Emissions from mesoscale in situ oil fires: The mobile 1991 experiments

A series of 14 mesoscale burns were conducted in 1991 to study various aspects of oil burning in situ. Extensive sampling and monitoring of these burns were conducted to determine the emissions. This was done at two downwind ground stations, one upwind ground station and in the smoke plume using a blimp and a remote-controlled helicopter. Particulate samples in air were taken and analyzed for polycyclic aromatic hydrocarbons (PAHs), PAHs were found to be lower in the soot than in the starting oil. Metals in the oil were found concentrated in the residue and could not be measured in soot samples using conventional industrial hygiene sampling techniques, Particulates in the air were measured by several means and found to be greater than recommended exposure Levels only up to 150 m downwind at ground level. Combustion gases including carbon dioxide, sulphur dioxide and carbon monoxide did not reach exposure level maximums. These gases were emitted over a broad area around the fire and are not directly associated with the plume trajectory. Volatile organic compound (VOCs) emissions are extensive from fires, but the levels are less than those emitted from a non-burning test spill. Over 50 compounds were identified and quantified, several at possible levels of concern up to 200 m downwind. Water under the burns was analyzed; no analytes of concern could be found at the detection levels of the methods. The burn residue was analyzed for the same compounds as the air particulate samples. The residue contained elevated amounts of metals, PAHs were at a lower concentration in the residue than in the starting oil, however there is a slight differential concentration increase in some higher molecular weight species. Overall, indications from these mesoscale trials are that emissions from in situ burning are low in comparison to other sources of emissions and result in concentrations of air contaminants that are below exposure limits beyond 500 m downwind. (C) 1997 Elsevier Science Ltd.