Animated Solution for Physics - Waves: A 3.6 m long pipe resonates with a source of frequency 212.5 Hz when water level is at certain heights in the pipe. Find the heights of water level (from the bottom of the pipe) at which resonances occur. Neglect end correction. Now the pipe is filled to a height H(≈3.6 m). A small hole is drilled very close to its bottom and water is allowed to leak. Obtain an expression for the rate of fall of water level in the pipe as a function of H. If the radii of the pipe and the hole are 2×10−2 m and 1×10−3 m respectively. Calculate the time interval between the occurrence of first two resonances. Speed of sound in air is 340 m/s and g=10 m/s2.
Visualized Solution
Visualizing the Resonance Column
We have a vertical pipe of length L=3.6 m open at the top and closed at the bottom by the water surface.
The air column above the water acts as a closed organ pipe of length l=L−H, where H is the height of the water level.
Resonance Condition for Closed Pipe
For a closed organ pipe, resonance occurs when the length of the air column l satisfies:
l=(2n−1)4λ=(2n−1)4fv
where n=1,2,3,… represents the harmonic mode, v is the speed of sound, and f is the frequency of the source.
Calculating the Fundamental Length l0
Let us calculate the fundamental air column length l0 (for n=1):
l0=4fv
Substituting v=340 m/s and f=212.5 Hz:
l0=4×212.5340=0.4 m
Determining Resonant Air Column Lengths
The possible resonant air column lengths are odd multiples of l0:
ln=(2n−1)l0=(2n−1)×0.4 m
Since the total length of the pipe is 3.6 m, ln must be less than or equal to 3.6 m:
ln∈{0.4 m,1.2 m,2.0 m,2.8 m,3.6 m}
Calculating Water Levels
The height of the water level from the bottom of the pipe is Hn=L−ln:
Hn=3.6−ln
Substituting the possible values of ln:
H1=3.6−0.4=3.2 m
H2=3.6−1.2=2.4 m
H3=3.6−2.0=1.6 m
H4=3.6−2.8=0.8 m
H5=3.6−3.6=0 m
Torricelli's Law & Continuity
By Torricelli's Law, the velocity of efflux of water from the small hole at the bottom is:
vefflux=2gH
By the Equation of Continuity, the rate of flow is:
A(−dtdH)=avefflux
where A=πR2 is the cross-sectional area of the pipe and a=πr2 is the area of the hole.
Deriving the Rate of Fall −dtdH
Rearranging the continuity equation:
−dtdH=Aa2gH=(Rr)22gH
Substituting the given values:
r=1×10−3 m, R=2×10−2 m, g=10 m/s2
−dtdH=(2×10−210−3)22×10×H
Simplifying the Rate of Fall
Calculate the constant term:
(Rr)2=(201)2=4001
2g=20≈4.472 m1/2s−1
−dtdH=40020H≈1.118×10−2H≈1.11×10−2H
Setting up Integration for Time Interval
The first resonance occurs at H1=3.2 m and the second at H2=2.4 m.
Separating variables:
H−1/2dH=−1.118×10−2dt
Integrating from H=3.2 m to H=2.4 m:
∫3.22.4H−1/2dH=−1.118×10−2∫0tdt
Solving the Definite Integral
Integrating both sides:
[2H]3.22.4=−1.118×10−2t
2(2.4−3.2)=−1.118×10−2t
2(3.2−2.4)=1.118×10−2t
Numerical Calculation
Calculate the square roots:
3.2≈1.789 m1/2
2.4≈1.549 m1/2
2(1.789−1.549)=1.118×10−2t
2(0.240)=1.118×10−2t
0.480=1.118×10−2t
Final Value of Time Interval
Solve for t:
t=1.118×10−20.480≈42.93 s≈43 s
Summary of Final Answers
1. Resonant water heights: 3.2 m,2.4 m,1.6 m,0.8 m
2. Rate of fall: −dtdH=(1.11×10−2)H
3. Time interval: 43 s
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The Sigma Insight: Standing Waves in Strings and Organ Pipes
Solution Diagram
Analyzing the Setup
Imagine standing next to a tall, vertical cylindrical tube filled with water.
At the top, the tube is open to the air, while the bottom is sealed by the water surface.
This system forms a classic closed organ pipe of variable length.
The length of the air column, which we will denote as l, is determined by the total length of the pipe L=3.6 m and the height of the water level H:
l=L−H=3.6−H
When a tuning fork of frequency f=212.5 Hz is held over the open end, it sends sound waves down the tube.
These waves reflect off the water surface, creating a standing wave pattern.
Resonance occurs when the length of the air column matches one of the natural modes of vibration of the closed pipe.
The Resonance Condition
For a pipe closed at one end, the boundary conditions require a displacement node at the water surface (where air molecules cannot move) and a displacement antinode at the open end (where air molecules vibrate with maximum amplitude).
This constraint means that the length of the air column must be an odd multiple of a quarter-wavelength:
ln=(2n−1)4λ=(2n−1)4fv
where n=1,2,3,… represents the harmonic mode, and v=340 m/s is the speed of sound in air.
Let us first find the fundamental resonant length l0 (for n=1):
l0=4fv=4×212.5340=0.4 m
Using this fundamental length, the possible resonant air column lengths are:
ln=(2n−1)×0.4 m
Since the physical length of the pipe is 3.6 m, the air column length ln cannot exceed 3.6 m.
This gives us the following possible resonant air column lengths:
ln∈{0.4 m,1.2 m,2.0 m,2.8 m,3.6 m}
To find the corresponding water heights Hn from the bottom of the pipe, we subtract each ln from the total length L=3.6 m:
Hn=3.6−ln
This yields the water heights at which resonance occurs:
H∈{3.2 m,2.4 m,1.6 m,0.8 m,0 m}
Fluid Dynamics of the Leaking Pipe
Now, let us introduce a dynamic twist to the problem.
The pipe is filled to the top (H≈3.6 m), and a small hole is drilled at the very bottom.
Water begins to leak out, causing the water level to fall.
To describe how fast the water level drops, we must combine two fundamental principles of fluid mechanics: Torricelli's Law and the Equation of Continuity.
According to Torricelli's Law, the velocity of efflux vefflux of water leaving a hole under a head of height H is:
vefflux=2gH
By the Equation of Continuity, the volume flow rate of water leaving the top of the pipe must equal the volume flow rate leaving the hole at the bottom:
A(−dtdH)=avefflux
where A=πR2 is the cross-sectional area of the pipe, and a=πr2 is the cross-sectional area of the hole.
Rearranging this equation gives the rate of fall of the water level:
−dtdH=Aa2gH=(Rr)22gH
Substituting the given values (r=1×10−3 m, R=2×10−2 m, and g=10 m/s2):
(Rr)2=(2×10−210−3)2=(201)2=4001
−dtdH=40012×10×H=40020H
Since 20≈4.472:
−dtdH≈(1.11×10−2)H
This elegant differential equation describes the rate of fall of the water level as a function of its instantaneous height H.
Calculating the Time Interval
As the water level falls from 3.6 m, the first resonance is heard when the water level reaches H1=3.2 m.
The second resonance is heard when the water level falls further to H2=2.4 m.
To find the time interval Δt between these two events, we must integrate our differential equation between these limits:
H−1/2dH=−1.118×10−2dt
Integrating both sides:
∫3.22.4H−1/2dH=−1.118×10−2∫0tdt
[2H]3.22.4=−1.118×10−2t
2(3.2−2.4)=1.118×10−2t
Let us calculate the numerical values of the square roots:
3.2≈1.789 m1/2
2.4≈1.549 m1/2
Substituting these back into the equation:
2(1.789−1.549)=1.118×10−2t
2(0.240)=1.118×10−2t
0.480=1.118×10−2t
Solving for t:
t=1.118×10−20.480≈42.93 s
Rounding to the nearest integer, we find that the time interval between the first two resonances is 43 s.