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5.Audio fundamentals

  1. 1Sound & frequency
  2. 2Mic, line & speaker level
  3. 3Balanced vs. unbalanced
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Sound & frequency

Pressure waves, wavelength, the range of hearing — and where speech lives.

Chapter 59 minFrequency explorer

Everything in audio — microphones, DSP, loudspeakers, acoustic panels — exists to capture, move or shape one thing: small, rapid changes in air pressure. Before any cable or connector, it helps to understand what that thing is and why its frequency changes how it behaves.

Sound is a pressure wave

When someone speaks, their vocal folds push and pull on the air. Each push squeezes the molecules together (compression); each pull spreads them apart (rarefaction). That pattern travels outward. The air itself barely moves — the pressure change is what travels, at roughly 343 metres per second in room-temperature air.

A microphone is a pressure sensor: a thin diaphragm moved by those changes, turned into a matching voltage. A loudspeaker is the same idea run backwards. In between, every piece of audio gear is handling a voltage that is a copy — an analog — of those pressure changes.

Frequency and wavelength

Frequency is how many complete cycles happen each second, measured in hertz (Hz). We hear it as pitch. Wavelength is the physical distance one cycle occupies in the air. The two are tied together by the speed of sound:

wavelength (m) = 343 ÷ frequency (Hz)

That gives a staggering range. A 20 Hz rumble has a wavelength of about 17 metres — longer than most rooms. A 20 kHz tone is under 2 centimetres. Same air, same speed, and yet the two behave like entirely different things.

Frequency explorer

632 Hz

Mids · 5.0 octaves above 20 Hz

20 Hz100 Hz1 kHz10 kHz20 kHz
Voice fundamentals
Narrowband phone call
Wideband (HD) voice
Wavelength in air54 cm
Phone
Ceiling tile
Door
Meeting room
1 cm20 m
Mids

500 Hz–2 kHz

Where the ear is busy: vowels and the core of most instruments.

How it behaves

In between

Similar in size to people and furniture, so objects partly block and scatter it.

Wavelength = 343 m/s ÷ frequency (air at about 20 °C). Band names are informal and their edges vary between sources. The tone plays quietly; laptop speakers can't reproduce the lowest frequencies.

Sweep from 20 Hz to 20 kHz. Watch where speech and phone calls sit, and how wavelength shrinks from room-sized to fingertip-sized.

The range of human hearing

The textbook range is 20 Hz to 20 kHz. In practice the top end falls with age and noise exposure, and many adults hear little above 15 kHz. Hearing is also far from flat: we are most sensitive between about 2 and 5 kHz, and much less sensitive to low frequencies at quiet levels.

Pitch works on octaves — each doubling of frequency sounds like the same step. 100 Hz to 200 Hz is one octave; so is 5 kHz to 10 kHz. That is why audio graphs use a logarithmic frequency axis, and why the hearing range is better described as about ten octaves than as “19,980 Hz wide.”

Where speech lives

RangeWhat's thereWhy it matters
~85–255 HzFundamental pitch of adult voicesGives a voice its weight and identity
~250 Hz–2 kHzVowels and most of the voice's energyLoudness and body
~2–4 kHzConsonants: t, k, s, f…Intelligibility — tells ‘fifty’ from ‘sixty’
300 Hz–3.4 kHzNarrowband telephone audioWhy classic phone calls sound thin
50 Hz–7 kHzWideband (‘HD’) voiceStandard on modern conferencing platforms
~85–255 Hz
What's thereFundamental pitch of adult voices
Why it mattersGives a voice its weight and identity
~250 Hz–2 kHz
What's thereVowels and most of the voice's energy
Why it mattersLoudness and body
~2–4 kHz
What's thereConsonants: t, k, s, f…
Why it mattersIntelligibility — tells ‘fifty’ from ‘sixty’
300 Hz–3.4 kHz
What's thereNarrowband telephone audio
Why it mattersWhy classic phone calls sound thin
50 Hz–7 kHz
What's thereWideband (‘HD’) voice
Why it mattersStandard on modern conferencing platforms
Key idea

Most of a voice's energy is low; most of its intelligibility is high. A room that sounds loud but muffled has lost its upper mids — which is why speech systems care far more about clarity between 1 and 4 kHz than about deep bass.

Why wavelength matters in a room

Sound interacts with objects that are similar to or larger than its wavelength. This one idea explains a great deal of room acoustics:

  • Low frequencies wrap around things. A 100 Hz wave is 3.4 m long; a table or a person barely registers to it. Bass leaks through walls and doors, and it's why you hear the thump from the room next door but not the words.
  • High frequencies travel in beams. Short wavelengths are blocked by heads and furniture and soaked up by soft surfaces. Loudspeakers become more directional as frequency rises.
  • Absorbers need depth to work low. A common rule of thumb says porous material works well once it is around a quarter-wavelength thick. A 50 mm panel handles speech frequencies nicely but does little to bass — taming low frequencies needs much deeper treatment.
In the field

A conference room with glass walls, a hard table and a bare ceiling will reflect speech frequencies everywhere. No microphone or DSP fully fixes that — adding absorption is often the cheapest intelligibility upgrade in the room.

Key takeaways

  • 01Sound is a travelling pressure wave; microphones and loudspeakers convert between pressure and voltage.
  • 02Wavelength = 343 ÷ frequency: about 17 m at 20 Hz and under 2 cm at 20 kHz.
  • 03Human hearing spans roughly 20 Hz–20 kHz (about ten octaves), and the top end falls with age.
  • 04Voice energy is mostly low, but intelligibility lives in the consonants between about 2 and 4 kHz.
  • 05Low frequencies wrap around objects and need deep treatment; high frequencies beam and are easily absorbed.

Check your understanding

Q1Roughly what is the wavelength of a 1 kHz tone in air?

Q2A remote participant says the room sounds loud but muffled and hard to understand. Which range is most likely missing?

Q3Why do thin acoustic panels do little to reduce boomy bass?

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