associate professor

  • 2012.4 - 2019.3

    Chuo University   Research and Development Initiative   Assistant professor

Professional Memberships

  • 2020.10 -  

    地盤工学会

  • JAPAN SOCIETY OF CIVIL ENGINEERS

Research Interests

  • 水工水理学

  • hydraulic jump

  • Riverbank Erosion

  • 流砂・河床変動

  • 河川工学

Research Areas

  • Social Infrastructure (Civil Engineering, Architecture, Disaster Prevention) / Hydroengineering

Papers

MISC

  • EVALUATION OF THE INCIPIENT MOTION OF LARGE BOULDERS BY COMBINING NON-HYDROSTATIC QUASI-THREE-DIMENSIONAL ANALYSIS (Q3D-FEBS) AND DISTINCT ELEMENT METHOD

    OHNO Jyunki, YAMASHITA Atsushi, TAKEMURA Yoshiharu, FUKUOKA Shoji

    Advances in River Engineering   28   277 - 282   2022

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    Language:Japanese   Publisher:Japan Society of Civil Engineers  

    DOI: 10.11532/river.28.0_277

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  • THE INFLUENCE OF SUSPENDED LOAD ON RIVER BED VARIATION IN THE BRAIDED RIVER OF THE ABE RIVER

    MORIMOTO Yusuke, TATEMATSU Akinori, FUKUOKA Shoji, TAKEMURA Yoshiharu

    Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering)   78 ( 2 )   I_871 - I_876   2022

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    Language:Japanese   Publisher:Japan Society of Civil Engineers  

    We have studied the role of non-equilibrium sediment transport of bed load on bed variations of the braided channels in the middle and lower reaches due to flood flows in the Abe River, which is composed of a wide grain-size distribution of bed materials including gravels. This paper focuses on the role of non-equilibrium sediment transport of suspended load which is greatly affected by the three-dimensional flood flows on bed variation. Our calculations showed that the amount of suspended load is relatively large in the flood descending period, and the tendency for bed load and suspended load to accumulate on the sandbars resulted in a large specific height difference between the sandbars and channels. We also confirmed that secondary flows develop at the side edges of sandbars due to the flow mixing between the flow over the sandbars and the flow in the channels promote the deposition of suspended load at the side edges of sandbars, and it causes the lateral movement of the sandbar and reduction of the width of the channel.

    DOI: 10.2208/jscejhe.78.2_i_871

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  • ANALYSIS OF RIVERBANK EROSION PROCESSES IN ALLUVIAL FANS: APPLICATION TO THE FILED EXPERIMENT IN THE JOGANJI RIVER

    TAKEMURA Yoshiharu, FUKUOKA Shoji

    Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering)   77 ( 2 )   I_799 - I_804   2021

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    Language:Japanese   Publisher:Japan Society of Civil Engineers  

    The erosion process of natural riverbank consists of three parts: bank toe erosion, bank failure and removal of the deposited material on the bank toe. Erosion of the riverbank occurs intermittently during flood events by repeating this process. However, it has not been considered enough in the flood flow and bed variation analysis in rivers. This paper proposes an analysis method of the bank erosion process in alluvial fans by considering the effects of the negative pore water pressure (the matrix suction), three-dimensional flows, and non-equilibrium sediment transports at near-bank area. Moreover, it is shown that the analysis method can explain the bank erosion process of the field experiment in the Joganji River.

    DOI: 10.2208/jscejhe.77.2_i_799

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    Other Link: https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-20K04711/

  • CONSIDERATION OF MOVEMENT OF BOULDERS USING QUASI-THREE-DIMENSIONAL ANALYSIS BASED ON FLOOD WATER SURFACE PLOFILES AND DETAILED RIVERBED OBSERVATION DATA

    OHNO Jyunki, YAMASHITA Atsushi, TAKEMURA Yoshiharu, FUKUOKA Shoji

    Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering)   77 ( 2 )   I_631 - I_636   2021

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    Language:Japanese   Publisher:Japan Society of Civil Engineers  

    Mountain rivers are composed of a wide range of particle sizes. In particular, the movement of boulders with a size of about 1.0m has an effect on flow resistance and sediment transport. In this study, we surveyed the existence and loss of boulders and gravels, and investigated the judgement method of boulder movement due to the flood flow in the Takiyama River. Using quasi-three-dimensional flood flow analysis by Q3D-FEBS based on the observed water surface profiles and detailed topographic survey data, we attempted to evaluate the movement of boulders by flood flows. The future issues on this matter are discussed.

    DOI: 10.2208/jscejhe.77.2_i_631

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  • ESTIMATION ON FLOOD DISCHARGE HYDROGRAPH BASED ON OBSERVED WATER SURFACE PROFILES IN RIVERS WITH BOULDERS

    Advances in River Engineering   27   265 - 270   2021

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  • DEVELOPMENT OF BRAIDED CHANNELS BY BED LOAD AND SUSPENDED LOAD IN THE GRAVEL BED OF THE ABE RIVER DUE TO FLOOD FLOWS

    MORIMOTO Yusuke, TAKEMURA Yoshiharu, FUKUOKA Shoji, TATEMATSU Akinori

    Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering)   77 ( 2 )   I_757 - I_762   2021

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    Language:Japanese   Publisher:Japan Society of Civil Engineers  

    The braided stream of the Abe River is considered to be formed by the non-equilibrium motion of the bed load and suspended load, which change significantly in time and space due to the complex riverbed topography of the braided channels. This paper presents the bed variation mechanism of braided bars in the Abe River by calculating the three-dimensional flows and non-equilibrium motion of the bed load and suspended load based on the time series data of the observed water surface profiles of the large flood in 2014. The calculation results could well explain the changes in mainstream positions due to the movement of the braided bars.

    DOI: 10.2208/jscejhe.77.2_i_757

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  • 扇状地河川における河岸侵食プロセスに関する研究

    竹村 吉晴

    第9回河川堤防技術シンポジウム   第9回   79 - 82   2021

  • 洪水流による物部川河口礫州の開口と変形機構 に関する研究 Reviewed

    竹村 吉晴

    河川技術論文集   26   669 - 674   2020

  • ANALYSIS OF THE FLOW IN UNDULAR AND HYDRAULIC JUMP STILLING BASINS USING NON-HYDROSTATIC QUASI-THREE DIMENSIONAL MODEL CONSIDERING FLOW EQUATIONS ON BOUNDARY SURFACES

    TAKEMURA Yoshiharu, FUKUOKA Shoji

    Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering)   75 ( 1 )   61 - 80   2019

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    Language:Japanese   Publisher:Japan Society of Civil Engineers  

    <p> This paper aims at development of a non-hydrostatic quasi-three dimensional model for the flow in undular and hydraulic stilling basins. It is challenging for the depth-integrated model to calculate the flow separation at boundary surfaces (water surface and bed surface). To solve this problem, a non-hydrostatic quasi-three dimensional model considering flow equations on boundary surfaces (Q3D-FEBS) was derived. Q3D-FEBS was applied to the undular and hydraulic jump experiments. The calculation results are in good agreement with the observation data such as water surface profiles and velocity distributions of the undular and hydraulic jump. Moreover, it was showed that Q3D-FEBS can calculate the breaking process of the undular jump and formation of the surface roller. Finally, the applicability of Q3D-FEBS for the flow in hydraulic jump stilling basins was discussed against observation data of a large scale hydraulic model experiment.</p>

    DOI: 10.2208/jscejhe.75.61

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  • 巨岩・巨石が点在する山地河川に対する平面二次元解析法の課題と新しい解析法の提案 Reviewed

    竹村 吉晴

    河川技術論文集   第25巻   267 - 272   2019

  • STUDY ON THE FLOOD STORAGE FUNCTIONS OF THE MIDDLE ARAKAWA RIVER WITH LARGE FLOOD PLAINS AND CROSS-LEVEES

    竹村 吉晴, 福岡 捷二, 吉井 拓也

    水工学論文集 Annual journal of Hydraulic Engineering, JSCE   62 ( 4 )   Ⅰ_1387 - 1392   2018

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    Language:Japanese   Publisher:土木学会  

    The middle Arakawa River has large flood plains, about 2.5km in maximum width. Flood storage functions of the middle Arakawa River had been strengthened by installing cross-levees which extend at right angles to levees and the Arakawa 1st retarding basin on the flood plains. New three retarding basins have been planed in the middle Arakawa River. This paper investigate the storage functions of the middle Arakawa River against the design flood hydrographs by numerical flood simulations based on the accurate flood flow model. The cross-levees increase the flood plain storage and delay the peak occurrence time of rate of storage. However, the large flood plains are filled with flood water at early stage of rising limb of the flood flows and do not have the sufficient storage space at the flood peak of the design hydrographs. For this reason, the peak discharge of the Iwabuchi control point exceeds the design discharge (6300m3/s).

    DOI: 10.2208/jscejhe.74.i_1387

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  • A COMPUTATION METHOD FOR FLOW OVER HYDRAULIC STRUCTURES WITH LARGE WATER SURFACE DEFORMATIONS CONSIDERING GENERATION AND FLUX OF VORTICITY AT THE FREE SURFACE

    竹村 吉晴, 福岡 捷二, 日下部 隆昭

    水工学論文集 Annual journal of Hydraulic Engineering, JSCE   61   Ⅰ_667 - 672   2017

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    Language:Japanese   Publisher:土木学会  

    DOI: 10.2208/jscejhe.73.I_667

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  • A COMUPUTAION METHOD FOR FLOW OVER HYDRAULIC STRUCTURES WITH LARGE WATER SURFACE DEFORMATIONS CONSIDERING GENERATION AND FLUX OF VORTICITY AT THE FREE SURFACE

    TAKEMURA Yoshiharu, FUKUOKA Shoji, KUSAKABE Takaaki

    J. JSCE, Ser. B1   73 ( 4 )   I_667 - I_672   2017

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    Language:Japanese   Publisher:Japan Society of Civil Engineers  

    &amp;nbsp;Considering the dynamic boundary condisition at free surface (zero tangential stress) was the fundamental problem for applying the General Bottom Velocity Computation (GBVC) method to the flow over hydraulic structures with large water surface deformations. The zero tangential stress condition causes generation and flux of vorticity at the free surface. We formulated these processes and developed GBVC-FSV method. GBVC-FSV method was applied to the flow over a vertical sill. A comparison with the results of GBVC method indicates that GBVC-FSV can calculate the flows with large water surface deformations more stably.

    DOI: 10.2208/jscejhe.73.I_667

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  • VALIDATION AND IMPROVEMENT OF THE PREDICTION MODEL FOR FLOOD FLOWS AND BED VARIATIONS IN THE GO RIVER CONFLUENCES BASED ON DETAILED OBSERVATIONS OF FLOOD WATER LEVELS AND BED CONDITIONS

    TAKEMURA Yoshiharu, FUKUOKA Shoji, HAMAMOTO Kentaro

    Advances in River Engineering   22   145 - 150   2016

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    Language:Japanese   Publisher:Japan Society of Civil Engineers  

    The Go River confluences are composed of three rivers having a comparable drainage area. The prediction model for flood flows and bed variations in the confluences is needed for investigating the flow and bed variation characteristics and estimating flood water storages by the river confluences. This paper validates the prediction model based on the BVC method against water levels observed at 200- 400m intervals in the confluence during two large floods of different rainfall patterns. Moreover, the cause of the excessive bed scouring around the flow attacking point of the confluence is explored from observations about local bed profiles and conditions around the flow attacking point by using a radio control boat and unmanned submarine. The changes in local bed conditions around complicated flow areas are considered in order to refine the prediction model for flood flows and bed variations.

    DOI: 10.11532/river.22.0_145

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  • FLOOD FLOW ANALYSIS ON NEW EVALUATION OF GROUND LEVEL ON WIDE AND VEGETATED FLOOD CHANNELS IN THE ARAKAWA RIVER

    FUKUDA Shota, TAKEMURA Yoshiharu, YOSHII Takuya, FUKUOKA Shoji

    Advances in River Engineering   22   133 - 138   2016

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    Language:Japanese   Publisher:Japan Society of Civil Engineers  

    The Arakawa river has a plan to build new three retarding basins in the middle reach. It is important to understand flood control functions in middle stream of the Arakawa river with wide and vegetated flood channels. It is necessary to understand flood inundation mechanism on wide flood channels by flood flow analysis. Laser profilers can make use of the creation of detailed topographic maps of such flood channels, but may count the top height of vegetation on the ground. In this paper, filtering techniques of the laser profiler data are developed for reproducing proper ground heights of flood channels in the Arakawa river. Finally, the new flood analysis which improved the existing flood analysis method is presented.

    DOI: 10.11532/river.22.0_133

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  • EVALUATION METHOD OF RETARDING STORAGE VOLUME FOR UNSTEADY TWO DIMENSIONAL FLOWS AND PROPAGATION MECHANISMS OF DISCHARGE AND WATER LEVEL HYDROGRAPHS THROUGH THE VALLEY OF THE KITAKAMI RIVER

    TAKEMURA Yoshiharu, FUKUOKA Shoji

    J. JSCE, Ser. B1   70 ( 4 )   I_721 - I_726   2014

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    Understanding of the propagation mechanisms of the discharge and water level hydrographs in river channels is important for proper river management. It has been known that discharge hydrographs of flood flows passing through channel contractions are distorted by longitudinal difference of the storage volume of water in the channel. In this case, propagation mechanisms of the discharge and water level hydrographs are different, unlike in the case of the flood flow through a uniform channel. This paper characterize a part of the storage volume of water that causes the distortion of a discharge hydrograph as retarding storage volume of water and its evaluation method is proposed. We apply this method to a large flood through the valley of the Kitakami River and propagation mechanisms of the discharge and water level hydrographs are explained with relation to the storage volume and retarding storage volume of flood water.

    DOI: 10.2208/jscejhe.70.I_721

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  • EVALUATION METHOD OF RETARDING STORAGE VOLUME FOR UNSTEADY TWO DIMENSIONAL FLOWS AND PROPAGATION MECHANISMS OF DISCHARGE AND WATER LEVEL HYDROGRAPHS THROUGH THE VALLEY OF THE KITAKAMI RIVER

    TAKEMURA Yoshiharu, FUKUOKA Shoji

    Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering)   70 ( 4 )   I_721 - I_726   2014

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    Language:Japanese   Publisher:Japan Society of Civil Engineers  

    Understanding of the propagation mechanisms of the discharge and water level hydrographs in river channels is important for proper river management. It has been known that discharge hydrographs of flood flows passing through channel contractions are distorted by longitudinal difference of the storage volume of water in the channel. In this case, propagation mechanisms of the discharge and water level hydrographs are different, unlike in the case of the flood flow through a uniform channel. This paper characterize a part of the storage volume of water that causes the distortion of a discharge hydrograph as retarding storage volume of water and its evaluation method is proposed. We apply this method to a large flood through the valley of the Kitakami River and propagation mechanisms of the discharge and water level hydrographs are explained with relation to the storage volume and retarding storage volume of flood water.

    DOI: 10.2208/jscejhe.70.i_721

    DOI: 10.2208/prohe1975.27.721

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  • NUMERICAL ANALYSIS OF FLOOD FLOWS AND BED VARIATIONS AT THREE RIVER CONFLUENCES : INTRODUCING MOMENTUM FLUX FROM NON-ORTHOGONAL DIRECTION OF GRID LINE

    竹村 吉晴, 福岡 捷二, 杉村 貴志

    水工学論文集 土木学会水工学委員会 編   57 ( 4 )   1_805 - 810   2013

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    Language:Japanese   Publisher:土木学会  

    In this study, the quasi-3D model composed of depth-integral vortex equation and shallow water equations was extended on the basis of finite volume method employing non-orthogonal grids for properly evaluating complex boundary of the confluences. And, we developed the flux integral method considering non-orthogonal direction of grid line based on the CIP-CSL scheme for evaluating the convection terms more accurately also in the complex flow field of the confluence. The extended quasi-3D model was applied to recent large floods at the Go River confluences to investigate the flood flow and bed variation during the flood events. From the calculation results, we clarified that separation zones formed at the confluences have pronounced effects on the three dimensional flow structure and bed variations for the downstream channel.

    DOI: 10.2208/jscejhe.69.I_805

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  • NUMERICAL ANALYSIS OF FLOOD FLOWS AND BED VARIATIONS AT THREE RIVER CONFLUENCES - INTRODUCING MOMENTUM FLUX FROM NON-ORTHOGONAL DIRECTION OF GRID LINE

    TAKEMURA Yoshiharu, FUKUOKA Shoji, SUGIMURA Takashi

    Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering)   69 ( 4 )   I_805 - I_810   2013

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    Language:Japanese   Publisher:Japan Society of Civil Engineers  

    In this study, the quasi-3D model composed of depth-integral vortex equation and shallow water equations was extended on the basis of finite volume method employing non-orthogonal grids for properly evaluating complex boundary of the confluences. And, we developed the flux integral method considering non-orthogonal direction of grid line based on the CIP-CSL scheme for evaluating the convection terms more accurately also in the complex flow field of the confluence. The extended quasi-3D model was applied to recent large floods at the Go River confluences to investigate the flood flow and bed variation during the flood events. From the calculation results, we clarified that separation zones formed at the confluences have pronounced effects on the three dimensional flow structure and bed variations for the downstream channel.

    DOI: 10.2208/jscejhe.69.I_805

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  • PROPAGATION AND TRANSFORMATION MECHANISM OF WATER LEVEL AND DISCHARGE HYDROGRAPHS OF FLOOD FLOWS THROUGH RIVER VALLEY

    竹村 吉晴

    大学院研究年報 理工学研究科篇   ( 42 )   2012.7

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  • EFFECTS OF RIVER MORPHOLOGY ON PROPAGATION AND TRANSFORMATION OF DISCHARGE AND WATER LEVEL HYDROGRAPHS OF FLOOD FLOWS THROUGH RIVER VALLEY

    TAKEMURA Yoshiharu, FUKUOKA Shoji

    Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering)   68 ( 1 )   35 - 54   2012

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    Publisher:Japan Society of Civil Engineers  

    &amp;nbsp;In this paper, first, we discuss the physical interpretation of prop agation and transformation of water level hydrographs and discharge hydrographs by one dimensional equations for flood flows. And, relationships between storage volume of flood flows and propagation and transformation of discharge hydrographs are discussed for rivers with longitudinal changes in cross sections. From above discussions, we define &quot;retarding storage volume of flood&quot; which is the storage volume of flood when average velocities are decreasing during rising period of water levels.&lt;br&gt;&amp;nbsp;By using unsteady two dimensional flow analysis, we estimate water level hydrographs and discharge hydrographs of large floods through the valleys of the Kitakami River and the Go River. From this analysis, propagation and transformation characteristics of water level hydrographs and discharge hydrographs are explained with relation to river morphology, storage volume and retarding storage volume of flood in the river valleys. Finally, we discuss the application of this study for river plan ning and river management.

    DOI: 10.2208/jscejhe.68.35

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  • PROPAGATION CHARACTERISTICS OF FLOOD FLOWS THROUGH GORGE SECTION IN RIVERS

    竹村 吉晴

    大学院研究年報 理工学研究科篇   ( 40 )   2010.7

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  • Propagation and Storage Volume of Flood Flows in River with A Series of Small Hydropower Dams

    TAKEMURA Yoshiharu, FUKUOKA Shoji, ASAMI Kazuto

    Journal of Japan Society of Hydrology & Water Resources   23 ( 2 )   129 - 143   2010.3

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    Language:Japanese   Publisher:水文・水資源学会  

    DOI: 10.3178/jjshwr.23.129

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  • Propagation and Storage Volume of Flood Flows in River with A Series of Small Hydropower Dams

    TAKEMURA Yoshiharu, FUKUOKA Shoji, ASAMI Kazuto

    JOURNAL OF JAPAN SOCIETY OF HYDROLOGY & WATER RESOURCES   23 ( 2 )   129 - 143   2010

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    Language:Japanese   Publisher:THE JAPAN SOCIETY OF HYDROLOGY AND WATER RESOURCES  

    A series of small hydropower dams have been constructed along gorge sections of river in Japan. It is important to study hydraulic characteristics of flood flow associated with hydropower dams which will be usable for the future flood control management. At first, we show the effect of the gate operation of small hydropower dam on flood propagation speed and discharge hydrographs from observed results and unsteady 1D flow analysis which was developed so as to consider the effect of the gate operation. Secondary, storage functions of a gorge with a series of small hydropower dams are evaluated on the basis of the results of unsteady 1D flow analysis before and after the construction of a series of small hydropower dams.

    DOI: 10.3178/jjshwr.23.129

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  • PROPAGATION MECHANISM OF FLOOD FLOWS THOUGHT GORGE SECTION OF THE GO RIVER AND KITAKAMI RIVER

    TAKEMURA Yoshiharu, FUKUOKA Shoji, WAKO Takatoshi, OHGA Yoshikazu

    Advances in River Engineering   16   425 - 430   2010

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    Language:Japanese   Publisher:Japan Society of Civil Engineers  

    There are a lot of river with long gorge sections in Japan. Because considering the balance of upstream and downstream reaches is the base of the flood control management, river improvement in gorge sections is a fundamental issue. So, it is important to understand the flood propagation mechanism in gorge sections. But because of the lack of the observed data in gorge sections, enough studies have not been conducted.

    In this study, we show the mechanism of flood propagation and the effect of the channel form on flood propagation in the gorge section of the Go River and Kitakami River from observed data and using the unsteady 2-D flow analysis.

    DOI: 10.11532/river.16.0_425

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Awards

  • 2024年度 河川技術シンポジウム 優秀発表賞

    2024.6   土木学会水工学委員会   大河津分水路新第二床固の段階施工計画の数値解析技術(Q3D-FEBS)による改善

    竹村吉晴

  • 令和3年度土木学会全国大会第76回年次学術講演会優秀講演者

    2021   土木学会   自立高さを考慮した河岸侵食プロセスの解析法と常願寺川現地実験への適用

  • 令和2度土木学会論文奨励賞

    2021   土木学会   波状跳水・完全跳水及びその減勢区間における境界面(水面・底面)上の流れの方程式を用いた非静水圧準三次元解析(Q3D-FEBS)

  • 平成30年度土木学会全国大会第73回年次学術講演会優秀講演者

    2018   土木学会   大型床固めに連接する魚道周辺の三次元流況―大型水理実験と準三次元解析による比較検討

  • 第35回関東支部技術研究発表会優秀発表者

    2008   土木学会関東支部   渓谷部を流下する洪水流の水位ハイドログラフの変形と伝播速度

  • 平成20年度土木学会全国大会第63回年次学術講演会優秀講演者

    2008   土木学会   渓谷河道域における洪水波形の変形についての検討

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Research Projects

  • 河口域の土砂動態解明に向けた洪水流と波浪の非静水圧準三次元解析法の開発と応用

    Grant number:23K04050  2023.4 - 2026.3

    日本学術振興会  科学研究費助成事業 基盤研究(C)  基盤研究(C)  中央大学

    竹村 吉晴

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    Grant amount: \4420000 ( Direct Cost: \3400000 、 Indirect Cost: \1020000 )

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  • Development of an analysis method for flushing of river mouth gravel bar due to erosion

    Grant number:20K04711  2020.4 - 2023.3

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (C)  Grant-in-Aid for Scientific Research (C)  Chuo University

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    Grant amount: \3900000 ( Direct Cost: \3000000 、 Indirect Cost: \900000 )

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  • 石礫河川における三次元局所流と非平衡流砂運動を考慮した河岸・堤防の侵食解析手法の開発

    2020.4 - 2022.3

    国土交通省  河川砂防技術研究開発公募 河川技術分野 

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  • 物部川河口部における洪水流による礫州の破壊機構と河口閉塞対策に関する研究

    2018.4 - 2020.3

    国土交通省  河川砂防技術開発公募 

    竹村吉晴

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    Authorship:Principal investigator  Grant type:Competitive

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  • 波状跳水から完全跳水への遷移を伴う流れと水面変動の準三次元解析法の研究

    2018.4 - 2020.3

    日本学術振興会  科研費 

    竹村吉晴

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    Authorship:Principal investigator  Grant type:Competitive

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  • 江の川三川合流部における洪水流・河床変動予測モデルと背水域を含む本・支川河道が洪水流の伝播・変形に与える効果の定量化に関する研究

    2014.4 - 2016.3

    国土交通省  河川砂防技術開発公募 

    竹村吉晴

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    Authorship:Principal investigator  Grant type:Competitive

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  • 河道貯留による流量ハイドログラフの変形機 構と流量低減効果の定量化に関する研究

    2014.4 - 2015.3

    河川財団  河川整備基金助成 

    竹村吉晴

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    Authorship:Principal investigator  Grant type:Competitive

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