In fluid dynamics, the conjugate depths refer to the depth (y1) upstream and the depth (y2) downstream of the hydraulic jump whose momentum fluxes are equal for a given discharge (volume flux) q. The depth upstream of a hydraulic jump is always supercritical. It is important to note that the conjugate depth is different from the alternate depths for flow which are used in energy conservation calculations.
Mathematical derivation
M–y diagram.
Beginning with an equal momentum flux M and discharge q upstream and downstream of the hydraulic jump:
\( {\displaystyle M={\frac {y_{1}^{2}}{2}}+{\frac {q^{2}}{gy_{1}}}={\frac {y_{2}^{2}}{2}}+{\frac {q^{2}}{gy_{2}}}.} \)
Rearranging terms gives:
\( {\displaystyle {\frac {q^{2}}{g}}\left({\frac {1}{y_{1}}}-{\frac {1}{y_{2}}}\right)={\frac {1}{2}}\left(y_{z}^{2}-y_{1}^{2}\right).} \)
Multiply to get a common denominator on the left-hand side and factor the right-hand side:
\( {\displaystyle {\frac {q^{2}}{g}}\left({\frac {y_{2}-y_{1}}{y_{1}y_{2}}}\right)={\frac {1}{2}}(y_{2}-y_{1})(y_{2}+y_{1}).} \)
The (y2−y1) term cancels out:
\( {\displaystyle {\frac {q^{2}}{g}}\left({\frac {1}{y_{1}y_{2}}}\right)={\frac {1}{2}}(y_{2}+y_{1})\qquad {\text{where }}q_{1}^{2}=y_{1}^{2}v_{1}^{2}=y_{2}^{2}v_{2}^{2}.} \)
Divide by y12
\( {\displaystyle {\frac {v_{1}^{2}}{g}}\left({\frac {1}{y_{1}y_{2}}}\right)={\frac {1}{2y_{1}^{2}}}(y_{2}+y_{1})\qquad {\text{recall }}Fr_{1}^{2}={\frac {v_{1}^{2}}{gy_{1}}}.} \)
Thereafter multiply by y2 and expand the right hand side:
\( {\displaystyle Fr_{2}^{2}={\frac {y_{2}^{2}}{2y_{1}^{2}}}+{\frac {y_{2}}{2y_{1}}}.} \)
Substitute x for the constant y2/y1:
\( {\displaystyle Fr_{1}^{2}={\frac {x^{2}}{2}}+{\frac {x}{2}}\Rightarrow 0={\frac {x^{2}}{2}}+{\frac {x}{2}}-Fr_{1}^{2}.} \)
Solving the quadratic equation and multiplying it by 4 2 {\displaystyle {\tfrac {\sqrt {4}}{2}}} \tfrac{\sqrt{4}}{2} gives:
\( {\displaystyle x={\frac {-{\tfrac {1}{2}}\pm {\sqrt {(1/2)^{2}+4(1/2)(Fr_{1}^{2})}}}{2(1/2)}}.}
Substitute the constant y2/y1 back in for x to get the conjugate depth equation
\( {\displaystyle {\frac {y_{2}}{y_{1}}}={\frac {1}{2}}\left({\sqrt {1+8Fr_{1}^{2}}}-1\right)}
Note that this equation is only applicable to hydraulic jumps over flat beds.
Hellenica World - Scientific Library
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