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Gradually varied flow (G.V.F)
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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.

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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+dhdxv2ghdhdx

=dzdx+dhdx[1v2gh]

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[1v2gh]

ibie=dhdx[1v2gh]

OR dhdx=(ibie)[1v2gh]

dhdx=(ibie)[1(fe)2]

[vgh=fe]

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