Velocity Of Sound In Different Media

Velocity Of Sound In Different Media

Vishal kumarUpdated on 02 Jul 2025, 08:04 PM IST

Introduction

Sound is a mechanical wave that requires a medium (like air, water, or solid materials) to propagate. The speed of sound depends on the properties of the medium through which it travels, such as density and elasticity. In gases, sound travels more slowly due to the larger distance between particles, while in liquids and solids, it moves faster because particles are closer together, allowing quicker transfer of energy. Temperature also plays a significant role in sound speed, especially in gases, where an increase in temperature causes faster molecular motion and, hence, a faster sound speed. The nature of the medium—whether it's a solid, liquid, or gas—affects how efficiently sound waves can propagate.

Speed of sound wave in a material medium -

For deriving the equation of speed let us consider a section AB of medium as shown in figure of cross-sectional area S. Let A and B be two cross-sections as shown. Let in this medium sound wave propagation be from left to right. If wave source is located at origin O and when it oscillates, the oscillations at that point propagate along the rod.

The stress at any cross section can be written as -
$
\delta_t=\frac{F}{S}
$
. . . . .. . . . (i)

Let us consider a section AB of the material as shown in the figure, of medium at a general instant of time t . The end A is at a distance 'x' from O and point B is at a distance 'x+d x' from O. Let in time duration 'dt' due to oscillations, medium particles at A be displaced along the length of medium by 'y' and those at B by 'y+d y' . The resulting positions of section are A' and B' as shown in figure. By this we can say that the section AB is elongated by a length 'dy' . Thus strain produced in it is -
$
E=\frac{d y}{d x} \ldots \ldots . .(i i)
$
If Young's modulus of the material of medium is $Y$, we have

$
Y=\frac{\text { Stress }}{\text { Strain }}=\frac{\delta_1}{E}
$

By using Hooke's law -

From Eqs. (i) and (ii), we have

$
\begin{aligned}
& Y=\frac{F / S}{d y / d x} \\
& F=Y S \frac{d y}{d x} \ldots . .(i i i)
\end{aligned}
$
Here, $F=$ Force
if $d m$ is the mass of section $A B$ and $a$ is its acceleration, which can be given as for a medium of density $\rho$ as

$
\begin{gathered}
d m=\rho S d x \\
a=\frac{d^2 y}{d t^2}
\end{gathered}
$
From Eq. (iv), we have

$
\begin{aligned}
& d F=(\rho S d x) \frac{d^2 y}{d t^2} \\
& \frac{d F}{d x}=\rho S \frac{d^2 y}{d t^2}
\end{aligned}
$
From Eq. (iii) on differentiating w.r.t. to $x$, we can write

$
\frac{d F}{d x}=Y S \frac{d^2 y}{d x^2}
$
From Eqs. (iv) and (v), we get

The above equation shows wave velocity

In the case of gas or liquid, which shows only volume elasticity, E = B, where B = Bulk modulus of elasticity.

For longitudinal wave for liquid or gas -
$
v=\sqrt{\frac{B}{\rho}}
$

where $\rho=$ Density of the medium

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Some Solved Examples

Example 1: The maximum pressure variation that the human ear can tolerate is $30 \mathrm{~N} / \mathrm{m}^2$. The maximum displacement for a sound wave in the air having a frequency of $10^3 \mathrm{kHz}$ is? (Use density of air $=\rho=1.2 \frac{\mathrm{kg}}{\mathrm{m}^3}$ and speed of sound in air $=$ $v=343 \mathrm{~m} / \mathrm{s}$ )
1) $\frac{2 \pi}{3} \times 10^{-2} \mathrm{~km}$
2) $\frac{2 \times 10^{-4}}{\pi} \mathrm{km}$
3) $\frac{\pi}{3} \times 10^{-2} \mathrm{~km}$
4) $\frac{10^{-4}}{3 \pi} \mathrm{km}$

Solution:
Equation of sound wave -

$
\Delta P=\Delta P_{\max } \cdot \sin \left[\omega\left(t-\frac{x}{v}\right)\right]
$

- wherein
$\Delta P=$ variation in pressure at a point
$\Delta P_{\text {max }}=$ maximum variation in pressure

$
\begin{aligned}
& \left(\Delta P_{\max }\right)=B A K \Rightarrow A=\frac{\Delta P}{B k} \\
& v=\frac{\omega}{k} \\
& B=\rho \times v^2 \\
& k=\omega \sqrt{\frac{\rho}{B}} \Rightarrow A=\frac{\Delta P_{\max }}{2 \pi f \rho v}=\frac{10^{-4}}{3 \pi} \mathrm{Km} \\
& \left(\text { Use } \rho=1.2 \frac{\mathrm{kg}}{\mathrm{m}^3} \text { and } v=343 \mathrm{~m} / \mathrm{s}\right)
\end{aligned}
$

Hence, the answer is the option 4.

Example 2: The pressure wave, $P=0.01 \sin [1000 t-3 x] \mathrm{Nm}^{-2}$, corresponds to the sound produced by a vibrating blade on a day when atmospheric temperature is $0^{\circ} \mathrm{C}$. On some other day when the temperature is T . the speed of sound produced by the same blade and at the same frequency is found to be $336 \mathrm{~ms}^{-1}$. Approximate value of $T$ (in ${ }^{\circ} \mathrm{C}$ ) is:
1) 4
2)11
3) 12
4)15

Solution
Equation of sound wave -

$
\Delta P=\Delta P_{\max } \cdot \sin \left[\omega\left(t-\frac{x}{V}\right)\right]
$

wherein
$\Delta P=$ variation in pressure at a point
$\Delta P_{\max }=$ maximum variation in pressure at $0^{\circ} \mathrm{C}$

$
\begin{aligned}
& P=0.01 \sin (1000 t-3 x) \mathrm{Nm}^{-2} \\
& V_1=\frac{\omega}{k}
\end{aligned}
$
$
\begin{aligned}
& V_1=\frac{1000}{3} \\
& \text { at temp } T \\
& V_2=336 \mathrm{~ms}^{-1} \\
& \frac{V_1}{V_2}=\sqrt{\frac{T_1}{T_2}} \quad \text { (Where T is in Kelvin) } \\
& \frac{\frac{1000}{3}}{336}=\sqrt{\frac{273}{T}} \\
& \Rightarrow T=277.41 \mathrm{k} \\
& =T=4.4^{\circ} \mathrm{C}
\end{aligned}
$
Hence, the answer is (4).

Example 3: Calculate the speed (in $\mathrm{m} / \mathrm{s}$ ) of the longitudinal wave in the helium gas of bulk modulus $1.7 \times 10^5 \mathrm{~Pa}$ and density is $0.18 \mathrm{~kg} / \mathrm{m}^3$ at $0^{\circ} \mathrm{C}$ and 1 atm pressure.
1) 972
2) 413
3) 314
4) 600

Solution
As we learnt in
Speed of sound wave -

$
v=\sqrt{\frac{B}{\rho}}
$

- wherein
$B$ is bulk modulus that represents the elastic property of the medium
$\rho=$ the density of the medium that represents the inertial property of the medium.


$V_{o_{2}} = \sqrt{\frac{B}{\rho}} = \sqrt{\frac{1.41 \times 10^{5}}{1.43}} = 314 m/s$

Hence, the answer is 314.

Example 4: A granite rod of 60 cm length is clamped at its middle point and is set into longitudinal vibrations. The density of granite is 2.7×103 kg/m3 and its Young’s modulus is 9.27×1010 Pa. What will be the fundamental frequency (in Hz) of the longitudinal vibrations ?

1) 5

2)7.5

3)2.5
4)10

Solution


$\begin{aligned} \nu_o & =\frac{v}{2 l}=\frac{1}{2 l} \cdot \sqrt{\frac{\gamma}{\rho}}=\frac{1}{2 * 0.6} \sqrt{\frac{9.27 * 10^{10}}{2.7 * 10^3}} \\ & =4.9 * 10^3 \mathrm{HZ} \simeq 5 \mathrm{kHZ}\end{aligned}$

Summary

The speed of sound is influenced by the medium's density and elasticity. In solids, sound waves travel faster than in liquids and gases because the particles are more tightly packed. Factors like temperature and pressure can also affect sound speed, particularly in gases, where warmer conditions generally mean faster sound propagation. For example, the speed of sound in air at 20°C is about 343 m/s, but it increases with rising temperatures. The mathematical formula for sound speed involves the medium's bulk modulus and density, but conceptually, it reflects how fast energy can transfer between particles. Understanding sound speed is crucial in fields like acoustics, engineering, and meteorology.

Frequently Asked Questions (FAQs)

Q: Why does the speed of sound in most liquids increase with pressure, unlike in ideal gases?
A:
In most liquids, the speed of soun
Q: How does the speed of sound in a gas mixture compare to the speeds in its component gases?
A:
The speed of sound in a gas mixture is not a simple average of the speeds in its component gases. Instead, it depends on the average molecular mass and the ratio of specific heats of the mixture. Generally, the speed in the mixture will be between the speeds of the individual components, but weighted towards the speed in the more abundant gas. The exact speed can be calculated using the mixture's effective gas constant and ratio of specific heats.
Q: What is the relationship between the speed of sound and the propagation of earthquakes?
A:
Earthquakes propagate through the Earth as seismic waves, which are similar in nature to sound waves but travel much faster due to the higher rigidity of rock compared to air. P-waves (primary waves) are compressional waves analogous to sound waves and travel at speeds of about 5-8 km/s in the Earth's crust, much faster than the speed of sound in air (0.343 km/s). The speed of seismic waves is crucial in determining the arrival times of earthquake signals at different locations.
Q: How does the speed of sound relate to the compressibility of a medium?
A:
The speed of sound in a medium is inversely proportional to the square root of its compressibility. Less compressible (more rigid) materials generally have a higher speed of sound. This is why sound typically travels faster in solids than in liquids, and faster in liquids than in gases. The relationship is described by the equation: v = √(1/ρκ), where v is the speed of sound, ρ is the density, and κ is the compressibility of the medium.
Q: Why does the speed of sound in air not depend significantly on frequency, while the speed of light in a medium often does?
A:
The speed of sound in air is largely independent of frequency because air acts as a non-dispersive medium for audible sound waves. The wavelengths of sound are much larger than the size of air molecules, so all frequencies interact with the medium similarly. In contrast, the speed of light in a medium can depend on frequency (a phenomenon called dispersion) because light wavelengths are often comparable to the size of atoms or molecules, leading to frequency-dependent interactions.
Q: How does the speed of sound in a plasma compare to that in a neutral gas?
A:
The speed of sound in a plasma is generally higher than in a neutral gas under similar conditions. This is because plasmas can support additional types of waves, including electromagnetic plasma waves, which can propagate much faster than ordinary sound waves. The exact speed depends on factors such as the plasma temperature, density, and the strength of any magnetic fields present.
Q: What is the significance of Mach number in relation to the speed of sound?
A:
The Mach number is the ratio of an object's speed to the speed of sound in the surrounding medium. It's a crucial parameter in aerodynamics and acoustics. When an object moves at Mach 1 (the speed of sound), it creates a shock wave. At speeds above Mach 1 (supersonic), the object moves faster than the pressure waves it creates, leading to complex shock wave patterns and significant changes in aerodynamic properties.
Q: How does the concept of acoustic metamaterials relate to manipulating the speed of sound?
A:
Acoustic metamaterials are artificially structured materials designed to control and manipulate sound waves in ways not possible with conventional materials. By carefully engineering the structure and properties of these materials, it's possible to create environments where the effective speed of sound is dramatically altered, or even made negative. This can lead to applications such as super-resolution acoustic imaging and sound cloaking.
Q: How does the speed of sound change in the ocean at different depths?
A:
The speed of sound in the ocean varies with depth due to changes in temperature, pressure, and salinity. Near the surface, it decreases with depth as temperature drops. At greater depths, it starts to increase again as the effect of increasing pressure becomes dominant. This creates a region of minimum sound speed called the SOFAR channel, where sound can travel long distances with little attenuation.
Q: What is the relationship between the speed of sound and the speed of seismic waves in the Earth?
A:
Seismic waves, like sound waves, are mechanical waves that propagate through a medium. However, seismic waves can travel much faster than sound waves in air because they travel through solid rock, which has higher elasticity and density than air. P-waves (primary waves) are compressional waves similar to sound waves and can travel at speeds of 5-8 km/s in the Earth's crust, much faster than the speed of sound in air (0.343 km/s).