more direct approach is to measure concentrations in situ. There
have been relatively few reports of measured atmospheric
abundance of AFCs given the potential impact.17-23 HCFC-22
the solid stationary phase columns tested were apparently capable
of performing adequate separation of volatile AFC compounds.
The purpose of this study is to evaluate the potential for using
the ECD to detect AFCs. The ECD response to the common
AFCs are measured relative to that of CFC-12, which is used as
an internal standard. We also examine the utility of a Poraplot-Q
WPLOT and Carboxen 1004 packed column in the separation of
the AFCs when ECD is used. No attempt was made to enhance
the ECD signals using oxygen doping.28,29 This technique has
been shown to increase detection limits for some AFC com-
pounds.24 On the hand, ECD response is known to be affected
by detector temperature. We perform a temperature-dependent
response study. The temperature-dependent response results
allows deduction of the electron capture mechanism and molecular
ion thermodynamics.
(
CHF
2
Cl), a refrigerant, has been in use the longest and has
received the most attention.1
7-20
3 2
HCFC-142b (CH CFCl ), used
since 1988 as a foam blowing agent and a solvent, has also been
measured.17,21,22 Atmospheric concentration trends for the popular
refrigerant HFC-134a (CF CH
3 2
F) have recently been reported.23
For the most part, these reports indicate higher than expected
concentrations.
With the exception of a single passive infrared absorption
report,19 AFC compounds have been detected using gas chroma-
tography with mass spectrometry (GC/ MS) operating in mass-
selective detection mode. Air samples are collected in either
stainless steel or aluminum cylinders and stored for later labora-
tory analysis. Analysis samples are concentrated prior to GC/
MS analysis. Detection requires preconcentration of nearly 1 L
of whole-air sample. Preconcentration has been performed using
cryogenic trapping techniques. There are problems with this
method such as supplying the liquid nitrogen, the cost, and the
band broadening that occurs when large volumes of sample are
desorbed and introduced into the column. Several researchers
EXPERIMENTAL SECTION
Apparatus. A Hewlett-Packard Model 5890a gas chromato-
62
graph equipped with both a Model G1223A Ni â source, electron
capture detector (ECD) and a Model 19231D/ E flame ionization
detector (FID) is used in this study. The ECD is a potentially
hazardous radioactive source and a semiannual wipe test is
required to assess its stability. The ECD and FID are used at
temperatures of 300 and 250 °C, respectively, except for the ECD
temperature-dependent response study described below. The
ECD makeup flow rate is 20 mL min- nitrogen. Gas samples
are introduced either by direct injection using the standard
splitless injector or by volumetric injection using a Valco, T series,
six-port valve with a 10 µL volume injection loop. The direct
injector is maintained at 200 °C for all experiments. The six-port
injection valve is mounted in the gas chromatograph oven.
Ultrapure nitrogen (Whitmore Oxygen) is used as the carrier and
make-up gas. Oxygen trap (Oxy-trap Alltech) and a molecular
sieve 40/ 50 mesh (Hewlett-Packard) are used to purify the gas
supply. Carrier and make-up gas flow rate are measured with
the Hewlett-Packard electronic flow sensing.
have reported the use of “microtraps” with carbonaceous adsor-
bents to address these problems.2
4-26
Simmonds et al.26 reported
on an automated GC/ MS instrument for field measurements using
both glass bead and carbonaceous adsorbent “microtraps” to
concentrate the AFC compounds. Since selective-ion monitoring
was not used, several liters of air are required for concentration
prior to GC/ MS analysis. Problems with this method are that
large numbers of potential interferents have to accounted for in
the MS data analysis and that the large sample volumes are subject
to problems associated with the use of adsorbent traps. The large
size of the instrument and the requirement for liquid nitrogen
prevent use of this method for true field measurements.
Sturges and Elkins24 reported on the use of electron capture
detection (ECD) with ambient temperature traps for preconcen-
tration. This method has potential for field monitoring due to
the relatively small size, the cost, and no need for cryogenics.
Speciation would have to be totally accomplished with chroma-
tography, though some selectivity may be attained with the ECD.
Sturrock et al.27 have evaluated several wide-bore capillary columns
for use in AFC analysis. Although no single column was perfect,
1
Separations are performed using two columns. The first is a
3
0 m, 0.53 mm internal diameter WPLOT Poraplot Q (J&W
Scientific, CA) column. The stationary phase of the Poraplot Q
is a styrene-divinylbenzene copolymer similar in characteristics
to the Porapak phase used in packed columns. The second
column is a Carboxen 1004 packed column (Supelco). This
stainless steel column has a length of 2 m, with 0.75 mm internal
diameter. Carrier flow rates are experimentally derived using a
Van Deemter plot of data obtained under isothermal conditions.
(
(
(
17) Pollock, W. H.; Heidt, L. E.; Lueb, R. A.; Vedder, J. F.; Mills, M. J.; Solomon,
S. J. Geophys. Res. 1 9 9 2 , 97, 12993-12999.
18) Montzka, S. A.; Myers, R. C.; Butler, J. H.; Elkins, J. W.; Cummings, S. O.
Geophys. Res. Lett. 1 9 9 3 , 20, 703-706.
19) Risland, C. P.; Goldman, A.; Murcray, F. J.; Blatherwick, R. D.; Kosters, J.
J.; Murcray, D. G.; Sze, N. D.; Massie, S. T. J. Geophys. Res. 1 9 9 3 , 95,
The carrier flow rates used in this study are 5.6 mL min- for the
1
Poraplot Q column and 9.6 mL min-1 for the Carboxen 1004
column. These carrier flow rates are used for isothermal condi-
tions and for the starting temperature with temperature program
conditions. Separation of the compounds tested could be achieved
isothermally and with temperature programming on the Poraplot
Q column. In order to achieve the separation of HFC-125, HCFC-
1
6477-16490.
20) Irion, F. W.; Brown, M.; Toon, G. C.; Gunson, M. R. Geophys. Res. Lett. 1994,
1, 1723-1726.
(
(
2
21) Schauffer, S. M.; Heidt, L. E.; Pollock, W. H.; Gilpin, T. M.; Vedder, J. F.;
Solomon, S.; Lueb, R. A.; Atlas, E. L. Geophys. Res. Lett. 1 9 9 3 , 20, 2567-
2
570.
22) Montzka, S. A.; Myers, R. C.; Butler, J. H.; Elkins, J. W. Geophys. Res. Lett.
9 9 4 , 21, 2483-2486.
2
2, and HCFC-124, on the Carboxen 1004 column, a temperature
(
(
program is used: 80 (1 min) and then 20 °C min- ramp to the
final 220 °C. Resolution was still poor in this case. Analysis time
was ∼12 min with the temperature program. Quantitative detector
response and retention time data are obtained using 200 °C
isothermal conditions by injecting each AFC compound in a
mixture with CFC-12.
1
1
23) Montzka, S. A.; Myers, R. C.; Butler, J. H.; Elkins, J. W.; Lock, L. T.; Clarke,
A. D.; Goldstein, A. H. Geophys. Res. Lett. 1 9 9 6 , 31, 169-172.
(
(
24) Sturges, W. T.; Elkins, J. W. J. Chromatogr. 1 9 9 3 , 642, 123-134.
25) O’Doherty, S. J.; Simmonds, P. G.; Nickless, G. J. Chromatogr. A 1 9 9 3 ,
6
57, 123-129.
(
(
26) Simmonds, P. G.; O’Doherty, S.; Nickless, G.; Swaby, R. A.; Knight, P.;
Ricketts, J.; Woffendin, G.; Smith, R. Anal. Chem. 1 9 9 5 , 67, 717-723.
27) Sturrock, G. A.; Simmonds, P. G.; Nickless, G. J. Chromatogr. A 1 9 9 3 , 648,
(28) Grimsrud, E. P.; Miller, D. A. Anal. Chem. 1 9 7 8 , 50, 1141-1145.
(29) Miller, D. A.; Grimsrud, E. P. Anal. Chem. 1 9 7 9 , 51, 851-859.
4
23-431.
3872 Analytical Chemistry, Vol. 69, No. 19, October 1, 1997