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古谷貴洋 1 ・山本浩一 2 ・速水祐一 3 ・濱田孝治 4 ・ 吉野健児 5 ・関根雅彦 6 Takahiro FURUTANI, Koichi YAMAMOTO,Yuichi HAYAMI,Takaharu HAMADA, Kenji YOSHINO and Masahiko SEKINE 1 山口大学大学院理工学研究科(〒755-8611山口県宇部市常盤台2-16-1) 2 正会員 准教授 山口大学院理工学研究科(〒755-8611山口県宇部市常盤台2-16-1) 3 准教授 佐賀大学低平地沿岸海域研究センター(〒840-8502 佐賀県佐賀市本庄町1番地) 4 正会員 准教授 佐賀大学低平地沿岸海域研究センター(〒840-8502 佐賀県佐賀市本庄町1番地) 5 特別研究員 佐賀大学低平地沿岸海域研究センター(〒840-8502 佐賀県佐賀市本庄町1番地) 6 正会員 教授 山口大学院理工学研究科(〒755-8611山口県宇部市常盤台2-16-1) Long term observation was carried out for the measurement of the suspended sediment transport in the inner part of the Ariake Bay, Japan. Acoustic Doppler Current Profilers were used to estimate the vertical distributions of the suspended particle matter. As a consequence, estimated vertical suspended sediment fluxesfor the two sections were calculated. The results showed that the suspended sediment came from the offshore regularly and it accumulated on the tidal flat. In the season of the laver cultivation, suspended sediment from offshore seemed to be inhabited by the field of the laver cultivation. After the season of the laver cultivation, suspended sediment moved again to the tidal flat. On the other hand, strong rainfall on the direct rainfall made surface sediment run off to the offshore. Bottom mud density and shear strength change seemed to be matched with the vertical suspended sediment budget in the observed points.

SEASONAL VARIATION CHARACTERISTICS OF THE SUSPENDED SEDIMENT TRANSPORTATION IN THE MUDFLAT OF THE ARIAKEBAY