The bathymetric evolution of the northeast part of the Ariake Sea and the Estuarine Channel of the Chikugogawa River was studied and the seasonal variations in the sediment phosphorus distribution in the region were analyzed. The tidal prism of a river mouth estuary determines the channel size of the main ebb tidal delta. The muddy bed of the estuarine channel was eroded by flood discharge, and the mixture of the bed materials and the discharged suspended sediments from the river basin deposited in the sandy delta.
The high concentrations of Al-P, Fe-P, residual organic P, and TOC in the fine sediment were continuously distributed from the sandy Chikugogawa river mouth delta to the muddy tidal flat in the front of the Rokkakugawa river mouth after the flood season. The size of the surface particles in the delta increased and the concentration of organic matter increased during the dry season.
These facts suggest that the fine silt and clay settled on the Chikugogawa river mouth delta are eroded by the tidal current, and a part of these particles return to the estuarine channel; the remaining particles migrate to the southwest sea area of the tidal flat. The suspended sediment around the delta is transported to the tidal flat that is offshore of the Rokkakugawa river mouth by estuarine circulation occurring in the innermost bay of the Ariake Sea.
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