The depth of flow of water, at a certain section of a rectangular channel of 5 m wide is 0.6 m. The discharge through the channel is 15 m³/s. If a hydraulic jump takes place on the downstream side, find the depth of flow after the jump.

Hydraulic Jump Calculation

Problem Statement

The depth of flow of water, at a certain section of a rectangular channel of 5 m wide is 0.6 m. The discharge through the channel is 15 m³/s. If a hydraulic jump takes place on the downstream side, find the depth of flow after the jump.

Given Data & Constants

  • Width of channel, \(B = 5 \, \text{m}\)
  • Initial depth of flow, \(d_1 = 0.6 \, \text{m}\)
  • Discharge, \(Q = 15 \, \text{m}^3/\text{s}\)
  • Acceleration due to gravity, \(g = 9.81 \, \text{m/s}^2\)

Solution

1. Calculate Initial Velocity and Froude Number

First, we calculate the area of flow and the velocity before the jump.

$$ \text{Area of flow, } A_1 = B \times d_1 = 5 \times 0.6 = 3.0 \, \text{m}^2 $$ $$ \text{Velocity, } V_1 = \frac{Q}{A_1} = \frac{15}{3.0} = 5.0 \, \text{m/s} $$

Next, we calculate the Froude number to confirm the flow is supercritical.

$$ \text{Froude Number, } Fr_1 = \frac{V_1}{\sqrt{g \cdot d_1}} = \frac{5.0}{\sqrt{9.81 \times 0.6}} \approx 2.06 $$

2. Calculate the Depth of Flow After the Jump (\(d_2\))

Since the Froude number is greater than 1, the flow is supercritical and a hydraulic jump can occur. We use the hydraulic jump formula for a rectangular channel.

$$ d_2 = \frac{d_1}{2} \left[ \sqrt{1 + 8 Fr_1^2} - 1 \right] $$ $$ d_2 = \frac{0.6}{2} \left[ \sqrt{1 + 8 \times (2.06)^2} - 1 \right] $$ $$ d_2 = 0.3 \left[ \sqrt{1 + 8 \times 4.2436} - 1 \right] $$ $$ d_2 = 0.3 \left[ \sqrt{1 + 33.949} - 1 \right] = 0.3 [\sqrt{34.949} - 1] $$ $$ d_2 = 0.3 [5.912 - 1] = 0.3 \times 4.912 \approx 1.474 \, \text{m} $$
Final Result:

The depth of flow after the hydraulic jump is approximately 1.47 m.

Explanation of a Hydraulic Jump

A hydraulic jump is a phenomenon that occurs in open channel flow when a high-velocity, shallow stream (supercritical flow) abruptly transitions to a low-velocity, deep stream (subcritical flow). This transition is characterized by a sudden rise in the water surface and significant turbulence and energy dissipation.

  • Supercritical Flow: The initial condition where the flow is fast and shallow. This is indicated by a Froude Number (\(Fr\)) greater than 1.
  • Subcritical Flow: The final condition where the flow is slow and deep, with a Froude Number less than 1.

The formula used is derived from the conservation of momentum principle across the jump. It allows us to directly calculate the resulting "sequent depth" (\(d_2\)) after the jump, based on the initial depth (\(d_1\)) and the initial Froude number.

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