
Small particles are required, to provide a large surface-area-to-mass ratio and for the solid to
remain in suspension. Surface absorption of air (oxygen) by the solid, or the evolution of combustible
gas or vapour on heating, may be a predisposing factor. The presence of moisture reduces the
tendency to ignite: it also favours agglomeration to produce larger particles. An increase in the
proportion of inert solid in particles tends to reduce combustibility.
The explosive range of dusts in air can be very wide. The limits vary with the chemical
composition and with the size of the particles. The lower limits are equivalent to a dense fog in
appearance. The upper limits are ill defined but are not generally of practical significance. The
important characteristics are the ease of ignition, lower explosive limits, the maximum explosion
pressure and the rates of pressure rise. Organic or carbonaceous materials, or easily oxidizable
metals (e.g. aluminium or magnesium) are more hazardous than nitrogenous organic materials.
The least hazardous materials are those which contain an appreciable amount of mineral matter.
For a summary of data for a range of dusts refer to Table 6.2.
Oxygen requirements
Most substances require a supply of oxygen in order to burn. Air contains about 21% oxygen.
Gases and vapours can produce flammable mixtures in air within certain limits. When the oxygen
content of air is increased (e.g. by enrichment with pure oxygen from a leaking cylinder) the fire
hazard is increased. Conversely, lowering the oxygen by, for instance, the presence of an inert gas
such as nitrogen, argon, or carbon dioxide, reduces the fire risk. Some chemicals contain their
own supply of oxygen (e.g. perchlorates) and can burn even in an oxygen-deficient atmosphere.
Just as chemicals can react violently with oxygen to produce a fire, certain substances can inflame
on reaction with other oxidizing agents (e.g. hydrocarbons with chlorine). Upper and lower
flammable limits exist for such systems. Oxidizing agents generally assist combustion (see page
234).
There is a critical oxygen content below which ignition of combustible dusts or gases will not
occur and this can provide a means for safe operation under an inert atmosphere, i.e. ‘inerting’.
Ignition sources
Combustion is generally initiated by the introduction of a finite amount of energy to raise a finite
volume of the material to its ignition temperature. Potential ignition sources for vapour–air
mixtures are listed in Table 6.3, and temperatures in Table 6.4. Heat sources can be chemical
energy (spontaneous combustion, chemical reaction), mechanical energy (e.g. friction), radiant
energy, solar energy, static energy or electrical current. Thus heat is generated from electrical
current by resistance, arcing or sparking. Resistance arises when the current flow exceeds the
capacity of the wire. The result is often a blown fuse, tripped circuit breaker or heating of the
circuit wire. Arcing occurs when electrical current jumps from one point to another, e.g. in a
switch or connection box when wires separate from connections, or as a result of worn insulation
between positive and neutral wires.
Common ignition sources include:
• Naked flames (e.g. Bunsen burners, welding torches, blow lamps, furnaces, pilot lights, matches,
glowing cigarettes or embers).
• Sparks created by arcs in electrical switchgear, engines, motors, or by friction (e.g. lighter
spark). Aluminium, magnesium, titanium and their alloys have an affinity for oxygen and in a
thermite reaction with rust produce temperatures ≤3000°C. A thermite flash can result from the
IGNITION AND PROPAGATION OF A FLAME FRONT 199