
The velocity of sound is dependent on the medium through which it travels. For example, the speed of sound in air is determined by factors such as temperature, humidity, and pressure, while in solids and liquids, it depends on the rigidity and density of the medium. In gases, the speed of sound is influenced by its compressibility. Various formulas exist to calculate the velocity of sound in different media, such as water and air. The speed of sound is significant in phenomena like earthquakes and echolocation, and it plays a crucial role in room acoustics and medical imaging.
| Characteristics | Values |
|---|---|
| Medium | Gases, Fluids, Solids |
| Factors determining speed of sound in air | Temperature, Humidity, Pressure |
| Formula for speed of sound in water | c = 1404.3 + 4.7 T − 0.04 T^2 |
| Formula for speed of sound in air | v_w = 331 m/s x sqrt(T/273 K) |
| Speed of sound in air | 343 m/s |
| Speed of sound in water | 0-100 C |
| Speed of sound in granite | P-waves: 4-7 km/s, S-waves: 2-5 km/s |
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What You'll Learn

The speed of sound in gases, fluids, and solids
The speed of sound is often thought of as the speed of sound waves in the air. However, the speed varies depending on the substance through which the sound waves are travelling. Typically, sound travels slowest in gases, faster in liquids, and fastest in solids. For example, sound travels at 343 m/s in air, at 1481 m/s in water, and at 5120 m/s in iron. In stiffer materials, such as diamond, sound can travel at 12,000 m/s, which is about the fastest it can travel under normal conditions.
In gases and liquids, sound consists of compression waves. In solids, waves can propagate as two different types: longitudinal waves, which are associated with compression and decompression in the direction of travel, and transverse waves, also called shear waves, which occur only in solids due to their ability to support elastic deformations. These different waves may have different speeds at the same frequency.
The speed of compression waves in solids is determined by the medium's compressibility, shear modulus, and density. The speed of shear waves, on the other hand, is determined only by the solid material's shear modulus and density. In fluid dynamics, the speed of sound in a fluid medium (gas or liquid) is used as a relative measure for the speed of an object moving through the medium. This ratio is known as the object's Mach number.
For monatomic gases, the speed of sound is approximately 75% of the mean speed of the atoms in that gas. In gases, the speed of sound depends on temperature, molecular weight, and heat capacity ratio. In solids and liquids, compression waves depend on both compressibility and density, while in gases, density contributes to compressibility in a way that makes the speed of sound independent of density.
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The effect of temperature and humidity
The velocity of sound is influenced by the properties of the medium through which the sound travels, such as air temperature, pressure, and humidity. An increase in temperature causes the molecules in a gas to move faster, leading to an increase in the speed of sound. This relationship is observed in formulas provided by various researchers, including Wilson (1959), Greenspan and Tschiegg (1959), and Del Grosso and Mader (1972), who derived formulas for sound velocity in water over a temperature range of 0–40°C.
Humidity also affects the velocity of sound. When humidity increases, the amount of water vapor in the air increases, leading to a decrease in air density since water vapor is less dense than nitrogen and oxygen, which predominantly make up dry air. The velocity of sound is inversely proportional to the square root of air density. Therefore, as humidity increases, so does the velocity of sound.
The formula for calculating the velocity of sound in a medium is given by:
V = √(γP/ρ)
Where:
- V is the velocity of sound
- Γ is the adiabatic index (constant for air)
- P is pressure
- Ρ is the density of the air
The speed of sound is not influenced by the distance traveled but rather by the properties of the medium through which it travels. Wind can also impact the measured speed of sound, but its effect is typically minimal.
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The speed of sound in water
The speed of sound in seawater depends on several factors such as pressure (and hence depth), temperature, and salinity. As a general rule, sound travels faster in warmer water. For example, sound travels at 1500.235 m/s in seawater at 1000 kilopascals, 10°C, and 3% salinity. A change in temperature of 1°C results in a change in the speed of sound by about 4 m/s, while a change in salinity of 1‰ results in a change of about 1 m/s.
Empirical equations have been derived to accurately calculate the speed of sound in seawater from variables such as pressure, temperature, and salinity. One such equation is c = 1404.3 + 4.7T − 0.04T^2, where c is the sound velocity in m/s and T is the temperature in °C. This equation is valid for temperatures between 15°C and 35°C and provides true values within 0.20 m/s.
The study of sound in the ocean is known as ocean acoustics. When objects vibrate underwater, they create sound-pressure waves that alternately compress and decompress the surrounding water molecules, causing the sound wave to travel through the water. These sound waves radiate in all directions away from the source and can be detected by structures in our ears or man-made sound receptors such as hydrophones, which are underwater microphones.
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The speed of sound and room acoustics
The speed of sound is 344 m/s or 770 mph when measured in dry air at 20°C. This is a respectable speed within a room, but slow enough over the ground for us to notice the delay between seeing a source of sound and hearing it. For example, we may notice a delay between seeing a distant firework and hearing the explosion. The speed of sound is independent of the rate at which sound vibrations occur, meaning the frequency of a sound does not affect its speed.
The speed of sound is determined by the properties of the medium through which it travels. For example, sound travels faster in helium than in deuterium because helium molecules can store heat energy from compression only in translation, not rotation. Thus, helium molecules travel faster in a sound wave and transmit sound faster. The speed of sound is also dependent on atmospheric pressure and temperature, with temperature being the more significant factor. The velocity at 0°C is 332 metres per second, rising by 0.6 metres per second for each °C increase in temperature.
The speed of sound also varies depending on altitude. Up to 11 km, temperature (and thus the speed of sound) decreases with increasing altitude, creating an acoustic shadow. This is known as a negative sound speed gradient. However, in the stratosphere above 20 km, the speed of sound increases with height due to an increase in temperature from heating within the ozone layer, resulting in a positive sound speed gradient.
Room acoustics are influenced by the interaction of sound waves with the physical dimensions of the room and the materials present. The original sound and the reflected sound can reinforce each other when the wavelength is equal to the distance between two parallel walls. This typically occurs at low frequencies due to their longer wavelengths and the difficulty in absorbing them. Low-frequency sound waves can also bend around obstacles in their path that are smaller than their wavelength, while high-frequency waves cannot. Attenuating low-frequency sound waves with porous absorptive materials can be challenging, as the thickness of the material must be at least 1/4 of the wavelength of the lowest frequency to be absorbed.
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The speed of sound in different media
The speed of sound is not the same in all media. It varies depending on the type of medium, such as solids, liquids, or gases. The speed of sound in a medium like air is determined by the properties of that medium, including its temperature, pressure, and humidity, rather than the distance travelled.
In general, sound waves travel faster in solids than in liquids, and faster in liquids than in gases. This is because the bond strength between particles is strongest in solid materials and weakest in gases. For instance, the speed of sound in solid steel is 5100 metres per second, while in air, it is around 343. Sound travels faster in water than in air, with a speed of 1480 metres per second in distilled water and 1531 metres per second in seawater at temperatures between 20°C and 25°C.
The density of a medium also influences the speed of sound. When the medium is dense, the molecules are closely packed, allowing sound to travel faster. Therefore, sound travels at a slower rate in a less dense object, given that they have similar elastic properties. For example, sound travels about twice as fast in aluminium as in gold due to the difference in their densities.
Additionally, the speed of sound in gases is proportional to the square root of the absolute temperature. In gases, sound travels at about 70% of the mean molecular speed, with higher values in monatomic gases (75%) and lower in diatomic gases (68%).
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Frequently asked questions
The velocity of sound refers to how fast sound energy moves through a given medium.
The speed of sound varies depending on the medium it travels through. For example, the speed of sound in air is relatively low because air is highly compressible. In contrast, liquids and solids are less compressible, resulting in higher sound velocities.
The velocity of sound in the air is influenced by factors such as temperature, humidity, and pressure. Specifically, the speed of sound increases with higher temperatures and lower humidity and pressure levels.
To calculate the velocity of sound in the air, you can use the equation v = 331 m/s * sqrt(T/273 K), where v is the velocity of sound, and T is the temperature in degrees Celsius.
The velocity of sound is independent of the distance traveled. However, when measuring the velocity of sound in a laboratory setting, distance is a necessary factor in the equation: Vs=2.D/ΔT, where V is velocity, D is distance, and ΔT is the time difference.





















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