Japan Geoscience Union Meeting 2015

Presentation information

Oral

Symbol A (Atmospheric and Hydrospheric Sciences) » A-HW Hydrology & Water Environment

[A-HW27] Water and material transport and cycle in watersheds: from headwater to coastal area

Sun. May 24, 2015 4:15 PM - 6:00 PM 301B (3F)

Convener:*Shinji Nakaya(Department of Civil Engineering, Faculty of Engineering, Shinshu University), Mitsuyo Saito(Graduate School of Environmental and Life Science, Okayama University), Shin-ichi Onodera(Graduate School of Integrated and Arts Sciences, Hiroshima University), Kazuhisa Chikita(Department of Natural History Sciences, Faculty of Science, Hokkaido University), Tomohisa Irino(Faculty of Environmental Earth Science, Hokkaido University), Masahiro Kobayashi(Forestry and Forest Products Research Institute), Seiko Yoshikawa(Narional Institute for Agro-Environmental Sciences), Noboru Okuda(Research Institute for Humanity and Nature), Chair:Kazuhisa Chikita(Department of Natural History Sciences, Faculty of Science, Hokkaido University), Masahiro Kobayashi(Forestry and Forest Products Research Institute)

4:30 PM - 4:45 PM

[AHW27-23] Bed load transport by floods based on the sedimentological analysis of river bed deposits sampled in Chikugo River

*Tomio INAZAKI1 (1.Public Works Research Institute)

Keywords:Chikugo River, river mouth, sediment core, flood, bed load

Sedimentological analysis was conducted to the cores sampled before and after floods at the same points in the estuary of the Chikugo River, Kyushu, southwest Japan. The analysis consisted of sedimentary structure observation to lacquer peels and digital soft X-ray images of the cores, dense and detailed grain size distribution analysis at 2 cm intervals, and susceptibility measurements. The purpose of this study was to understand sediment transport along the channel of Chikugo River, which is the largest river flowing into Ariake Sound where has taken place such severe environmental deteriorations as devastating decrease in fishery production, depletion of dissolved oxygen concentration, and enrichment of mud contents in the bottom deposits. Analyses of the river bed cores sampled at the mouth of the Chikugo River revealed 5 cm erosion of the surficial bed along with accretion of 36 cm thick sand-dominant deposits during the 5 months including 4 time flood events. It is possible to interpret that the sand rich surficial deposits, classified into medium to coarse sand, were transported through the channel to the mouth even by small to medium scale floods.