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Aerosols.

Invisible, everywhere, and in every breath you take. Here's what they are — and why they matter.

What they are

An aerosol is a gas carrying tiny solid or liquid particles. Small enough to float. Small enough to breathe.

FogWater droplets
SmokeCombustion particles
DustMineral particles
CloudsDroplets on particles
SpraysLiquid droplets
BreathExhaled droplets

Liquid or solid.

Droplets — like mist, sprays or the water in clouds — and solid particles — like dust, soot or pollen — are both aerosols. Many real particles are a mix of both.

Primary or secondary.

Some particles are released directly, like sea salt or soot. Others form in the air itself, when gases react and condense into new particles.

Sources

Where aerosols come from.

Most of the particles in our air are natural. But the ones we make ourselves are often the smallest — and the ones that matter most for health.

Oceans

Breaking waves and bursting bubbles launch salt particles into the air. By mass, sea spray is one of the largest aerosol sources on the planet.

Deserts

Wind lifts mineral dust that travels across continents. Saharan dust regularly reaches Europe and helps fertilise the Amazon.

5,000+ km

across the Atlantic

Volcanoes

Eruptions inject sulfur gases high into the atmosphere, where they form particles that reflect sunlight.

≈ 0.5 °C

global cooling after Mount Pinatubo, 1991

Forests

Trees release compounds that turn into particles — the blue haze over forested hills. Plus pollen and fungal spores.

Wildfires

Smoke from large fires can stay aloft for weeks and cross oceans before it settles.

And you.

Breathing, speaking, singing, coughing — every one of them releases fine droplets from your airways. You're producing aerosols right now.

Every breath.

Size

Size decides everything.

Drag the slider to explore five orders of magnitude — and see where a particle of that size lands when you breathe it in.

2.5 µm
Fine dust · PM2.5
The air-quality benchmark. Small enough to travel deep into the lung.
1 nm100 µm
Small airways & deep lung
Where most particles of this size settle

Simplified. Deposition depends on breathing pattern, particle density and shape.

In the body

What happens when you inhale.

The respiratory tract is a natural particle filter. Each section catches a different size — which is exactly why size control is the key to inhaled medicine.

> 10 µm

Nose and throat

Large particles can't follow the bends of the airway. They hit the walls early and are swallowed or cleared.

5 – 10 µm

Windpipe and bronchi

Medium particles make it past the throat but settle in the larger airways.

1 – 5 µm

Small airways and deep lung

The target window for most inhaled medicines. These particles travel deep and settle gently.

0.1 – 1 µm

Mostly breathed out again

Too small to settle quickly, too large to diffuse fast — many leave with the next exhale.

≤ 0.1 µm

Alveoli

Ultrafine particles move by diffusion and can reach the tiny air sacs where gas exchange happens.

23

generations of branching airways

≈ 480 M

alveoli in an adult lung

50–100 m²

of surface for gas exchange

Climate

Every cloud begins with an aerosol.

Water vapour needs a surface to condense on. Without aerosol particles as seeds, clouds as we know them wouldn't form.

Seeds for clouds

Sea salt, sulfate and dust particles act as cloud condensation nuclei. More particles mean more, smaller droplets — and brighter clouds.

Mirrors in the sky

Particles scatter and absorb sunlight. Their overall effect cools the planet — and how much remains one of the big open questions in climate science.

Medicine

Breathing in, on purpose.

Inhaled medicine reaches the lung directly and acts fast. The devices have improved over time — but the core principles haven't moved much.

1800s

The first portable nebulisers turn liquid medicine into a mist.

1956

The pressurised metered-dose inhaler arrives — the “puffer” most people know.

1960s–70s

Dry powder inhalers deliver medicine without propellants, driven by the patient's breath.

2000s

Soft mist inhalers produce a slow, fine cloud that's easier to inhale.

This is where we come in.

We combine chemistry and aerosol physics to control what happens between the molecule and the breath.