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High-water Level River Discharge Measurement Method in Japan

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Technical Problem of <strong>Measurement</strong> us<strong>in</strong>g<br />

Floats.2(Hypothesis on Disturbed flow <strong>in</strong> the downstream of bridge piers)<br />

Actual discharge value:Q<br />

Q<br />

<br />

<br />

Non-back flow field<br />

Back flow field<br />

<strong>Discharge</strong> observed value based on the current standard Q’<br />

Q 1 =A 1 <br />

Q 2 =A 2 V 2<br />

Non-back flow field<br />

Q 1 <strong>Discharge</strong> of non-back flow field ,A 1 river area of non-back flow field,<br />

V 1 average velocity of non-back flow field,<br />

Q 2 <strong>Discharge</strong> of back flow field,A 2 river area of back flow field,<br />

V 2 average velocity of back flow field<br />

V 1<br />

Q=Q 1 +Q 2<br />

=A 1 V 1 +A 2 V 2<br />

Q 1 =A 1 V 1<br />

Q<br />

<br />

<br />

Non-back flow field<br />

Q 1<br />

=A 1<br />

(V 1<br />

+V <br />

)<br />

Back flow field Q 2<br />

=A 2<br />

(V 1<br />

+V <br />

)<br />

Q’= Q 1<br />

+Q 2<br />

=(V 1<br />

+V <br />

)(A 1<br />

+A 2<br />

)<br />

Non-back flow field Q 1<br />

=A 1<br />

(V 1<br />

+V <br />

)<br />

Q 1 <strong>Discharge</strong> of non-back flow field,A 1 river area of non-back flow field,V 1 average velocity of non-back flow field,<br />

V acceleration by aboideau ris<strong>in</strong>g effect,Q 2 <strong>Discharge</strong> of back flow field,A 2 river area of back flow field<br />

comparison of <strong>Discharge</strong> observed value of current standard and Actual discharge observed value<br />

Q’=Q+(V 1 -V )A 2 +V (A 1 +A 2 )<br />

<strong>Discharge</strong> observed value based on the current<br />

standard has overestimates the river discharge<br />

The part become exorbitance<br />

caused bythe underl<strong>in</strong>e part<br />

Tone <strong>River</strong> downstream construction office<br />

Tone <strong>River</strong> downstream part river bed and discharge observation research report <strong>in</strong> 1999

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