工学部

Masahiro Tamai

  (玉井 昌宏)

Profile Information

Affiliation
Professor, Faculty of Engineering, Department of Civil Engineering, Osaka Sangyo University

J-GLOBAL ID
201801002265996524
researchmap Member ID
7000023175

Papers

 69
  • TAMAI Masahiro
    Journal of Japan Society of Civil Engineers, Ser. G (Environmental Research), 76(7) III_511-III_519, 2020  
    The authors showed that cold nocturnal darainage flows break out in the northern part of Osaka Plain, can lower temperature of the part by 2℃ and have velocity profiles similar to those of gravity density currents on inclined plains. In the present study, numerical simulation using the WRF was conducted to examine structures and generation mechanisms of the flows. The accuracy of the calculation was checked by comparison with some existing meteorological data. The simulation results showed that the drainage flow which the authors have been studying is generated by outflow of cold air mass which accumulates in the Tada basin into Osaka Plain and there are other nocturnal drainages which flow on flood plains of the Akutagawa and Aigawa Rivers in the part.
  • TSUJIMOTO Gozo, TAMAI Masahiro
    Journal of Japan Society of Civil Engineers, Ser. B3 (Ocean Engineering), 75(2) I_725-I_730, 2019  
    A new method by the concept of entropy has been used to classify sediment color distribution. We objectively characterized the distribution profile and clarified the relationship between the geology and sediment characteristics. Sediment colors were defined by L*a*b* instead of RGB, and of the following four indexes, lightness, hue, saturation and chromaticity, lightness was the optimal index. In order to determine the optimal number of groups, a C-H criterion, Rs statistic and the skewness of the third moment on sediment color distribution were used. The sediment colors could be divided into 7 groups. Kagoshima Pref. has geology of the Shirasu plateaus, but the sediment color could be grouped by white minerals such as quartz and feldspar contained in granite and pyrophorite and colored minerals such magnetite contained in mafic volcanic rock, and therefore, they can be related to geology. In addition, it could be possible to make sediment transport path clear by focusing on a specific mineral such as olives.
  • TAMAI Masahiho, TSUJIMOTO Gozo
    Journal of Japan Society of Civil Engineers, Ser. B3 (Ocean Engineering), 74(2) I_808-I_813, 2018  
    Purposes of the present study are to obtain quantitatively color characteristics of sands which were collected in the mainland beaches in Kagoshima Pref., Japan and to examine relationships between the color characteristics and geological features of the surrounding area of the beaches. Some relationships between the two are clarified, such as that a lot of the beaches have sand colors of medium dark brown under the influence of late Pleistocene non-alkaline pyroclastic flow volcanic rocks, Holocene non-alkaline pyroclastic flow volcanic rocks and non-alkaline pyroclastic mafic volcanic rocks make beach sand color dark gray, and dark blown sands of some east coasts in Osumi Peninsula originate in middle Miocene to late Miocene granodiorite.
  • 玉井 昌宏
    Coastal Engineering Proceedings, 36, 2018  Peer-reviewed

Research Projects

 3

研究テーマ

 4
  • 研究テーマ(英語)
    大阪平野に流入する冷気流の流動構造とヒートアイランド現象に及ぼす影響に関する研究
    研究期間(開始)(英語)
    2010/04/01
  • 研究テーマ(英語)
    河川や海岸の砂の色彩の土砂管理における利用可能性に関する研究
    研究期間(開始)(英語)
    2013/04/01
  • 研究テーマ(英語)
    阿蘇山起源SO2の熊本平野や火口原における高濃度事象に関する研究
    研究期間(開始)(英語)
    2016/04/01
  • 研究テーマ(英語)
    都市域の農業用水路の治水機能に関する研究
    研究期間(開始)(英語)
    2017/04/01