Detection of Organic Components in
Atmospheric Aerosols
Atmospheric particles that can be natural or anthropogenic, are defined as a suspension of fine
solid or liquid particles in air. They are either emitted or formed in the atmosphere and their
particle sizes affect their transport and deposition. Their most important impacts, such as
respiratory health hazards, visibility reduction, and climate effects are dependent upon the
particle size that ranges from a few nanometers to a few hundred micrometers. Chemical
composition of aerosol particles is generally determined by gas- and liquid-chromatographic
techniques, mostly with mass spectrometric detection. Use of liquid chromatography (LC) has
increased in atmospheric analysis due to the recently recognized importance of highly oxidized
compounds in aerosol formation and growth, improved separation efficiency of the columns, and
high-resolution mass spectrometric detection.
Sampling and Sample Preparation
Sample preparation techniques used for solid samples, such as extraction, clean-up, and
concentration, are also suitable for aerosol samples, in general. The analysis mode (target,
nontarget) and analysis technique determine the choice of sample preparation method. Liquid
extraction, assisted with temperature, pressure, ultrasound, or microwaves, is frequently used
(Table 1). Soxhlet extraction, which gives the best recoveries, is less used, because of long
extraction time and high solvent consumption. Sonication, instead, is the most popular due to
cheap instrumentation, low solvent consumption, and short extraction time. Concentrations of
aerosol constituents are relatively low; thus samples are usually concentrated after extraction
with nitrogen flow.
Table 1. Examples of Sampling and Sample Preparation Methods for the Analysis of Different
Compound Classes in Atmospheric Aerosols2
Compound
Class
Sampling
Sample Preparation
Analysis
PAHs
HVS (quartz), 24 h,
550 m3
Microwave (120°C, 900
V, 40 min, 20 mL
CH2Cl2)
HPLC (C18)-FLD
Hydroxy-PAHs
HVS (quartz), 24 h,