Sound Attenuation Formula:
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Sound attenuation over distance refers to the decrease in sound pressure level as sound waves propagate through a medium. This natural phenomenon occurs due to spherical spreading of sound energy and is described by the inverse square law in free field conditions.
The calculator uses the sound attenuation formula:
Where:
Explanation: The formula calculates the sound pressure level drop in decibels when comparing the sound level at distance d to the sound level at reference distance d₀.
Details: Understanding sound attenuation is crucial for noise control engineering, acoustic design, environmental noise assessment, and predicting how sound levels decrease with distance from sources like industrial equipment, transportation, or entertainment venues.
Tips: Enter both distance values in meters. The reference distance is typically the measurement point where the original sound level is known. Both values must be positive numbers greater than zero.
Q1: What is the reference distance (d₀)?
A: The reference distance is the point where the original sound pressure level is measured or known, serving as the baseline for calculating attenuation at other distances.
Q2: Does this formula account for atmospheric absorption?
A: No, this formula only accounts for geometric spreading. Atmospheric absorption, which depends on humidity, temperature, and frequency, requires additional calculations.
Q3: What is the 6 dB rule?
A: For every doubling of distance from a point source in free field conditions, sound pressure level decreases by approximately 6 dB according to the inverse square law.
Q4: How does terrain affect sound attenuation?
A: Terrain features like hills, buildings, and vegetation can significantly alter sound propagation, causing deviations from the theoretical attenuation calculated by this formula.
Q5: Is this applicable to all sound frequencies?
A: While the basic distance attenuation applies to all frequencies, higher frequencies typically experience additional attenuation due to atmospheric absorption and scattering.