At the time of its greatest popularity, flame atomic absorption was used primarily in
the analysis of solutions for trace metals. For solid samples, the technique requires
that samples be dissolved. With the exception of a few well-documented interferences,
samples and standards need not be made very similar. Flame atomic
absorption offers the analyst high precision (0.2 to 0.5% RSD) determinations and
moderate detection limits. Electrothermal atomization (graphite furnace) atomic
absorption spectrometry, on the other hand, offers high sensitivity and low detection
limits. Graphite furnace
AAS (GF
AAS) does provide poorer precision and a higher
level of matrix interferences than are experienced with the flame-based technique.
However, advances such as the use of stabilized temperature platform furnace
(STPF) technology and Zeeman background correction have reduced or eliminated
most of the interferences previously associated with GF
AAS.
Both the flame and graphite furnace
AAS techniques are used widely today and
both provide excellent means of trace elemental analysis. Most atomic absorption
instruments are limited, however, in that they typically measure only one element
at a time. The instrumental setup or operating conditions may require changing
hollow cathode lamps or using different furnace parameters for each element to be
determined. Because of the different operating conditions and furnace parameters
required for each element, conventional atomic absorption techniques do not lend
themselves readily to multi-element simultaneous analysis.
Also, despite advances in nonlinear calibration, the need for sample dilution is
greater than for present-day OES techniques, due to the limited working (calibration)
range for the
AAS techniques. Consequently, devices for automatic sample dilution
when a sample concentration exceeds the calibration range are available. For those
samples that require element preconcentration for lower detection limits, flow-injection
techniques coupled with cold vapor mercury or hydride generation equipment
and GF
AAS can not only provide significant improvements in detection limits, over
100 times better as compared to conventional hydride generation AA, but also may
reduce potential interferences by the complete removal of matrix components.
Stanley Greenfield of Birmingham, England is credited with the first published report
(1964) on the use of an atmospheric pressure inductively coupled plasma (ICP) for
elemental analysis via optical emission spectrometry (OES) [1]. The conclusions
from this landmark paper summarize what Greenfield identified as the advantages
of plasma emission sources over flames, ac sparks and dc arcs:
The plasma source has a high degree of stability, has the ability to
overcome depressive interference effects caused by formation of
stable compounds, is capable of exciting several elements that are
not excited in orthodox chemical flames, and gives increased sensitivity
of detection [over flame photometry].