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KOUE Jinichi
Graduate School of Maritime Sciences / Department of Maritime Sciences
Assistant Professor

Researcher basic information

■ Research Keyword
  • Oceanology and Limnology
  • Gravity current
  • Structure of stratification
  • Hydrology
  • Climate change
  • Lake Biwa
  • Shock Wave
  • Cavitation
■ Research Areas
  • Natural sciences / Atmospheric and hydrospheric science
  • Aerospace, marine, and maritime Engineering / Marine and maritime engineering
  • Environmental science/Agricultural science / Environmental dynamics

Research activity information

■ Paper
  • Jinichi Koue
    This study provides a comprehensive examination of colliding density currents with a range of density differences from 1% to 4%, using controlled laboratory experiments with saltwater and freshwater. The research reveals that when density currents collide, they generate internal bore, with the denser fluid flowing consistently beneath the lighter fluid. A significant finding is the temporary stalling and oscillatory motion of the current fronts during collisions, which is linked to a partial dissipation of kinetic energy and the subsequent formation of internal waves. Numerical simulations showed close agreement with experimental observations, reproducing the location of the tidal fronts well and verifying the accuracy of the hydrodynamic model used. Moreover, the study demonstrates that collisions between fluids with different densities notably enhance diffusion and mixing efficiency. This has important implications for environmental science, particularly in understanding and predicting density-driven fluid dynamics in aquatic systems such as estuaries and coastal zones. The enhanced mixing efficiency observed could be crucial for applications in environmental and pollution control, offering insights into material transport and pollutant dispersion.
    MDPI AG, Feb. 2025, Journal of Marine Science and Engineering, 13(2) (2), 363 - 363
    [Refereed]
    Scientific journal


  • Jinichi Koue
    AbstractThis study investigates the intricate dynamics of nutrient transport and stratification in Lake Biwa, highlighting the significant impact of river inflows on water quality. Utilizing a validated three-dimensional flow field model and ecosystem model including a bottom sediment model, the analysis revealed that nutrient concentrations, specifically NH₄⁺, NO₂⁻, NO₃⁻, and PO₄3⁻, exhibited pronounced seasonal variations. In the RN_double scenario, NH₄⁺ and NO₂⁻ concentrations demonstrated a slight increase of 0.1 µg/L, respectively, while NO₃⁻ concentrations rose by 0.05–0.10 µg/L in response to precipitation changes. Conversely, in the RN_half scenario, NH₄⁺ and NO₂⁻ concentrations decreased, with NO₃⁻ seeing a more substantial decline of approximately 0.1 µg/L, attributed to reduced precipitation. PO₄3⁻ levels exhibited a maximum decrease of 0.03 µg/L from summer to autumn. Furthermore, simulations limiting nutrient inflows indicated a modest reduction in concentrations: NH₄⁺ decreased by approximately 0.03 µg/L during summer, and NO₂⁻ decreased by around 0.05 µg/L from spring to summer. The results suggest that while immediate improvements in dissolved oxygen levels are limited, effective long-term nutrient management could stabilize oxygen concentrations and improve overall water quality. These findings underscore the necessity for comprehensive water management strategies to mitigate eutrophication effects and support the ecological health of Lake Biwa.
    Dec. 2024, Terrestrial, Atmospheric and Oceanic Sciences, English
    [Refereed]
    Scientific journal

  • Jinichi Koue
    Density currents, fluid flows driven by differences in density, play a crucial role in disaster prevention for water pollution and tsunami mitigation, particularly due to thermal releases from power plants. Understanding their dynamics is pivotal for effective mitigation strategies. While the influence of seabed and lake bottom topography on density currents is well-studied, research on how embankment shapes affect these currents has been limited. This study aimed to fill this gap by experimentally and numerically analyzing the flow dynamics of density currents using various embankment shapes in a controlled water tank environment. The findings revealed distinct variations in density perturbation across different embankment shapes. Specifically, density currents exhibited reduced head velocities in embankments shaped as right-angled triangles, rectangles, and L-shapes, in that sequential order. This research underscores the significance of embankment design in modifying density currents, offering valuable insights for optimizing disaster management strategies related to water pollution and tsunami hazards induced by thermal effluents from industrial sources.
    Nov. 2024, Water, English
    [Refereed]
    Scientific journal

  • Akihisa Abe, Jinichi Koue
    Jul. 2024, Marine Engineering, English
    Scientific journal

  • Jinichi Koue
    This study investigates enclosed water bodies to understand the intricate interactions among physical, chemical, and biological processes. A one-dimensional model, integrating sediment and ecosystem components, was developed to analyze oxygen depletion, nutrient dynamics, and the influence of sediment organic matter on oxygen concentrations due to stratification. Oxygen and nutrient concentrations were derived by combining results from a one-dimensional vertical diffusion model with the ecosystem model. The dissolution, adsorption, and desorption of inorganic substances in bottom mud react differently under anaerobic and aerobic conditions, necessitating separate formulations for reduction and oxidation reactions in the bottom mud model. In Lake Biwa, Japan’s largest lake, dissolved oxygen levels have decreased despite regulatory efforts since the 1970s, prompting an investigation into the causes of oxygen-depleted water masses. The model was thus applied to examine oxygen consumption in Lake Biwa’s deep sediments, shedding light on anoxia in enclosed water bodies. This study emphasizes the significance of bottom sediments in water quality models and their implications for ecosystems. Furthermore, the adaptive nature of this model allows for its application in various water bodies, including freshwater reservoirs, lakes, and saltwater bays.
    Jul. 2024, Water (Switzerland), 16(13) (13)
    [Refereed]
    Scientific journal

  • Jinichi Koue, Saori Shyu, Akihisa Abe
    International Society of Offshore and Polar Engineers, Mar. 2024, International Journal of Offshore and Polar Engineering, 34(1) (1), 93 - 100
    [Refereed]
    Scientific journal

  • Jinichi Koue, Satoshi Onishi, Akihisa Abe
    International Society of Offshore and Polar Engineers, Mar. 2024, International Journal of Offshore and Polar Engineering, 34(1) (1), 67 - 74
    [Refereed]
    Scientific journal

  • Jinichi Koue
    This study examines the potential impacts of climate change on Lake Biwa, Japan’s largest freshwater lake, with a focus on temperature, wind speed, and precipitation variations. Leveraging data from the IPCC Sixth Assessment Report, including CCP scenarios, projecting a significant temperature rise of 3.3–5.7 °C in the case of very high GHG emission power, the research investigates how these shifts may influence dissolved oxygen levels in Lake Biwa. Through a one-dimensional model incorporating sediment redox reactions, various scenarios where air temperature and wind speed are changed are simulated. It is revealed that a 5 °C increase in air temperature leads to decreasing 1–2 mg/L of dissolved oxygen concentrations from the surface layer to the bottom layer, while a decrease in air temperature tends to elevate 1–3 mg/L of oxygen levels. Moreover, doubling wind speed enhances surface layer oxygen but diminishes it in deeper layers due to increased mixing. Seasonal variations in wind effects are noted, with significant surface layer oxygen increases from 0.4 to 0.8 mg/L during summer to autumn, increases from 0.4 to 0.8 mg/L in autumn to winter due to intensified vertical mixing. This phenomenon impacts the lake’s oxygen cycle year-round. In contrast, precipitation changes show limited impact on oxygen levels, suggesting minor influence compared to other meteorological factors. The study suggests the necessity of comprehensive three-dimensional models that account for lake-specific and geographical factors for accurate predictions of future water conditions. A holistic approach integrating nutrient levels, water temperature, and river inflow is deemed essential for sustainable management of Lake Biwa’s water resources, particularly in addressing precipitation variations.
    2024, Acta Geochimica
    [Refereed]
    Scientific journal

  • Jinichi Koue
    Abstract Climate change-induced extreme weather events, including prolonged droughts and intense rainfall, exert a significant influence on river inflows. These inflows act as vital conduits for nutrient transport, water quality modulation, and the regulation of thermal dynamics in lakes and oceans. In this context, this study conducts a comprehensive examination of the multifaceted effects stemming from river water characteristics, snowmelt water influence, and shifts in precipitation patterns on the stratification dynamics of Lake Biwa in Japan. To facilitate these investigations, a hydrodynamic model was developed to simulate thermal stratification in Lake Biwa. The results demonstrate that an increase in precipitation and river water flow, specifically doubling these factors, leads to noticeable cooling of the lake’s surface layer and a consequent destabilization of stratification during the stratification period. Conversely, halving these factors stabilizes stratification. Furthermore, elevating river water temperature by 5 °C raises water temperature near the upper thermocline, encouraging vertical mixing within the surface layer. Conversely, a 5 °C decrease induces significant temperature fluctuations and an unstable stratification extending from the surface to deeper layers. Notably, the spatial variance in water temperature within Lake Biwa is profoundly influenced by fluctuations in river water temperature. This study underscores the critical importance of considering river plumes in the study of material circulation, stratification dynamics, and ecological well-being in lakes and oceans. Given the mounting concerns related to eutrophication and the prevalence of anoxia in aquatic ecosystems, this research provides invaluable insights into assessing the impacts of river plumes on Lake Biwa’s stratification structure and seasonal dynamics.
    Springer Science and Business Media LLC, Dec. 2023, Environmental Processes, 10(4) (4)
    [Refereed]
    Scientific journal

  • Jinichi Koue
    May 2023, Theoretical and Applied Mechanics Letters, 100439
    [Refereed]
    Scientific journal

  • EFFECTS OF STRONG WINDS ON THE BOTTOM LAYER DURING THE WEAK STRATIFICATION PERIOD IN LAKE BIWA, JAPAN
    Jinichi Koue
    Apr. 2023, International Journal of GEOMATE, Vol. 24(104), 44 - 52
    [Refereed]

  • DYNAMIC EFFECTS OF THE HEAD EDGE BEHAVIOR OFGRAVITY CURRENT
    Jinichi Koue
    Mar. 2023, International Journal of GEOMATE, Vol. 24(103), 128 - 135
    [Refereed]

  • Jinichi Koue, Hikari Shimadera, Tomohito Matsuo, Akira Kondo
    Abstract The currents of gyre (circulation) flow play an important role in the transportation and mixing of dissolved or suspended nutrients and chemical substances. In recent years, the climate change has affected the flow field in Lake Biwa. However, how much the climate change can influence the flow field has not been clarified enough yet. In the present study, using a three-dimensional hydrodynamic model, we investigated the effect of changes in air temperature, wind speed, and precipitation on the change of the flow field in Lake Biwa. For sensitivity analysis, numerical simulations were performed for a baseline case using realistic meteorological data from 2007 to 2012, as well as hypothetical cases using meteorological data. The analysis revealed that the change in air temperature and precipitation changed stratification and vorticity in the surface layer in each season. The strength of the stratification affected the gyre strength in the surface layer. The change in wind speed, on the other hand, changed the wind stress acting on the lake's surface, influencing the strength of gyre significantly. Increased wind speed lengthened the radius of the gyre in Lake Biwa, while decreased wind speed made it weaker above and below the thermocline.
    IWA Publishing, Mar. 2023, Journal of Hydroinformatics
    [Refereed]
    Scientific journal

  • STUDY ON THE ANALYSIS OF THE CONTROLLING FACTORS OF HYPOXIA IN THE BOTTOM OF LAKE BIWA, JAPAN
    Jinichi Koue
    Feb. 2023, International Journal of GEOMATE, 24(102) (102), 101 - 108
    [Refereed]

  • Jinichi Koue
    Jan. 2023, International Journal of GEOMATE, 24(101) (101), 11 - 117
    [Refereed]
    Scientific journal

  • Jinichi Koue
    Hypoxia in Lake Biwa, Japan remains a serious water environmental problem. One of the causes of hypoxia in the lake is the formation of a thermocline, which is largely affected by meteorological factors, such as (1) air temperature, (2) wind speed, and (3) precipitation. However, the effects of these three meteorological factors on the formation of the thermocline have not been clarified quantitatively. In this study, applying a three-dimensional hydrodynamic model to Lake Biwa, the effects of each of the three meteorological elements on the formation of the thermocline was quantitatively analyzed to clarify the governing factors of meteorological conditions in the formation of anoxic oxygen. Sensitivity analysis of the stratification structure in Lake Biwa was performed by changing the three meteorological factors of (1) air temperature, (2) wind speed, and (3) precipitation. As a result, the change in wind speed gives the greatest effect on the stratification structure, the change in air temperature makes the difference in the stratification structure from the surface layer to the vicinity of the thermocline, and the change in precipitation affects it less than the others.
    MDPI, Jan. 2022, HYDROLOGY, 9(1) (1), English
    [Refereed]
    Scientific journal

  • Jinichi Koue, Hikari Shimadera, Tomohito Matsuo, Akira Kondo
    The dynamics of dissolved oxygen in lake is a fundamental issue of comprehending the water environmental habitats of aquatic organisms. In recent years, the decrease in dissolved oxygen has been observed at the bottom of the northern part of Lake Biwa, Japan. In recent years, eutrophication and global warming caused the decrease in the dissolved oxygen in the deep layer. Under these circumstances, in order to preserve the ecosystem of Lake Biwa and to provide water resources, the environmental changes in Lake Biwa should be accurately grasped. In our present study, a water quality model considering the flow field from hydrodynamic model was developed in order to grasp the concentration of phytoplankton, zooplankton, nitrogen, phosphorus, dissolved oxygen and chemical oxygen demand in Lake Biwa. Numerical simulation was carried out for 3 years from 2007 to 2009. Comparisons of the simulations with the observations showed that the seasonal and interannual change of dissolved oxygen was well reproduced. The dissolved oxygen decreased during decomposing the organic matter by bacteria in the bottom layer with little oxygen supply from the atmosphere and the photosynthesis from the phytoplankton under the thermocline from spring to autumn. The simulation confirmed that in each year, the dissolved oxygen was supplied in all layers by the overturning in winter.
    GEOMATE INT SOC, Feb. 2020, INTERNATIONAL JOURNAL OF GEOMATE, 18(66) (66), 56 - 61, English
    [Refereed]
    Scientific journal

  • Jinichi Koue, Hikari Shimadera, Tomohito Matsuo, Akira Kondo
    Climatic factors such as air temperature and wind speed can affect the structure of stratification in Lake Biwa. In general, the rise in air temperature and the decrease in wind speed weaken the vertical mixing and strengthen the structure of the stratification, which interrupts the transport of the substances. However, how much the change of each climate element can influence the structure of the stratification is not clarified. Therefore, it is important to evaluate the effects of each element on the stratification quantitatively. In the present study, we investigated the effect of the change in air temperature and wind speed on the seasonal change of stratification in Lake Biwa by using a three-dimensional hydrodynamic model. Numerical simulations were carried out for a baseline case using realistic meteorological data from 2007 to 2012 and hypothetical cases using meteorological data with modified air temperature or wind speed for sensitivity analysis. The analysis showed that the increase and decrease in air temperature changed the vertical water temperature uniformly in almost all layers. Thus, the strength of the stratification is hardly changed. The increase and decrease in wind speed, however, altered the water temperature near the surface of the lake, so that it significantly influenced the stratification. The increase in wind speed made the water parcels of the surface layer well mixed, and the decrease in wind speed made the mixed layer thinner.
    MDPI AG, Oct. 2018, Water, 10(10) (10), 1492 - 1492
    [Refereed]
    Scientific journal

  • Jinichi Koue, Hikari Shimadera, Tomohito Matsuo, Akira Kondo
    Water temperature near the surface of a lake increases with increasing air temperature, which results in stratification. The strength of stratification substantially influences the transport of water parcels from the surface to the bottom of a lake. In recent years, the stratification in Lake Biwa-the largest freshwater lake in Japan-has been stronger. However, it is difficult to reproduce the stratification well in the simulations. In the present study, we built a hydrodynamic model for the purpose of analyzing the structure of the stratification in detail. Using the model, we evaluated the reproducibility of the seasonal and annual changes of vertical water distribution and flow field in Lake Biwa from 2007 to 2011. The hydrodynamic model results show that the vertical water distribution approximately agrees with the field observations based on the statistical analysis. The seasonal change of thermal stratification is reasonably reproduced by the hydrodynamic model simulations. In the simulation, there are mainly two circulation flows at the surface layer of the lake. The first flows anticlockwise and the second flows clockwise in the northern part of Lake Biwa. In order to compensate for the surface water flow, the water under the thermocline sometimes flows in the opposite direction under each circulation flow.
    MDPI AG, Jan. 2018, Water (Switzerland), 10(1) (1), English
    [Refereed]
    Scientific journal

  • Jinichi Koue, Hikari Shimadera, Tomohito Matsuo, Akira Kondo
    Water temperature near the surface of a lake increases with increasing air temperature, which results in stratification. The strength of stratification substantially influences the transport of dissolved oxygen from the surface to the bottom water of a lake. In recent years, the decrease in dissolved oxygen at the bottom of the northern part of the Lake Biwa, the largest freshwater lake in Japan, has been observed. The main cause of this is considered to be the change in stratification, which depends on weather and climate conditions. In the present study, numerical simulations were carried out to investigate the effect of strong wind on the structure of stratification in Lake Biwa. The baseline simulation was conducted using actual meteorological data, and experimental simulations were conducted using meteorological data with modified wind speed and direction. The numerical experiments showed that if the magnitude of the wind is strong enough, the stratification collapses and the wind can enhance the vertical mixing in the bottom layer even in the summer season with strong thermal stratification. In a stratified season, when the strong wind blows predominantly in one direction, the rate of the vertical mixing changes by the wind direction. Moreover, as the duration of the strong wind extends, vertical mixing easily occurs.
    GEOMATE International Society, 2018, International Journal of GEOMATE, 14(45) (45), 35 - 40, English
    [Refereed]
    Scientific journal

  • Koue Jinichi, Shimadera Hikari, Kondo Akira
    In recent years, the dissolved oxygen at the bottom of the Lake Biwa has been decreasing. It is considered that the decrease in precipitation (about 100 mm), the rise in temperature (about 1 or 2 Celsius degree), and the decrease in wind speed (about 5 %) during the past 20 years leads to this phenomena. In particular, the rise in air temperature and the decrease in wind speed weakens the vertical mixing, and it may cause the reason of low oxygenation at the bottom layer.
    In our present study, we show that we can reproduce the seasonal and inter-annual change of the structure of water stratification with developing the 3-dimensional hydrodynamic model. This model can reproduce the observed vertical water distribution in order to elucidate how the change of the stratification due to global warming will influence the low dissolved oxygen in Lake Biwa in the future.
    THE JAPAN SOCIETY OF HYDROLOGY AND WATER RESOURCES, 2016, Proceedings of 2016 Annual Conference, Japan Society of Hydrology and Water Resources, 29, 21 - 21, Japanese
    [Refereed]

  • Jun. 2009, International Offshore and Polar Engineering
    [Refereed]

  • Nov. 2008, 日本船舶海洋工学会 関西支部秋季講演会
    [Refereed]

■ Lectures, oral presentations, etc.
  • 河口部における流況制御が琵琶湖の水質環境に与える影響の解析
    川村竜斗, 公江仁一
    The 59th Annual Conference of JSWE, Mar. 2025

  • 平板間隙内キャビテーション噴流の衝撃波生成に関する研究
    公江仁一, 阿部晃久, 三村治夫
    2024年度衝撃波シンポジウム, Mar. 2025

  • 放電誘起キャビテーション噴流の衝撃波生成特性に関する研究
    公江仁一, 阿部晃久
    2024年度衝撃波シンポジウム, Mar. 2025

  • 金属棒材の打撃で誘起される水中衝撃波動と気泡生成挙動に関する研究
    阿部晃久, 公江仁一, 藤本岳洋
    2024年度衝撃波シンポジウム, Mar. 2025

  • Consideration of the Impact of River Inflows on Nutrient Dynamics and Water Quality in Enclosed Water Area
    Jinichi Koue
    The 14th International Conference on Geotechnique, Construction Materials and Environment, GEOMATE,, Nov. 2024

  • 閉鎖性水域における底泥の栄養塩・有機物濃度による密度変化の影響
    公江仁一
    土木学会 第52回環境システム研究論文発表会, Nov. 2024

  • Investigation on shock wave phenomena generated around a rod loaded to axial impact in water
    Jinichi Koue, Saori Shu, Akihisa Abe
    2023年度衝撃波シンポジウム, Mar. 2024

  • Consideration for Utilizing Shock Waves Generated by Cavitation-jets to Remove Marine Organisms
    Akihisa Abe, Jinichi Koue
    2023年度衝撃波シンポジウム, Mar. 2024

  • 先端形状が異なる飛翔体の水中貫入による速度減衰効果の考察
    宮下晃, 公江仁一, 阿部晃久
    高速度イメージングとフォトニクスに関する総合シンポジウム, Dec. 2023

  • Exploring the Dynamics of River Inflow and its Effects on the Deep Layer of Lake Biwa through Numerical Simulations
    Jinichi Koue
    13th International Conference on Geotechnique, Construction Materials and Environment, Nov. 2023

  • Generation and behavior of underwater shock waves and microbubbles produced by metal plate discharge
    Jinichi Koue, Akihisa Abe
    The 34th International Symposium on Shock Waves (ISSW34), Jul. 2023

  • Experimental analysis of underwater noise produced by impacted bars
    Jinichi Koue, Saori Shyu, Akihisa Abe
    23rd International Offshore and Polar Engineering Conference, Jun. 2023

  • Compressible hydrodynamic consideration of cavitating jets on the scraping action of organisms attached on marine structures
    Jinichi Koue, Satoshi Onishi, Akihisa Abe
    23rd International Offshore and Polar Engineering Conference, Jun. 2023

  • 水中衝撃波と弾性膜の干渉によるOHラジカルの生成効果
    山下 理央, 公江 仁一, 阿部 晃久
    2022年度衝撃波シンポジウム, Mar. 2023

  • 先端形状が異なる飛翔体の水中貫入に伴う周囲流れの解析
    平井 龍志, 公江 仁一, 阿部 晃久
    2022年度衝撃波シンポジウム, Mar. 2023

  • 金属板を介した水中放電による衝撃波と微小気泡生成
    丸山 泉輝, 公江 仁一, 阿部 晃久
    2022年度衝撃波シンポジウム, Mar. 2023

  • Analysis of Seasonal and Interannual Variations in Dissolved Oxygen Concentration at the Bottom of Lake Biwa, Japan
    Jinichi Koue
    8th International Conference on Structure, Engineering and Environment, Nov. 2022

  • 付着物除去効果向上のためのキャビテーション噴流挙動の観測と解析
    大西智士, 公江仁一, 阿部晃久
    第92回(令和4年)マリンエンジニアリング学術講演会, Oct. 2022

  • 洋上風車パイル打設時の水中騒音発生メカニズムに関する研究
    鄒 思織, 宮下 晃, 公江 仁一, 阿部 晃久
    第92回(令和4年)マリンエンジニアリング学術講演会, Oct. 2022

  • Formation of metal carbide by electrochemical reduction of CO2 in molten LiCl-KCl
    Fukuda Haruka, Yamada Atsushi, Koue Jinichi, Suzuki Yuta, Goto Takuya, Isogai Tomohiro, Yamauchi Akiyoshi, Kishikawa Yosuke
    The 53th Symposium on Molten Salt Chemistry, Nov. 2021

  • Electrochemical Behavior of CO2 reduction in a phosphonium-based ionic liquid
    Tchorap-Yamamoto Shoma, Koue Jinichi, Suzuki Yuta, Kobatake Hidekazu, Goto Takuya, Isogai Tomohiro, Yamauchi Akiyoshi, Kishikawa Yosuke
    The 53th Symposium on Molten Salt Chemistry, Nov. 2021

  • Electrochemical reduction of CO2 in [DEME][BF4] containing H2O, The 53th Symposium on Molten Salt Chemistry
    Kozasa Kentaro, Koue Jinichi, Suzuki Yuta, Goto Takuya, Isogai Tomohiro, Yamauchi Akiyoshi, Kishikawa Yosuke
    The 53th Symposium on Molten Salt Chemistry, Nov. 2021

  • Effect of change of each meteorological element on the circulation in Lake Biwa, Japan
    Jinichi Koue, Hikari Shimadera, Tomohito Matsuo, Akira Kondo
    ECSA 58 - EMECS 13 Estuaries and coastal seas in the Anthropocene, Sep. 2021

  • Numerical simulation for seasonal and inter-annual change of dissolved oxygen in Lake Biwa, Japan
    Jinichi Koue, Hikari Shimadera, Tomohito Matsuo, Akira Kondo
    9th International Conference on Geotechnique, Construction Materials and Environment, Nov. 2019

  • Individual difference in skin blood flow with air temperature variation
    Otsuka Y, Maeda T, Shiochi S, Matsuo T, Shimadera H, Koue J, Kondo A
    International Workshop on Environmental Engineering 2019, Jun. 2019

  • Sensitivity Analysis of Structure of the Stratification in Lake Biwa by Changing Meteorological Elements
    Jinichi Koue, Hikari Shimadera, Tomohito Matsuo, Akira Kondo
    Conference: 17th world lake conference, Oct. 2018

  • Numerical assessment of the impact of strong wind on thermal stratification in Lake Biwa
    Jinichi Koue, Hikari Shimadera, Tomohito Matsuo, Akira Kondo
    7th International Conference on Geotechnique, Construction Materials and Environment, Nov. 2017

  • 琵琶湖における成層構造の季節経年変動の再現性
    公江仁一, 嶋寺光, 近藤明
    水文・水資源学会, Sep. 2016

  • 琵琶湖流動場モデルによる温度成層の再現性評価
    公江仁一, 近藤明, 嶋寺光, 武川さゆみ, 劉彦妮
    空気調和・衛生工学会近畿支部学術研究発表会, Mar. 2016

  • Structure of the Head of Gravity Currents in a Long Channel
    Jinichi Koue, Takuya Katayama, Testuo Katsuragi, Nobuhiro Baba, Kenichi Kitaura
    19th International Offshore and Polar Engineering Conference, Jun. 2009

  • 密度界面の不連続性における数値振動を抑制するスキームの開発
    公江仁一
    日本船舶海洋工学会 関西支部秋季講演会, Nov. 2008

■ Affiliated Academic Society
  • 衝撃波学会

  • 電気化学会

  • マリンエンジニアリング学会

  • 土木学会

  • 水文水資源学会

  • 日本船舶海洋工学会

■ Research Themes
  • Elucidation of the removing mechanism of marine organisms stuck to structure using cavitation jets and development of a nozzle expanding the removal effect area
    阿部 晃久, 藤本 岳洋, 公江 仁一, 三村 治夫
    Japan Society for the Promotion of Science, Grants-in-Aid for Scientific Research, Grant-in-Aid for Scientific Research (B), Kobe University, 01 Apr. 2023 - 31 Mar. 2027

  • 閉鎖性水域の貧酸素化の解消改善方法の提案
    公江仁一
    環境再生保全機構, 環境研究総合推進費, 神戸大学, Apr. 2023 - Mar. 2026, Principal investigator

  • 気候変動と富栄養化が閉鎖性水域に及ぼす影響評価
    公江仁一
    ひょうご科学技術協会, 学術研究助成金, 神戸大学, Apr. 2023 - Mar. 2024, Principal investigator

■ Industrial Property Rights
  • 一酸化炭素、又は有機化合物の製造方法
    後藤 琢也, 公江 仁一, 鈴木 祐太, 小笹 健太郎, 野崎 紗矢, チョラプ山本笙真, 磯貝 智弘, 岸川 洋介, 山内 昭佳
    特願2022-019162, 10 Feb. 2022, 特開2022-123865
    Patent right

  • METHOD FOR MANUFACTURING CARBON MONOXIDE OR ORGANIC COMPOUND
    GOTO Takuya, KOUE Jinichi, SUZUKI Yuta, KOZASA Kentaro, NOZAKI Saya, TCHORAP-YAMAMOTO Shoma, ISOGAI Tomohiro, KISHIKAWA Yosuke, YAMAUCHI Akiyoshi
    特願PCT/JP2022/005415
    Patent right

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