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If the depth of flow in a channel changes gradually over a long length of the channel the flow is said to be gradually, varied flow and is denoted by G.V.F.
Equation for Gradually varied flow:
Before deriving an equation, following assumptions are made:
1] Bed slope of the channel is small.
2] Flow is steady and hence Q is constant
3] Accelerative effect is negligible.
4] Energy correction factor 'a' is unity
5] Roughness co-efficient is constant for the length of the channel.
6] Chezy's formula, manning formula are applicable to G.V.F to find slope.
7] Channel is prismatic.
Consider a rectangular channel having gradually varied flow,
Let, Z = height of bottom of channel
h = depth of flow
v = mean velocity of flow
ib = slope of the channel bed
ie = slope of energy line
b = width of channel
Q = discharge through channel
Energy equation at any section is given by Bernoulli's equation,
E=z+h+v22g - - - - (1)
Differentiating w.r. to 'x' where 'x' is measured along the bottom of the channel in direction of flow,
dEdx=d2dx+dhdx+ddx(v22g) - - - - (2)
Now, ddx(v22g)=ddx(q2A×2g)
v=QA
=ddx(Q2b2h2×2g)
=Q2b2×2gddx(1h2)
(∵ Q , b, g are) constant
=Q2b2×2gddh[1h2)dhdx
=Q2b2×2g[−2h3]dhdx
=−2q2b2×2gh3dhdx
=Q2b2h2×ghdhdx
=−v2gh
[∵Qbh=v]
Substituting the value of ddx(v22g)
in equation (2), we get,
dEdx=dzdx+dhdx−v2ghdhdx
=dzdx+dhdx[1−v2gh]
Now, dEdx = slope of energy line = - ie.
dzdx = slope of the bed of the channel = - ib
negative sign because as with the increase of x, the value of E and z decreases.
substituting the value of dEdx and dzdx
in equation (3), we get,
−i_e=−i_b+dhdx[1−v2gh]
ib−ie=dhdx[1−v2gh]
OR dhdx=(ib−ie)[1−v2gh]
dhdx=(ib−ie)[1−(fe)2]
[∴v√gh=fe]