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•The spacing between pools and riffles is found to be regular and usually about 5-7 times the width of the channel.

•This regular spacing is said to be as a result of the secondary flow such as helicoidalflow.

•The helicoidal flow moves material from the outer bend and deposits it on the inner bend of the next bend this movement increases the sinuosity of the river, producing a regular meandering channel which is about ten times the bed width.

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