Toxic hazard is a difficult notion to understand. It relates to certain targets’ exposure to a hazard which corresponds with a cloud generated following accidental discharge of a chemical substance into the atmosphere (leak, tank failure etc.).
Toxic gas discharge can be continuous (jet) or short-lived (puff). It is dispersed into the atmosphere under the effect of its initial velocity, the gravity effect due to gas density, wind, atmospheric conditions (atmospheric stability, i.e. vertical temperature profile), hygrometry and relief.
Atmospheric dispersion corresponds with the evolution of a cloud of hazardous products over time and space. Two simultaneous phenomena occur when a gas is dispersed into the atmosphere. These phenomena are gas transport, notably under the effect of the wind, and gas dissemination. During its dissemination, the cloud absorbs air and therefore dilutes. Its toxicity thus decreases as the distance from the discharge point increases.
The parameters most influential on distant toxic effects are as follows:
There are numerous possible causes, mostly including:
Toxic gases are characterised by their effects on man by the notion of dose, taking into account gas concentration in the air and time of exposure to this atmosphere.
Three thresholds are distinguished:
Gases with high toxicity and high density, such as chlorine, are particularly dangerous: significant effects can reach distances of up to ten kilometres for the most serious types of discharge (example: total failure of a large capacity).
Protection resources against the causes of toxic leakage will not be examined in great detail.
There are several ways to ensure protection against toxic effects, for example:
For further information:
How are risks studied?
Atmospheric dispersion: data sheet 2 of the Circular of 28 December 2006