Gas Chromatography Mass Spectrometry

Ronald A. Hites
Indiana University
School of Public and Environmental Affairs
and Department of Chemistry


Summary

General Uses

• Identification and quantitation of volatile and semivolatile organic compounds in complex mixtures
• Determination of molecular weights and (sometimes) elemental compositions of unknown organic
compounds in complex mixtures
• Structural determination of unknown organic compounds in complex mixtures both by matching
their spectra with reference spectra and by a priori spectral interpretation

Common Applications
• Quantitation of pollutants in drinking and wastewater using official U.S. Environmental Protection
Agency (EPA) methods
• Quantitation of drugs and their metabolites in blood and urine for both pharmacological and forensic
applications

610 Handbook of Instrumental Techniques for Analytical Chemistry
• Identification of unknown organic compounds in hazardous waste dumps
• Identification of reaction products by synthetic organic chemists
• Analysis of industrial products for quality control

Samples
State
Organic compounds must be in solution for injection into the gas chromatograph. The solvent must be
volatile and organic (for example, hexane or dichloromethane).
Amount
Depending on the ionization method, analytical sensitivities of 1 to 100 pg per component are routine.
Preparation
Sample preparation can range from simply dissolving some of the sample in a suitable solvent to extensive
cleanup procedures using various forms of liquid chromatography.
Analysis Time
In addition to sample preparation time, the instrumental analysis time usually is fixed by the duration
of the gas chromatographic run, typically between 20 and 100 min. Data analysis can take another 1 to
20 hr (or more) depending on the level of detail necessary.
Limitations
General
Only compounds with vapor pressures exceeding about 10–10 torr can be analyzed by gas chromatography
mass spectrometry (GC-MS). Many compounds with lower pressures can be analyzed if they are
chemically derivatized (for example, as trimethylsilyl ethers). Determining positional substitution on
aromatic rings is often difficult. Certain isomeric compounds cannot be distinguished by mass spectrometry
(for example, naphthalene versus azulene), but they can often be separated chromatographically.
Accuracy
Qualitative accuracy is restricted by the general limitations cited above. Quantitative accuracy is controlled
by the overall analytical method calibration. Using isotopic internal standards, accuracy of
±20% relative standard deviation is typical.
Gas Chromatography Mass Spectrometry 611
Sensitivity and Detection Limits
Depending on the dilution factor and ionization method, an extract with 0.1 to 100 ng of each component
may be needed in order to inject a sufficient amount.
Complementary or Related Techniques
• Infrared (IR) spectrometry can provide information on aromatic positional isomers that is not
available with GC-MS; however, IR is usually 2 to 4 orders of magnitude less sensitive.
• Nuclear magnetic resonance (NMR) spectrometry can provide detailed information on the exact
molecular conformation; however, NMR is usually 2 to 4 orders of magnitude less sensitive.
Introduction
Like a good marriage, both gas chromatography (GC; see Chapter 8) and mass spectrometry (MS; see
Chapter 30) bring something to their union. GC can separate volatile and semivolatile compounds with
great resolution, but it cannot identify them. MS can provide detailed structural information on most
compounds such that they can be exactly identified, but it cannot readily separate them. Therefore, it
was not surprising that the combination of the two techniques was suggested shortly after the development
of GC in the mid-1950s.
Gas chromatography and mass spectrometry are, in many ways, highly compatible techniques. In
both techniques, the sample is in the vapor phase, and both techniques deal with about the same amount
of sample (typically less than 1 ng). Unfortunately, there is a major incompatibility between the two
techniques: The compound exiting the gas chromatograph is a trace component in the GC’s carrier gas
at a pressure of about 760 torr, but the mass spectrometer operates at a vacuum of about 10–6 to l0–5 torr.
This is a difference in pressure of 8 to 9 orders of magnitude, a considerable problem.
How It Works
The Interface
The pressure incompatibility problem between GC and MS was solved in several ways. The earliest approach,
dating from the late 1950s, simply split a small fraction of the gas chromatographic effluent into
the mass spectrometer (1). Depending on the pumping speed of the mass spectrometer, about 1 to 5%
of the GC effluent was split off into the mass spectrometer, venting the remaining 95 to 99% of the analytes
into the atmosphere. It was soon recognized that this was not the best way to maintain the high
sensitivity of the two techniques, and improved GC-MS interfaces were designed (2). These interfaces
reduced the pressure of the GC effluent from about 760 torr to l0–6 to 10–5 torr, but at the same time, they
612 Handbook of Instrumental Techniques for Analytical Chemistry
passed all (or most) of the analyte molecules from the GC into the mass spectrometer. These interfaces
were no longer just GC carrier gas splitters, but carrier gas separators; that is, they separated the carrier
gas from the organic analytes and actually increased the concentration of the organic compounds in the
carrier gas stream.
The most important commercial GC carrier gas separator is called the jet separator; see Fig. 31.1
(3). This device takes advantage of the differences in diffusibility between the carrier gas and the organic
compound. The carrier gas is almost always a small molecule such as helium or hydrogen with a
high diffusion coefficient, whereas the organic molecules have much lower diffusion coefficients. In
operation, the GC effluent (the carrier gas with the organic analytes) is sprayed through a small nozzle,
indicated as d1 in Fig. 31.1, into a partially evacuated chamber (about 10–2 torr). Because of its high
diffusion coefficient, the helium is sprayed over a wide solid angle, whereas the heavier organic molecules
are sprayed over a much narrower angle and tend to go straight across the vacuum region. By collecting
the middle section of this solid angle with a skimmer (marked d3 in Fig. 31.1) and passing it to
the mass spectrometer, the higher-molecular-weight organic compounds are separated from the carrier
gas, which is removed by the vacuum pump. Most jet separators are made from glass by drawing down
a glass capillary, sealing it into a vacuum envelope, and cutting out the middle spacing (marked d2 in
Fig. 31.1). It is important that the spray orifice and the skimmer be perfectly aligned.
These jet separators work well at the higher carrier gas flow rates used for packed GC columns (10
to 40 mL/min); however, there are certain disadvantages. Packed GC columns are an almost infinite
source of small particles upstream of the jet separator. If one of those particles escapes from the column,
it can become lodged in the spray orifice and stop (or at least severely reduce) the gas flow out of the
GC column and into the mass spectrometer. Part of this problem can be eliminated with a filter between
the GC column and the jet separator, but eventually a particle will plug up the orifice. In fact, sometimes
it is not a particle at all, but rather tar (mostly pyrolyzed GC stationary phase) that has accumulated in
the spray orifice over time. Clearly, these devices require maintenance.
Currently, the most common strategy, which is ideally suited for capillary GC columns, is to pass
all of the carrier gas flow into the ion source of the mass spectrometer (4). This works only if the GC
gas flow is sufficiently small and the pumping speed of the mass spectrometer’s vacuum system is suf-
Figure 31.1 The jet separator, a device for interfacing a
packed column GC with an MS. The three distances are
typically d1, 100 μm; d2, 300 μm; and d3, 240 μm.
Gas Chromatography Mass Spectrometry 613
ficiently high to handle the gas flow. For most capillary GC columns, the gas flow is 1 to 2 mL/min,
and for most modern mass spectrometers, the pumping speed is at least 300 L/sec. The development of
flexible, fused silica capillary columns has made this approach routine. In fact, the only time a jet separator
is now used is for a few applications that require packed or thick stationary phase GC columns
(for example, for permanent gas analysis).
In practice, most GC-MS interfacing is now done by simply inserting the capillary column directly
into the ion source. Fig. 31.2 is a diagram of one such system. The fused silica column runs through
a 1/16-in.-diameter tube directly into the ion source. Other gases, such as methane for chemical ionization,
are brought into the ion source by a T joint around the capillary column. One of the other two
lines into the ion source is used for a thermocouple vacuum gauge tube so that the pressure in the ion
source can be roughly measured. The remaining line into the ion source is for the delivery of the mass
spectrometer calibration standard, perfluorotributylamine. Most joints are welded together to avoid
leaks when this inlet system is thermally cycled or vented. The only removable (Swagelok) fitting is
at the junction of the GC column and the far end of the inlet tube (marked with an asterisk in Fig. 31.2).
This fitting uses Vespel ferrules. Once the ferrules are on the GC column and it is in the ion source, it
is desirable to cut off a few centimeters of the column, if possible. This eliminates the possibility of
fine particles partially occluding the end of the column.
If the end of the column cannot be placed directly in the ion source, the material in the GC-MS
interface becomes important. The interface is held at 250 to 280 °C; thus, it should not include a reactive
metal (such as copper). In some interfaces, glass-lined stainless steel tubing has been used, even though
this tubing is difficult to bend properly.
Figure 31.2 A typical GC-MS interface for fused silica capillary GC columns. The end of the GC column enters
the ion source of the mass spectrometer.
614 Handbook of Instrumental Techniques for Analytical Chemistry
In summary, for capillary GC-MS, the best interface is no interface at all; run the flexible, fused
silica GC column directly into the ion source. Using a column that is 25 to 30 m long by 220 to 250 μm
inner diameter gives an ion source pressure of 10–6 to 10–5 torr, a more than acceptable pressure at which
to obtain electron impact spectra. This gives a helium or hydrogen GC carrier gas velocity of 25 to 35
cm/sec or a flow of about 1 to 2 mL/min. The GC columns most widely used for GC-MS are those in
which the stationary phase has been chemically bonded to the fused silica; DB-5 is a common trade
name. Occasionally, there have been problems with the plastic cladding on the outside of the GC column.
This cladding is usually hot (typically 250 °C) and under vacuum. Thus, it may decompose, giving
background ions in the mass spectrum or weakening the fused silica itself.
The Data System
The amount of data that can be produced during one GC-MS experiment is overwhelming. In a typical
GC-MS experiment, the mass spectrometer might be scanned every 2 sec during a 90-min GC
run, whether GC peaks are entering the mass spectrometer or not. Assuming that each mass spectrum
has an average of 100 mass/intensity measurements, one such GC-MS experiment will give 270,000
mass/intensity pairs. Because these data have several significant figures and because other ancillary
data are also obtained, the data output from a typical GC-MS experiment is about 1 megabyte. To
manage this high data flow, computers are required; thus, it is virtually impossible to purchase a GCMS
system without a powerful (but small) computer acting as a data system.
How do data systems work? Two things are going on at the same time (5). There are two different
rates within the system. There is a slow rate that times the start and stop of the mass spectrometer
scan. This is usually set such that 10 to 15 mass spectra are obtained across a typical GC peak. Because
these peaks are usually on the order of 20 to 30 sec wide, the mass spectrometer scan speed is
usually set at 2 to 3 sec per spectrum. While this scan is going on, the computer must read the output
of the electron multiplier at a rate fast enough to define the mass peak profile. In most commercial
GC-MS data systems, the voltage output from the preamplifier on the electron multiplier is converted
from an analog signal to a digital value (using an analog-to-digital converter) at a rate of 10,000 to
100,000 times per sec. This process generates large amounts of data: If the analog-to-digital converter
worked at 10,000 conversions/second, each minute of the GC-MS experiment would generate
600,000 numbers. This would quickly fill most bulk storage devices; thus, to avoid saving all of these
data, most data systems find the mass peaks in real time and convert them into mass intensity pairs,
which are then stored on the computer’s hard disk. Once the most recent mass spectral scan is stored,
this cycle is repeated until the end of the gas chromatogram is reached. Each of the spectra stored on
the hard disk has a retention time associated with it, which can be related directly to the gas chromatogram
itself. The latter is usually reconstructed by the GC-MS data system by integrating the
mass spectrometer output. All modern GC-MS data systems are capable of displaying the mass spectrum
on the computer screen as a bar plot of normalized ion abundance versus mass-to-change (m/z)
ratio (often called mass). Like the other parts of the GC-MS instrument, the data system must be calibrated.
Typically this is done by running a standard compound, such as perfluoro-tributylamine.
What It Does
Gas chromatographic mass spectrometry is the single most important tool for the identification and
Gas Chromatography Mass Spectrometry 615
quantitation of volatile and semivolatile organic compounds in complex mixtures. As such, it is very
useful for the determination of molecular weights and (sometimes) the elemental compositions of unknown
organic compounds in complex mixtures. Among other applications, GC-MS is widely used for
the quantitation of pollutants in drinking and wastewater. It is the basis of official EPA methods. It is
also used for the quantitation of drugs and their metabolites in blood and urine. Both pharmacological
and forensic applications are significant. GC-MS can be used for the identification of unknown organic
compounds both by matching spectra with reference spectra and by a priori spectral interpretation. The
identification of reaction products by synthetic organic chemists is another routine application, as is
the analysis of industrial products for control of their quality.
To use GC-MS, the organic compounds must be in solution for injection into the gas chromatograph.
The solvent must be volatile and organic (for example, hexane or dichloromethane). Depending
on the ionization method, analytical sensitivities of 1 to 100 pg per component are routine. Sample
preparation can range from simply dissolving some of the sample in a suitable solvent to extensive
cleanup procedures using various forms of liquid chromatography. In addition to the sample preparation
time, the instrumental analysis time is usually fixed by the duration of the gas chromatographic run,
typically between 20 and 100 min. Data analysis can take another 1 to 20 hr (or more) depending on
the level of detail necessary.
GC-MS has a few limitations. Only compounds with vapor pressures exceeding about 10–10 torr
can be analyzed by GC-MS. Many compounds that have lower pressures can be analyzed if they are
chemically derivatized (for example, as trimethylsilyl ethers). Determining positional substitution on
aromatic rings is often difficult. Certain isomeric compounds cannot be distinguished by mass spectrometry
(for example, naphthalene versus azulene), but they can often be separated chromatographically.
Quantitative accuracy is controlled by the overall analytical method calibration. Using isotopic
internal standards, accuracy of ±20% relative standard deviation is typical.
Mass Spectrometer Components
Electron ionization (Chapter 30) is most commonly used to produce ions from the compounds separated
by the GC. Chemical ionization may also be used. Quadrupole (p. 656), ion trap (p. 656), and time-offlight
analyzers may be used to separate ions in the MS. These analyzers have rapid response times and
relatively low costs.
Analytical Information
GC-MS is used both for the qualitative identification and for the quantitative measurement of individual
components in complex mixtures. There are different data analysis strategies for these two applications.
Qualitative
There are three ways of examining GC-MS data. First, the analyst can go through the gas chromatogram
(as reproduced by the mass spectrometer) and look at the mass spectra scanned at each GC peak maximum.
This has the advantage of being relatively quick but the disadvantage of missing components of
the mixture that are not fully resolved by the GC column. The second approach is to look at each mass
616 Handbook of Instrumental Techniques for Analytical Chemistry
spectrum in turn, in essence stacking up the mass spectra one behind the other and examining them individually.
This has the advantage of completeness but the disadvantage of tedium. The third approach
is to look at the intensity of one particular mass as a function of time.
This third approach makes use of the three-dimensional nature of GC-MS data. Two of these dimensions
are the mass versus intensity of the normal mass spectrum; the third dimension is the GC retention
time over which the mass spectral data are acquired. This idea is illustrated in Fig. 31.3. The xaxis
represents GC retention time, the y-axis represents intensity, and the z-axis represents mass (or
more properly, m/z ratios). As shown in Fig. 31.3, a mass spectrum is displayed in the y–z plane. Because
a mass spectrum is scanned every 1 to 3 sec, it is also possible to examine the data in the x–y
plane. This is a plot of the intensity of one selected mass as a function of time. This plot is called a mass
chromatogram (6).
An example may make this concept clear. At the retention time marked with an asterisk in Fig.
31.3, the abbreviated mass spectrum extending into the foreground (the y–z plane) was observed. This
happens to be the mass spectrum of methyl stearate; note the relatively abundant ion at m/z 298, which
is this compound’s molecular weight. The mass chromatogram of m/z 298 is shown in the x–y plane
in Fig. 31.3. Note that this mass chromatogram shows one peak, which corresponds to the retention
time of methyl stearate. In other words, of all the hundreds of mass spectra taken during this GC-MS
experiment, m/z 298 is present in only a very few spectra. Only compounds with m/z 298 in their mass
Figure 31.3 A diagram demonstrating the three-dimensional nature of GC-MS data. The abbreviated mass spectrum
extending onto the foreground is that of methyl stearate; the mass chromatogram of m/z 298 (the molecular
ion of methyl stearate) is also shown.
Gas Chromatography Mass Spectrometry 617
spectra will show up in the mass chromatogram of that mass.
Mass chromatograms can be thought of as a very selective gas chromatographic detector, in this
case, one that responds only to methyl stearate. Other compounds can be selectively detected by picking
other masses. For example, m/z 320 would be a good mass to use for the selective detection of a tetrachlorodibenzo-
p-dioxin because this is its molecular weight. If a mass that is present in the mass spectra
of a class of compounds is selected, that compound class can be selectively detected. For example, m/
z 149 is present in the mass spectra of alkyl phthalates for alkyl chain lengths greater than two carbon
atoms. Thus, the mass chromatogram of m/z 149 would selectively show all the phthalates in a sample.
Mass chromatograms are also useful for determining whether a given mass belongs in a given mass
spectrum. For example, if the liquid phase from a GC column is beginning to thermally decompose, all
of the mass spectra taken during a GC-MS experiment with that column might show a moderately abundant
ion at m/z 207. However, the mass chromatogram of m/z 207 will not show peaks because the
source of this ion is bleeding continuously from the column and is not a discrete compound. In fact, the
mass chromatogram of 207 will probably track the temperature program of the GC column; see trace
(a) in Fig. 31.4. Using this approach, it is easy to distinguish between the ions that really belong in a
given mass spectrum and those from background. By looking at sets of mass chromatograms, it is possible
to determine whether various ions come from the same compound even if the compounds are not
completely resolved by the GC column. If ions belong together (that is, they come from the same GC
peak), the mass chromatograms for all these ions will be superimposable in time; see traces (c) and (d)
in Fig. 31.4. In fact, these mass chromatograms should all have the same peak shape because they all
came from the same GC peak. If the mass chromatograms are not superimposable in time or in shape,
the corresponding ions are probably from different compounds, which may have come out of the GC
column at slightly different retention times; compare trace (b) to traces (c) or (d) in Fig. 31.4.
Because GC-MS experiments are somewhat complicated, there is always a possibility for something
to go wrong. To prevent this, stringent quality assurance procedures are necessary. The following
is a nonexhaustive list of some of these problems and what can be done about them.
First, because the analyst is often working at ultra trace levels (a few nanograms, for example),
Figure 31.4 Hypothetical mass chromatograms of four masses. (a) A background ion from the GC column bleed
(m/z 207, for example); (b) an ion from a later-eluting compound; (c, d) two ions from an earlier-eluting compound.
Note the offset between (b) and (c) or (d).
618 Handbook of Instrumental Techniques for Analytical Chemistry
it is possible for a compound that was not originally in the sample to sneak in during the analytical
procedure. In particular, sample contamination can come from solvents and glassware. The former
problem can be prevented by using high-quality (and expensive) solvents, the latter by heating the
glassware to 450 °C after solvent and acid washing. The most common contaminant is probably di(2-
ethylhexyl)phthalate. Its mass spectrum is shown in Fig. 31.5. Note the important ions at m/z l49,
l67, and 279. It pays to remember this spectrum; it was once published as that of a natural product
(7). Phthalates are extremely common as plasticizers. They are particularly abundant (5 to 20%) in
polyvinylchloride-based plastic products such as Tygon tubing.
Second, if components in the sample decompose before or after workup, the analyst will not obtain
accurate results. Under these conditions, it is possible to identify (and quantitate) a compound that was
not originally in the sample, or the analyte of interest could have vanished from the sample. Thus, both
false positives and false negatives can result from sample decomposition. This can happen while the
sample is waiting to be analyzed or during the analysis itself. For example, a GC injection port held at
250 to 300 °C can cause thermal decomposition of some compounds. One useful procedure is to add
(or spike) the analyte into a sample at a known concentration. If there is a substantial loss of this compound
or the suspicious formation of another compound, sample decomposition may be a problem.
Third, if the GC column or GC-MS interface is not working properly, the whole GC-MS experiment
is in jeopardy. Cold spots are a common problem, as are catalytic surfaces that selectively remove
some compounds from the GC gas stream. These problems can be identified using a mixture of standard
compounds of varying polarities and acidities.
Fourth, either the mass spectrometer itself or the data system may not be working properly. In this
case, incorrect isotope ratios, mass discrimination (ions at higher masses appear less abundant than they
should), or mass assignment errors could occur. The key to identifying these problems is to run an overall
mass spectrometer performance standard. The one recommended (mandated in many cases) by the
EPA is decafluorotriphenylphosphine, the mass spectrum of which is shown in Fig. 31.6. This compound
is a good standard. It is easy to run by GC-MS, and it has ions up to about m/z 450. The abun-
Figure 31.5 Mass spectrum of di(2-ethylhexyl)phthalate, a very common experimental contaminant. The structures
of some ions are shown.
Gas Chromatography Mass Spectrometry 619
dances for the various ions, as required by the EPA, are published in the Federal Register (8) and in
various other official EPA methods (9). These requirements change from time to time, but they are
available from the EPA.
To ensure qualitative identification of an organic compound using GC-MS, several criteria should
be met: First, the mass spectra of the unknown compound and of the authentic compound must agree
over the entire mass range of the spectra. It is particularly important to compare the patterns within narrow
mass ranges (for example, from m/z 50 to 60 in Fig. 31.5); these patterns should agree almost exactly.
In this case, the spectrum of the authentic compound might come from a library of reference
spectra or from the actual compound itself. In the latter case, the compound could be purchased or synthesized.
Second, the GC retention times of the unknown compound and of the authentic compound
must agree within about ±1 to 2 sec. It is often convenient to do this experiment by coinjecting the unknown
mixture and the authentic compound. The GC peak in question should increase in size by the
correct factor. Third, a compound cannot be considered fully identified in a mixture unless two other
questions are addressed: Is the identification plausible? Why is it present in a given sample? If an identification
is implausible or if there is no reason for a compound to be present in a sample, the identification
could be wrong or the compound could be a contaminant.
Quantitative
GC-MS can also be used to measure the concentration of one or more analytes in a complex mixture.
Quantitation can be based on peak areas from mass chromatograms or from selected ion monitoring.
The latter requires more explanation (10).
With the selected ion monitoring technique, the mass spectrometer is not scanned over all masses;
instead, the instrument jumps from one selected mass to another. The advantage of this approach is that
the mass spectrometer spends much more time at a given mass, the signal-to-noise ratio at that mass
Figure 31.6 Mass spectrum of decafluorotriphenylphosphine, an EPA-mandated standard. The structures of some
ions are shown.
620 Handbook of Instrumental Techniques for Analytical Chemistry
improves, and the overall sensitivity of the experiment increases by a factor of 100 to 1000. For example,
the mass spectrometer might integrate for 500 msec at mass m1, jump to mass m2 in 10 msec, integrate
for 500 msec at that mass, and jump back to m1 in 10 msec, repeating this cycle for the duration
of the GC run. In essence, the intensities of the two masses are recorded as a function of GC retention
time, with measurements made every 1.02 sec. In practice, rather than only two masses, 5 to 10 masses
are usually monitored simultaneously for 100 to 200 msec each. In this manner, the GC-MS response
of 5 to 10 compounds, depending on the specificity of the selected masses, can be measured.
The difference between mass chromatograms and selected ion monitoring is significant. With the
latter technique, the responses from only a few preselected masses are recorded. With mass chromatograms,
all of the masses are scanned; thus, no preselection is required. This is the necessary tradeoff for
higher sensitivity. Clearly, the mass spectrum of the analyte must be known so that the masses that
uniquely characterize it can be selected. This information can be obtained from the literature (or from
a library of reference spectra) or from the laboratory. Each selected set of masses can be monitored for
the duration of the complete GC run or for only selected GC retention times (often called time windows).
Selected ion monitoring is almost fully software driven; thus, it is very flexible. Different sets
of masses, different time windows, and different integration times can be easily set up.
To convert the peak areas to mass of analyte, whether from mass chromatograms or from selected
ion monitoring, the peak areas must be calibrated. The two main strategies are based on external and
internal standards. With external standards, the area of one or more mass chromatogram is calibrated
with a known amount of the analyte injected into the GC-MS in a different experiment. Detection limits
of a few nanograms can be achieved with this technique. However, the strategy that gives the most accurate
quantitative results is the use of internal standards, which are known amounts of compounds added
to the sample before isolation of the analytes begins. After sample extraction and cleanup, only the
ratio of response between the analyte and the internal standard must be measured. This ratio multiplied
by the amount of the internal standard gives the amount of the analyte injected into the GC-MS system.
This can be converted to concentration using the correct dilution factors.
The best internal standards are chemically very similar to the analyte; thus, any losses of the analyte
during the analytical procedure are duplicated by losses of the internal standard, so it is a self-correcting
system. Homologues of the analyte can be used as internal standards, but the very best are
isotopically labeled versions of the analyte. Using isotopically labeled standards and selected ion monitoring,
it is possible to get sensitivities of less than 1 pg. Depending on the relationship of the internal
standard to the analyte, the precision and accuracy of most analyses are improved by at least a factor of
2 to 3 over external calibration. The tradeoff is complexity and cost. Ideally, an internal standard for
each analyte in a mixture should be used, and isotopic standards can sometimes cost several hundred
dollars for a few milligrams.
Applications
The analysis of octachlorodibenzo-p-dioxin (OCDD) in sediment from Lake Ontario is a useful example
of a quantitative measurement made with GC-MS. This example also demonstrates the use of isotopically
labeled internal standards. These experiments were done in the author’s laboratory using
electron capture negative ionization, but the principle is the same regardless of the ionization technique
selected.
OCDD has a molecular weight of 456 (usually called M). The mass spectrum of the unlabeled (native)
compound is dominated by an ion cluster corresponding to M-Cl, the most intense peak of which
Gas Chromatography Mass Spectrometry 621
is m/z 423, which is the first isotope peak (the one containing one 37Cl) in this cluster. The isotopic standard
used for this experiment was per-37Cl-labeled OCDD, which has a molecular weight of 472. Its
M-Cl ion is at m/z 435. Because there is no 35Cl in this molecule, there are no isotope peaks. Selected
ion monitoring of m/z 423 and 435 was used for the measurements.
The first step in this procedure is to calibrate the internal standard against a known amount of native
OCDD. This calibration results in a response factor relating the response of the native compound
to the labeled compound. Standard solutions of each were prepared such that 1 μL had 85 pg of native
and 40 pg of labeled OCDD. Injection of 1 μL of this standard gave the selected ion monitoring results
shown in Fig. 31.7(a); the areas of the two peaks are given as values of A in the figure. The response
factor is
(31.1)
In this case, the response factor is (16,581/85 pg) divided by (24,073/40 pg), which is 0.32. This is what
it should be, given equimolar responses of the two compounds and given their difference in isotopic
composition.
The selected ion monitoring data for an unknown sample are shown in Fig. 31.7(b). In this case,
1000 pg of the labeled OCDD was added to 1.8 g (dry weight) of Lake Ontario sediment before extraction.
After extensive cleanup on silica and alumina, two clean GC-MS peaks were obtained with the
areas shown in the figure. The calculation of the final concentration of OCDD in the sediment proceeds
as follows: First, the amount of the internal standard in the sediment is divided by the weight of dry
sediment; in this case, 1000 pg/1.8 g = 560 pg/g. Second, a corrected area of the native OCDD is calculated
by dividing the area of this peak by the response factor; in this case, this corrected area is
37,011/0.32 = 115,660. (Note that these areas have consistent but arbitrary units.) Third, the ratio of the
native and labeled areas is 115,660/12,569 = 9.2. This is the factor by which the concentration of native
OCDD exceeds the labeled compound. Fourth, the concentration of the labeled material is multiplied
by this factor to obtain a final concentration of native OCDD in the sediment. This value is 9.2 ´ 560
pg/g = 5100 pg/g. This measurement was part of a larger study that indicated that the major source of
polychlorinated dibenzo-p-dioxins and dibenzofurans to the atmosphere was the combustion of municipal
or chemical waste rather than coal (11).
A qualitative application has been selected from the work of a colleague in the author’s department
who has been carrying out studies of the electrochemical reduction of phthalide (12); see Fig. 31.8 for
all structures and data. Dimethylformamide was the solvent and tetra-n-butylammonium perchlorate
was the supporting electrolyte. Products derived from the electrolysis were analyzed by GC-MS, and
the gas chromatogram and mass spectra shown in Fig. 31.8 were obtained. The peak at 18.16 min was
due to phthalide, and the peak at 18.34 min was due to n-tetradecane, which had been added in a known
amount as an internal standard for purposes of quantitating the products. The identities of the other two
peaks were not immediately clear.
The mass spectrum of the peak at 15.21 min (see Fig. 31.8, middle) indicates that this compound
has a molecular weight of 185 Da; because this is an odd number, this compound probably has at least
one nitrogen atom. There is a substantial loss of 43 Da to give the ion at m/z 142, and there is also a
major loss of 42 Da to give the ion at m/z 100. These two losses suggest the presence of at least two
C3H7 moieties. Remembering that the supporting electrolyte was tetra-n-butylammonium perchlorate,
it was reasonable to suggest that this peak was tri-n-butylamine. This assignment was verified by comparison
of this mass spectrum and gas chromatographic retention time with those of authentic material.
The structures of the ions at m/z 100, 142, and 185 are suggested on the mass spectrum; however, it is
important to remember that these ion structures are a result of the interpretation of the spectrum and are
not produced by the data system.
The mass spectrum of the peak at 19.40 min (see Fig. 31.8, bottom) indicates that this compound
Response factor
Area423 ¤ pg Native OCDD
Area435 ¤ pg Labeled OCDD = -------------------------------------------------------------------
622 Handbook of Instrumental Techniques for Analytical Chemistry
has a molecular weight of 192 Da. There was a substantial loss of 56 Da to give the ion at m/z 136. The
ion at m/z 91 was probably a tropylium ion (C7H7
+), and this suggested that this molecule was derived
from phthalide. The meaning of the ions at m/z 118 and 119 was not obvious, but the difference between
91 and 119 suggested the presence of a carbonyl group (28 Da) in this molecule. Putting these
ideas together and noting the components of the reaction mixture, it was hypothesized that this compound
was butyl 2-methylbenzoate. Again, the structures of the major ions are suggested on the mass
Figure 31.7 Selected ion monitoring records of m/z 423 (from native octachlorodibenzo-p-dioxin) and m/z 435
(from 37Cl8-octachlorodibenzo-p-dioxin) showing quantitation by the isotopic internal standard method. Only the
gas chromatographic retention time range between 62 and 69 min is shown. The values of A are the areas of the
peaks, in arbitrary units.
Gas Chromatography Mass Spectrometry 623
Figure 31.8 Gas chromatogram of a reaction mixture from the electrochemical reduction of phthalide. The solvent
was dimethylformamide and the supporting electrolyte was tetra-n-butylammonium perchlorate. The two
compounds at 15.21 and 19.40 min were unknown; their mass spectra are shown.
624 Handbook of Instrumental Techniques for Analytical Chemistry
spectrum. The validity of the identification of this GC peak was verified by comparison of the mass
spectrum and gas chromatographic retention time with those of the authentic compound. Apparently,
this compound results from a reaction between an electrogenerated intermediate (radical anion of phthalide)
and the tetra-n-butylammonium cation (of the supporting electrolyte). Moreover, there is reason
to believe that the process leading to butyl 2-methylbenzoate actually occurs in the heated injection
port of the gas chromatograph.
Nuts and Bolts
Relative Costs
Although in principle GC-MS experiments can be performed on magnetic sector instruments, in practice
almost all GC-MS today is done on quadrupole or ion trap instruments. These instruments are relatively
inexpensive and are simple to control by a computer. The major factor influencing the cost of a
quadrupole- or ion-trap–based GC-MS system is the ionization methods available on the instrument
and the mass range of the mass spectrometer. Simple quadrupole or ion trap instruments that use only
electron impact ionization and have a mass range of 20 to 700 cost about $50,000. Those capable of
both positive and negative chemical ionization and with mass ranges of 20 to 2000 cost about $200,000.
Operating costs include instrument maintenance, GC carrier gases and columns, and spare parts. In
most laboratories, these costs are about 5% of the instrument cost per year.
Vendors for Instruments and Accessories
The following list is not exhaustive; several smaller companies enter the field each year and several
leave. The following are some of the larger companies that deal with complete GC-MS systems. See
Chapter 28 (p. 564) for a detailed list of vendors, including addresses for the following vendors.
The Finnigan Corp. (San Jose, CA) sells several instruments, some based on traditional quadrupole
technology, some based on ion trap technology, some based on triple quadrupole technology,
and a few based on magnetic sector technology. Various ionization methods are available.
Micromass UK (Manchester, U.K.) also has a wide range of instruments available with a wide
range of ionization methods. Some are quadrupole based; some are magnetic sector based.
The Hewlett-Packard Corp. (Palo Alto, CA) markets several quadrupole-based instruments ranging
from small benchtop instruments designed for the chromatographer to versatile, stand-alone instruments
that can accommodate both gas and liquid chromatographic inlet systems.
Varian Associates, Inc. (Walnut Creek, CA) sells ion-trap–based GC-MS systems. These are typically
small instruments with a good price-to-performance ratio.
With all of these companies, the recent trend has been to produce smaller and smaller instruments.
Thirty years ago a GC-MS system with its data system occupied a whole room (or even two). Now these
systems fit on the top of a small bench or table. Not only does this trend save space, but it saves manufacturing
costs, some of which are passed on to the instrument purchaser. These smaller instruments
Gas Chromatography Mass Spectrometry 625
also have fewer parts, making them less costly to maintain. There is also a trend toward increasing automation.
Modern instruments are often equipped with an automatic injection system, and once filled
with samples, the data system can control all functions of the instrument including sample introduction.
Thus, once a trained person has developed the methodology and set up the data system, the instrument
will almost run itself.
Required Level of Training
The required level of training and expertise varies as a function of the level of data interpretation. At
the simplest level, because of the computer interface, most GC-MS instruments can be operated by people
with no formal training in mass spectrometry or chemistry. A high school education is often sufficient.
Maintenance of the instrument requires some mechanical and electronic skills, but again no
formal training in mass spectrometry or chemistry is needed. For interpretation of the data, some chemistry
training is needed, particularly organic chemistry. Many graduates of high-quality undergraduate
programs in chemistry and most graduates of graduate programs in analytical or organic chemistry acquire
these skills through their course work. Given a normal undergraduate course sequence in organic
chemistry, most technically trained people can acquire specific training in mass spectrometry through
1- to 2-week courses offered through professional societies (such as the American Chemical Society or
the American Society for Mass Spectrometry).
Service and Maintenance
Unlike most other spectrometers, in which radiation is passed through the sample, with mass spectrometry,
the sample is inserted directly into the instrument. Thus, these instruments require more care than
most others. The analyst should expect to clean the ion source every 2 to 4 mo and change the GC column
every 3 to 6 mo. The instrument is electronically complex but highly modularized; thus, most electronic
failures are corrected by replacement of a printed circuit board. The data systems are relatively
hardy and are furnished with diagnostic software for both the computer and the mass spectrometer.
Downtime for most modern instruments should be less than 5 to 10%, and maintenance costs should be
less than 5% of the instrument cost per year.
Suggested Readings
CHAPMAN, J. R., Practical Organic Mass Spectrometry, 2nd ed. New York: Wiley, 1993.
HITES, RONALD A., Handbook of Mass Spectra Environmental Contaminants, 2nd ed. Boca Raton, FL: Lewis
Publishers, 1992.
KARASEK, FRANCIS W., AND RAY E. CLEMENT, Basic Gas Chromatography–Mass Spectrometry: Principles &
Techniques. Amsterdam: Elsevier, 1988.
MCLAFFERTY, FRED W., Registry of Mass Spectral Data, 5th ed. New York: Wiley, 1989.
MCLAFFERTY, FRED W., Registry of Mass Spectral Data with Structures (CD-ROM), 5th ed. New York: Wiley,
1989.
MCLAFFERTY, FRED W., AND FRANTISEK TURECEK, Interpretation of Mass Spectra, 4th ed. Mill Valley, CA: University
Science Books, 1993.
NATIONAL INSTITUTE OF STANDARDS AND TECHNOLOGY, NIST/EPA/NIH Mass Spectral Library for Windows™
(61.4 megabytes). Gaithersburg, MD: NIST Standard Reference Data, 1995.
626 Handbook of Instrumental Techniques for Analytical Chemistry
WATSON, J. THROCK, Introduction to Mass Spectrometry, 2nd ed. New York: Raven Press, 1985.
References
1. R. S. Gohlke, Analytical Chemistry, 31 (1959), 535–41.
2. J. T. Watson and K. Biemann, Analytical Chemistry, 37 (1965), 844–51.
3. R. Ryhage, Analytical Chemistry, 36 (1964), 759–64.
4. T. E. Jensen and others, Analytical Chemistry, 54 (1982), 2388–90.
5. R. A. Hites and K. Biemann, Analytical Chemistry, 40 (1968), 1217–21.
6. R. A. Hites and K. Biemann, Analytical Chemistry, 42 (1970), 855–60.
7. P. Kintz, A. Tracqui, and P. Mangin, Fresenius Journal of Analytical Chemistry, 339 (1991), 62–3.
8. Fed. Regist., 49 (1984), 43234–439.
9. EPA Method 525.1, Rev 2.2, May 1991; NTIS order numbers PB-89-220461 and PB-91-108266.
10. C. C. Sweely and others, Analytical Chemistry, 38 (1966), 1549–53.
11. J. M. Czuczwa and R. A. Hites, Environmental Science Technology, 20 (1986), 195–200.
12. M. L. Vincent and D. G. Peters, Journal of Electroanalyical Chemistry Interfacial Electrochemistry, 327
(1992), 121–35.

http://www.prenhall.com/settle/chapters/ch31.pdf
http://www.miplaza.com/materialsanalysis/projects/technicalnotesmolecularandstructuralanalysis/hplc.pdf

Tidak ada komentar:

Posting Komentar