Particulate matter

Particulate matter is the sum of all solid and liquid particles suspended in air many of which are hazardous. 

• This complex mixture includes both organic and inorganic particles, such as dust, pollen,soot, smoke, and liquid droplets. 
• These particles vary greatly in size, composition, and origin.

Particle size matter:-

The aerodynamic properties of particles determine how they are transported in air and how they can be removed from it. 

These properties also govern how far they get into the air passages of the respiratory system. Additionally, they provide information on the chemical composition and the sources of particles.

Particles have irregular shapes and their aerodynamic behaviour is expressed in terms of the diameter of an idealised sphere. 

The sampling and description of particles is based on this aerodynamic diameter, which is usually simply referred to as ‘particle size’. 

Particles having the same aerodynamic diameter may have different dimensions and shapes. Some airborne particles are over 10,000 times bigger than others in terms of aerodynamic diameter.

Based on size, particulate matter is often divided into two main groups:

• The coarse fraction contains the larger particles with a size ranging from 2.5 to 10 µm (PM₁₀ - PM_2.5).
• The fine fraction contains the smaller ones with a size up to 2.5 µm (PM_2.5). The particles in the fine fraction which are smaller than 0.1 µm are called ultrafine particles.

How are particles formed?

Coarse particles are produced by the mechanical break-up of larger solid particles. The coarse fraction can include dust from roads, agricultural processes, uncovered soil or mining operations, as well as non-combustible materials released when burning fossil fuels. Pollen grains, mould spores, and plant and insect parts can also contribute to the coarse fraction. Finally, evaporation of sea spray can produce large particles near coasts.

Fine particles are largely formed from gases. Ultrafine particles (up to 0.1 µm) are formed by nucleation, which is the initial stage in which gas becomes a particle. These particles can grow up to a size of 1 µm either through condensation, when additional gas condensates on the particles, or through coagulation, when two or more particles combine to form a larger particle. Particles produced by the intermediate reactions of gases in the atmosphere are called secondary particles.

• Combustion of fossil fuels such as coal, oil, and petrol can produce
• coarse particles from the release of non-combustible materials such as fly ash,
• fine particles from the condensation of materials vaporized during combustion, and
• secondary particles through the atmospheric reactions of sulphur oxides and nitrogen oxides initially released as gases.