The natural frequency, or fundamental frequency, often referred to simply as the fundamental, is defined as the lowest frequency of a periodic waveform. In music, the fundamental is the musical pitch of a note that is perceived as the lowest partial present. In terms of a superposition of sinusoids, the fundamental frequency is the lowest frequency sinusoidal in the sum. In some contexts, the fundamental is usually abbreviated as f0 (or FF), indicating the lowest frequency counting from zero. In other contexts, it is more common to abbreviate it as f1, the first harmonic. (The second harmonic is then f2 = 2⋅f1, etc. In this context, the zeroth harmonic would be 0 Hz.)
Since the fundamental is the lowest frequency and is also perceived as the loudest, the ear identifies it as the specific pitch of the musical tone [harmonic spectrum]....The individual partials are not heard separately but are blended together by the ear into a single tone.
All sinusoidal and many non-sinusoidal waveforms repeat exactly over time – they are periodic. The period of a waveform is the smallest value of for which the following equation is true:
Where is the value of the waveform at . This means that this equation and a definition of the waveform’s values over any interval of length is all that is required to describe the waveform completely. Waveforms can be represented by Fourier series.
Every waveform may be described using any multiple of this period. There exists a smallest period over which the function may be described completely and this period is the fundamental period. The fundamental frequency is defined as its reciprocal:
Since the period is measured in units of time, then the units for frequency are 1/time. When the time units are seconds, the frequency is in , also known as Hertz.
For a tube of length with one end closed and the other end open the wavelength of the fundamental harmonic is , as indicated by the first two animations. Hence,
Therefore, using the relation
where is the speed of the wave, we can find the fundamental frequency in terms of the speed of the wave and the length of the tube:
If the ends of the same tube are now both closed or both opened as in the last two animations, the wavelength of the fundamental harmonic becomes . By the same method as above, the fundamental frequency is found to be
At 20 °C (68 °F) the speed of sound in air is 343 m/s (1129 ft/s). This speed is temperature dependent and increases at a rate of 0.6 m/s for each degree Celsius increase in temperature (1.1 ft/s for every increase of 1 °F).
The velocity of a sound wave at different temperatures:-
- v = 343.2 m/s at 20 °C
- v = 331.3 m/s at 0 °C
In music, the fundamental is the musical pitch of a note that is perceived as the lowest partial present. The fundamental may be created by vibration over the full length of a string or air column, or a higher harmonic chosen by the player. The fundamental is one of the harmonics. A harmonic is any member of the harmonic series, an ideal set of frequencies that are positive integer multiples of a common fundamental frequency. The reason a fundamental is also considered a harmonic is because it is 1 times itself.
The fundamental is the frequency at which the entire wave vibrates. Overtones are other sinusoidal components present at frequencies above the fundamental. All of the frequency components that make up the total waveform, including the fundamental and the overtones, are called partials. Together they form the harmonic series. Overtones which are perfect integer multiples of the fundamental are called harmonics. When an overtone is near to being harmonic, but not exact, it is sometimes called a harmonic partial, although they are often referred to simply as harmonics. Sometimes overtones are created that are not anywhere near a harmonic, and are just called partials or inharmonic overtones.
The fundamental frequency is considered the first harmonic and the first partial. The numbering of the partials and harmonics is then usually the same; the second partial is the second harmonic, etc. But if there are inharmonic partials, the numbering no longer coincides. Overtones are numbered as they appear above the fundamental. So strictly speaking, the first overtone is the second partial (and usually the second harmonic). As this can result in confusion, only harmonics are usually referred to by their numbers, and overtones and partials are described by their relationships to those harmonics.
Consider a spring, fixed at one end and having a mass attached to the other; this would be a single degree of freedom (SDoF) oscillator. Once set into motion, it will oscillate at its natural frequency. For a single degree of freedom oscillator, a system in which the motion can be described by a single coordinate, the natural frequency depends on two system properties: mass and stiffness; (providing the system is undamped). The natural frequency, or fundamental frequency, ω0, can be found using the following equation:
k = stiffness of the spring
m = mass
ω0 = natural frequency in radians per second.
If we desire the natural frequency, we simply divide the omega value by 2π. Or:
f0 = natural frequency (SI unit: Hertz (cycles/second))
k = stiffness of the spring (SI unit: Newtons/metre or N/m)
m = mass (SI unit: kg).
While doing a modal analysis, the frequency of the 1st mode is the fundamental frequency.
- Greatest common divisor
- Missing fundamental
- Natural frequency
- Harmonic series (music)#Terminology
- Pitch detection algorithm
- Scale of harmonics
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