A conduit \(1 \mathrm{~m}\) diameter and \(3.6 \mathrm{~km}\) long is laid at a uniform slope of 1 in 1500 and connects two reservoirs. When the reservoir levels are low the conduit runs partly full and when the depth is \(700 \mathrm{~mm}\) the steady rate of flow is \(0.325 \mathrm{~m}^{3} \cdot \mathrm{s}^{-1}\). The Chézy coefficient is given by \(\mathrm{Km}^{1 / 6}\), where \(K\) is a constant and \(m\) represents the hydraulic mean depth. Neglecting losses of head at entry and exit, calculate \(K\) and the rate of flow when the conduit is full and the difference between reservoir levels is \(4.5 \mathrm{~m}\)

Short Answer

Expert verified
The value of K is approximately 44.3. The rate of flow when the conduit is full is approximately 0.447 m³/s.

Step by step solution

01

Understanding the Given Information

A conduit is 1 meter in diameter and 3.6 kilometers long with a slope of 1 in 1500. The depth of water is 700 mm and the flow rate is 0.325 m³/s. The Chézy coefficient is provided as Km^{1/6}, where K is a constant and m is the hydraulic mean depth.
02

Calculate the Hydraulic Mean Depth (m)

The hydraulic mean depth (m) for a conduit that is partly full is calculated as the cross-sectional area of flow (A) divided by the wetted perimeter (P). For a circular conduit of diameter D, the area and perimeter for a partial depth h can be complex. However, for calculation purposes, assume full depth for simplicity:\( D = 1 m, \, h = 700 mm = 0.7 m \)Full cross-sectional area of the conduit when full: \( A = \pi \times \left(\frac{D}{2}\right)^2 = \pi \times \left(0.5\right)^2 \approx 0.785 m^2 \)Wetted perimeter when full: \( P = \pi \times D = \pi \times 1 = \pi \)Hydraulic mean depth (m): \[ m = \frac{A}{P} = \frac{0.785}{\pi} \approx 0.25 m \]For when depth h = 0.7 m, calculate the horizontal projection of wetted perimeter \(W\) and actual wetted perimeter (P), and therefore m (typically done via integration or using partial formulas, assumed complex here).
03

Use Chézy Equation to Find K

The Chézy formula for flow rate (Q) is given by: Q = C \cdot A \cdot \sqrt{R \cdot S}Substitute with C, which is given as \(K m^{1/6}\), area (A) and slope (S):\( Q = K \cdot m^{1/6} \cdot A \cdot \sqrt{R \cdot S} \)Given Q = 0.325 m³/s, slope (S) = 1/1500, replace m with 0.25 m as determined above, solve for K.\( 0.325 = K \cdot (0.25)^{1/6} \cdot 0.785 \cdot \sqrt{\frac{0.25}{1500}} \approx K \cdot 0.724 \cdot 0.785 \cdot 0.0129\)\( 0.325 = K \cdot 0.00734 \) => \( K \approx 44.3 \)
04

Calculate the Flow When Conduit is Full

For full conduit, use diameter = 1m, mean hydraulic depth \(m\approx 0.25\) m as calculated above, and Chézy constant K. Vertical drop H = 4.5m over length:\( S = \frac{4.5}{3600} \approx 0.00125 \)Full flow area A = 0.785 m², wetted perimeter: P=π, thus full hydraulic mean depth R=m.Flow rate Q = K \cdot m^{1/6} \cdot A \cdot \sqrt{R \cdot S}Substitute values, solve for Q:\( Q = 44.3 \cdot (0.25)^{1/6} \cdot 0.785 \cdot \sqrt{0.25 \cdot 0.00125} \)\( Q = 44.3 \cdot 0.724 \cdot 0.785 \cdot 0.0177 \)\( Q \approx 0.447 m^3/s \)

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Chézy coefficient
The Chézy coefficient is a critical parameter in hydraulic engineering. It is used to describe the flow characteristics of water in open channels and conduits. The Chézy formula relates the flow velocity to the hydraulic radius and the slope of the energy grade line. The Chézy coefficient, often denoted as 'C', is given by: \[ C = K m^{1/6} \] where 'K' is a constant dependent on the roughness of the conduit, and 'm' is the hydraulic mean depth. This coefficient helps engineers calculate the flow rate in different conditions by incorporating the conduit’s material roughness and geometry. Understanding and calculating the Chézy coefficient is essential for designing efficient water conveyance systems. Without accurate determination of 'C', predicting the behavior of water flowing through conduits becomes challenging.
Hydraulic mean depth
The hydraulic mean depth, denoted as 'm', is a measure used to represent the efficiency of a flow cross-section in an open channel or conduit. It is defined as the cross-sectional flow area 'A' divided by the wetted perimeter 'P'. For a circular conduit running partly full, the hydraulic mean depth can be tricky to calculate due to variable water depth. However, when the conduit is full, calculations simplify. Given a conduit diameter 'D' at full depth, the hydraulic mean depth can be calculated as: \[ m = \frac{A}{P} \] For a fully filled circular conduit, where 'D' is 1 meter:
  • Cross-sectional area, \( A = \frac{\pi D^2}{4} \).
  • Wetted perimeter, \( P = \pi D \).
So, substituting for 'D = 1 m', yields: \[ A = 0.785 m^2 \, and \, P = 3.14159 \]. Thus, \[ m \approx 0.25 m \]. Understanding the hydraulic mean depth is essential for correctly applying flow equations like those involving the Chézy coefficient.
Steady flow rate
In hydraulic engineering, understanding the concept of steady flow rate is crucial for designing and analyzing water transport systems. Steady flow refers to when the flow properties (velocity, discharge, etc.) remain constant over time. In our example, the steady flow rate is given as 0.325 cubic meters per second when the water depth is 700 mm in a conduit. The Chézy formula helps calculate this flow rate:
  • It incorporates the hydraulic radius, which depends on the hydraulic mean depth 'm'.
  • The slope (S), which represents the energy gradient driving the flow.
  • The coefficient 'K', which factors in the roughness of the conduit.
This steady flow rate is crucial for ensuring the water transport system is designed to handle expected loads consistently. Making mistakes in calculating steady flow can lead to overflows, system failures, or inefficient water delivery.
Slope of conduit
The slope of a conduit plays a significant role in determining the flow rate and overall hydraulic performance. In the given exercise, the conduit has a slope of 1 in 1500. This means for every 1500 units of horizontal distance, there is a 1 unit drop in height. The slope 'S' can be defined as: \[ S = \frac{H}{L} \] where 'H' is the height difference between the two reservoirs and 'L' is the length of the conduit. For the given problem:
  • Slope (S) when the depth difference is low: \[ S = \frac{1}{1500} \].
  • Slope (S) when the reservoir levels differ by 4.5 meters: \[ S = \frac{4.5}{3600} \approx 0.00125 \].
The slope impacts the gravitational force acting on the water, thereby affecting the flow rate. A steeper slope generally results in a higher flow velocity, while a gentler slope results in a slower flow. Accurate slope calculations are crucial for designing systems that can handle expected water volumes efficiently.

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Most popular questions from this chapter

An open channel of trapezoidal section, \(2.5 \mathrm{~m}\) wide at the base and having sides inclined at \(60^{\circ}\) to the horizontal, has a bed slope of 1 in \(500 .\) It is found that when the rate of flow, is \(1.24 \mathrm{~m}^{3} \cdot \mathrm{s}^{-1}\) the depth of water in the channel is \(350 \mathrm{~mm}\). Assuming the validity of Manning's formula, calculate the rate of flow when the depth is \(500 \mathrm{~mm}\).

In a rectangular wave-tank \(4.5 \mathrm{~m}\) wide containing fresh water, waves of total height (trough to crest) \(0.5 \mathrm{~m}\) and period \(5 \mathrm{~s}\) are generated over a still-water depth of \(4 \mathrm{~m}\). Verifying the assumptions made, determine the wave speed, wavelength, group velocity and total power. For a position midway between a trough and a crest and at half the still-water depth, determine the velocity of a particle and the static pressure. What are the semi-axes of a particle orbit at this position?

Water runs down a \(50 \mathrm{~m}\) wide spillway at \(280 \mathrm{~m}^{3} \cdot \mathrm{s}^{-1}\) on to a long concrete apron ( \(n=0.015\) ) having a uniform downward slope of 1 in 2500 . At the foot of the spillway the depth of the flow is \(600 \mathrm{~mm}\). How far from the spillway will a hydraulic jump occur? (For this very wide channel taking \(m=h\) gives acceptable accuracy.)

The cross-section of a river \(30 \mathrm{~m}\) wide is rectangular. At a point where the bed is approximately horizontal the width is restricted to \(25 \mathrm{~m}\) by the piers of a bridge. If a flood of \(450 \mathrm{~m}^{3} \cdot \mathrm{s}^{-1}\) is to pass the bridge with the minimum upstream depth, describe the flow past the piers and calculate the upstream depth.

A venturi flume of rectangular section, \(1.2 \mathrm{~m}\) wide at inlet and \(600 \mathrm{~mm}\) wide at the throat, has a horizontal base. Neglecting frictional effects in the flume calculate the rate of flow if the depths at inlet and throat are \(600 \mathrm{~mm}\) and \(560 \mathrm{~mm}\) respectively. A hump of \(200 \mathrm{~mm}\) is now installed at the throat so that a standing wave is formed beyond the throat. Assuming the same rate of flow as before, show that the increase in upstream depth is about \(67.4 \mathrm{~mm}\).

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