2007•PROCEEDINGS OF HYDRAULIC ENGINEERINGOpen access

EFFECTS OF FLOOD PLAIN ON MAIN CHANNEL WITH FLOOD FLOW OF THE MATSUURA RIVER

Kunitoshi Watanabe, Ryuichi HIRAKAWA

Open full text 2 citations

Abstract

In the Matsuura river digs the ground in the rice field of Azame down because there were for a long time a lot of floods, makes a flood plain there, and the natural regeneration business that starts restore the marsh is done. In this study, the flow including this Azame was analyzed by the numerical simulation. As a result of the numerical experiment, it was understood to be suppressed even to about the half when the flood plain existed while flow velocity in the narrow section reached 4.5m/s in the current state without the flood plain river channel at the flow rate peak. Moreover, the source location of the maximum flow velocity shifted to the left bank neighborhood though the peak at the flow velocity of the main current part in the flood plain downstream edge was suppressed by about 60% of the current state river channel.

Open-access reader

About this research paper

What this paper is about

In the Matsuura river digs the ground in the rice field of Azame down because there were for a long time a lot of floods, makes a flood plain there, and the natural regeneration business that starts restore the marsh is done. In this study, the flow including this Azame was analyzed by the numerical simulation. As a result of the numerical experiment, it was understood to be suppressed even to about the half when the flood plain existed while flow velocity in the narrow section reached 4.5m/s in the current state without the flood plain river channel at the flow rate peak. Moreover, the source location of the maximum flow velocity shifted to the left bank neighborhood though the peak at the flow velocity of the main current part in the flood plain downstream edge was suppressed by about 60% of the current state river channel.

Why it matters

OpenAlex reports 2 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

In the Matsuura river digs the ground in the rice field of Azame down because there were for a long time a lot of floods, makes a flood plain there, and the natural regeneration business that starts restore the marsh is done. In this study, the flow including this Azame was analyzed by the numerical simulation. As a result of the numerical experiment, it was understood to be suppressed even to about the half when the flood plain existed while flow velocity in the narrow section reached 4.5m/s in the current state without the flood plain river channel at the flow rate peak. Moreover, the source location of the maximum flow velocity shifted to the left bank neighborhood though the peak at the flow velocity of the main current part in the flood plain downstream edge was suppressed by about 60% of the current state river channel.

Key concepts: Floodplain, Flood myth, Hydrology (agriculture), Current (fluid), Channel (broadcasting), Flow (mathematics), Geology, 100-year flood

Related papers

Back to paper searchBrowse research topicsOriginal source
EFFECTS OF FLOOD PLAIN ON MAIN CHANNEL WITH FLOOD FLOW OF THE MATSUURA RIVER — Research Paper | ScholarLens