Zobrazeno 1 - 10
of 141
pro vyhledávání: '"ASHIDA, Kazuo"'
Publikováno v:
京都大学防災研究所年報. B. 35(B-2):41-62
A numerical model is developed based on a two-layer flow model for the purposes of predicting the flow and the bed evolution of alluvial rivers with complicate geometries including the case of compound channel flow. The reasons for using a two-layer
Publikováno v:
京都大学防災研究所年報. B. 35(B-2):63-78
Braided channels which are generally produced in mountain streams, vary spatially and temporally. The channel processes are composed of widening phase, bifurcating phase and merging phase.In this paper, flume tests are conducted to investigate wideni
Autor:
ASHIDA, Kazuo, SAWADA, Toyoaki
Publikováno v:
京都大学防災研究所年報. B. 35(B-2):29-39
Observational studies on the runoff, sediment yield and the sediment transport have been carried out in an experimental basin, the Ashiaraidani creek (6.5 km^2), which is a tributary of the Jintsu River.(1) The relation between sediment yield and rai
Autor:
Study Group for Laboratory Automation in Sediment Hydraulics, IMAMOTO, Hirotake, SAWAI, Kenji, FUJITA, Yuichiro, UTAMI, Tadashi, ASHIDA, Kazuo, TAKAHASHI, Tamotsu, EGASHIRA, Shinji, SATOFUKA, Yoshihumi, MURAMOTO, Yoshio, KAWATA, Yoshiaki, FUJIKI, Shigeo, FUJIHARA, Seiji, TSUCHIYA, Yoshito, UENO, Testuo, NAKAGAWA, Hajime, YAMASHITA, Takao, ISHIGAKI, Taisuke
Publikováno v:
京都大学防災研究所年報. B. 35(B-2):389-402
This study was carried out as a joint work among the research sections of DPRI concerning with experimental hydraulics. Various methods and problems about the measurement, control and analysis in sediment hydraulics were discussed and some of them we
Autor:
ASHIDA, Kazuo
Publikováno v:
京都大学防災研究所年報. A. 35:65-81
The author has engaged in the research on erosion, sediment transport and sedimentation for forty years since his graduation from Kyoto University in 1952 to the time of his retirement from Kyoto University in 1992.Firstly, he stressed the importance
Publikováno v:
京都大学防災研究所年報. B. 35(B-2):79-88
The flow characteristics of fine sands and water mixture is discussed in terms of experimented results concerning the flow resistance, sediment concentration profiles and sediment diffusion. (1) Flow resistance does not change so much in the range of
Autor:
ASHIDA, Kazuo, SAWADA, Toyoaki
Publikováno v:
京都大学防災研究所年報. B. 34(B-2):209-220
Field survey and observation were carried out for clarifying the real situation of sediment yield on a bare slope, sediment runoff in the steep channel, and debris flow on the Ashiaraidani creek (6.5 hA), which is a tributary of the Jintsu River.(1)
Publikováno v:
京都大学防災研究所年報. B. 34(B-2):247-260
Braided channels are generally produced in mountain streams with very active sediment yields.Such channels vary spatially and temporally, which results in a big variation of the sediment discharge.The bed material is composed of a wide range of grain
Publikováno v:
京都大学防災研究所年報. B. 34(B-2):261-274
In the previous paper^1)- the authors presented a bed-load equation which was derived from their constitutive relations of debris flow. The equation underestimates somewhat the bed-load rate in the range of non-dimensional shear stress smaller than 0
Autor:
ASHIDA, Kazuo, EGASHIRA, Shinji, SATOFUKA, Yoshifumi, LIU, Bingyi, UMEMOTO, Masaki, KAWATA, Toshiki
Publikováno v:
京都大学防災研究所年報. B. 34(B-2):221-246
In most rivers in Japan, tolerable degradation occurs because of the sediment trap by the reservoirs upstream, and the severe gravel mining which was done during the period of rapid increase in economy.As a result, disasters during flood have been in