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Atmospheric Environment 38 (2004) 557–572
ARTICLE IN PRESS
*Correspond
303-492-6388.
E-mail addr
(D. Helmig).
1352-2310/$ - se
doi:10.1016/j.at
Analytical techniques for sesquiterpene emission rate studiesin vegetation enclosure experiments
Detlev Helmig*, Florence Bocquet, Jan Pollmann, Tobias Revermann
Institute of Arctic and Alpine Research (INSTAAR) University of Colorado, Campus Box 215, Boulder, CO 80309-0450, USA
Received 8 July 2003; accepted 3 October 2003
Abstract
Sesquiterpene (SQT) compounds (C15H24) and their oxygenated alcohol and ketone derivatives are biogenic volatile
organic compounds that have been identified in emissions from vegetation. SQT emission rates and landscape flux
estimates are highly uncertain. Reliable ambient flux measurements have not been possible because of low-ambient
concentrations, rapid atmospheric reactions (prohibiting ambient tower flux measurements), and analytical challenges
and uncertainties that stem from the low volatility of SQT. Standards from an in situ capillary diffusion system with 18
SQT compounds and four other organic compounds (geranylacetone, 1,3,5-tri-isopropylbenzene, diphenylmethane,
nonylbenzene) were used to thoroughly investigate experimental procedures for SQT emission rate studies by vegetation
enclosure techniques. Recovery rates in tubing materials, sampling bags, leaf cuvettes, on six solid adsorbent materials
(Tenax TA, Tenax GR, Carbotrap, Carbotrap C, Unibeads, Glass Beads) for gas chromatography analysis, and gas
chromatography retention indices and mass spectral fragmentation patterns were determined. SQT compounds were
found to exhibit a high degree of stickiness to all materials tested. However, the non-oxygenated SQT can be recovered
in enclosure experiments for quantitative emission rate determination after careful consideration of the analytical
conditions. It is utmost important to allow sufficient purging and equilibration times for all materials in contact with
the sample air. In contrast oxygenated SQT were irreversibly lost in enclosure experiments which made their
quantitative measurement prohibitive. Results for the other organic compounds were similar and indicate that these
data mostly stem from the volatility of these compounds. Consequently, the findings of this study provide guidelines for
the analysis of a wide range of volatile organic compounds in the BC13–C17 volatility range.
r 2003 Elsevier Ltd. All rights reserved.
Keywords: Semi-volatile organic compounds; Sesquiterpenes; Emissions from vegetation; Enclosure experiments; Solid adsorbent
sampling; Gas chromatography
1. Introduction
Sesquiterpene hydrocarbons (C15H24, SQT) and some
oxygenated alcohol, aldehyde, and ketone analogous
derivatives (C15H22O, C15H24O, C15H26O) have been
identified in studies on biogenic volatile organic
compound (BVOC) emissions from both natural and
ing author. Tel.: +1-303-492-2509; fax: +1-
ess: [email protected]
e front matter r 2003 Elsevier Ltd. All rights reserve
mosenv.2003.10.012
agricultural vegetation (Buttery et al., 1985; Bicchi et al.,
1989; Omata et al., 1990; Winer et al., 1992; K .onig et al.,
1995; Rudolph et al., 1997; Schuh et al., 1997; Llusia
and Penuelas, 1998; Zhang et al., 1999; Hansen and
Seufert, 1994; Ciccioli et al., 1999; Bartelt and Wicklow,
1999; Helmig et al., 1999a; Kim et al., 2000; Agelopou-
los et al., 2000; Hakola et al., 2001). A few preliminary
studies indicate that SQT landscape fluxes may be
significant (Ciccioli et al., 1999; Helmig et al., 1999b),
possibly contributing to up to 16% of the overall carbon
BVOC landscape flux (Helmig et al., 1999b). Because of
their rapid atmospheric reactions (Grosjean et al., 1993;
d.
ARTICLE IN PRESSD. Helmig et al. / Atmospheric Environment 38 (2004) 557–572558
Shu and Atkinson, 1994, 1995; Hoffmann et al., 1997)
and high aerosol yields (Hoffmann et al., 1997) SQT are
suspected to contribute to secondary aerosol formation.
Biogenic precursor compounds have long been specu-
lated to play an important role in atmospheric aerosol
formation (Went, 1960; Schuetzle and Rasmussen, 1978;
Yokouchi and Ambe, 1985; Mlot, 1995), but their
quantitative contribution remains highly uncertain.
SQT have also garnered interest in research on
chemically mediated plant–insect interactions. The
motivation for this research is the development of
ecological and environmentally safe methods for agri-
cultural pest control. Experiments on corn and tobacco
have demonstrated that these plants respond to envir-
onmental stress, in particular to herbivore attack by
synthesizing and releasing a variety of terpenoid
compounds including SQT (Alborn et al., 1997; Pare
and Tumlinson, 1997a, b, 1999; Halitschke et al., 2000;
Degenhardt and Gershenzon, 2000; De Moraes et al.,
2001; Pichersky and Gershenzon, 2002; Gouinguen!e and
Turlings, 2002). These volatile emissions have been
found to be a defense and communication mechanism of
injured plants. For instance, in experiments on corn
seedlings it was shown that volatile BVOC including
SQT attract wasps that attack caterpillars feeding on the
corn (Turlings and Tumlinson, 1992; Turlings et al.,
1995).
Only a few quantitative emission studies have been
attempted. Substantial uncertainties in SQT emission
rates arise from the lack of defined analytical techniques
for SQT identification and from SQT losses in enclosure
experiments or in eddy correlation flux studies. These
uncertainties stem from the semi-volatile nature of SQT.
With molecular weights in the range of 204–222 gmol�1,
these compounds are too low in volatility for samples
and standards to be stored and quantitatively recovered
from storage containers such as compressed air gas
cylinders and gas sampling flasks or canisters. An
alternative approach for standard generation by capil-
lary diffusion has recently been reported to yield reliable
SQT standards for analytical testing (Komenda et al.,
2001; Helmig et al., 2003).
Landscape fluxes of other, lighter BVOC have
preferably been investigated by ambient flux measure-
ment techniques from tower platforms, tethered bal-
loons or research aircraft. Experimental approaches
include eddy correlation, tower gradient, mixed layer
gradient or mixed layer budget methods (Guenther et al.,
1996a, b; Fuentes et al., 2000). These techniques have
successfully been used for isoprene, monoterpenes and
several other oxygenated BVOC. A requirement for the
applicability of these methods is that mixing ratios in
turbulent eddies (resulting in vertical gradients) are due
to the transport from the source (canopy) to the
atmosphere above rather than from atmospheric deple-
tion by chemical reactions. These conditions are
generally met for the listed BVOC. These BVOC have
atmospheric lifetimes on the order of 1 h, which are long
compared to the scale of atmospheric mixing and
transport in the planetary boundary layer.
SQT are more reactive than isoprene and mono-
terpenes. SQT atmospheric lifetimes from their reactions
with ozone, and the OH and NO3 radicals have been
estimated to be only a few minutes (Grosjean et al.,
1993; Shu and Atkinson, 1994, 1995; Hoffmann et al.,
1997). Consequently, significant depletion by atmo-
spheric reactions is expected within the immediate
vicinity of the source. Because of the substantial SQT
losses within the plant canopy, above-canopy flux
measurements are deemed to underestimate the overall
biosphere SQT flux. The fate of the emitted SQT is
somewhat uncertain at this time, but it appears likely
that a portion of the SQT products is trapped within the
plant canopy and that another portion of SQT escapes
the canopy as gas-phase reaction products, or in organic
aerosols. In one particular case, this speculation has
been experimentally proven: Ciccioli et al. (1999) found
that relaxed eddy correlation fluxes of b-caryophylleneover an orange orchard were only B1
6of the estimates
that were derived from scaled-up enclosure measure-
ments.
Consequently, SQT emission rates are best deter-
mined by enclosure techniques, such as with leaf cuvettes
or branch bag enclosures. While the artificial conditions
imposed during enclosure experiments are a valid
concern, precise light and temperature control has been
shown to yield valuable BVOC emission data (Guenther
et al., 1996a, b; Ciccioli et al., 1999; Fuentes et al., 2000).
Furthermore, enclosure studies are particularly advan-
tageous for SQT emission rate studies because oxidant
levels (e.g. OH, O3) are low and residence times of SQT
in air can be kept in the second to minute range. This
approach eliminates the difficulties associated with the
ambient level measurements (see above).
Preconcentration on solid adsorbents followed by
thermal desorption and GC analysis has become a well-
accepted VOC analysis technique in a wide range of
applications. Most techniques described in the literature
are for compounds in the C5–C10 volatility range. This
range has been extended occasionally to more volatile
C2–C4 VOC (Helmig, 1999) using stronger (higher
surface area) adsorbents. In contrast, the applicability of
adsorbent sampling/thermal desorption for heavier
(>C10) and semi-volatile VOC has received little
attention. Consequently, very little research has been
presented that can be applied to SQT analysis. In
particular, data on SQT thermal stability, breakthrough
on solid adsorbents, recovery rates from adsorbents and
potential losses to surfaces are needed to facilitate SQT
analysis in enclosure experiments.
In this research six different adsorbent materials were
tested for analysis of SQT in air samples. Furthermore,
ARTICLE IN PRESSD. Helmig et al. / Atmospheric Environment 38 (2004) 557–572 559
experimental systems, such as an automated cartridge
sampler, tubing materials, Teflon bags, and leaf cuvettes,
which typically are used for sampling of BVOC in
vegetation emission studies, were investigated for their
retention of SQT. Four non-SQT semi-volatile VOC
were included in these experiments in order to investi-
gate if findings were SQT specific or generally applicable
to VOC in the C13–C17 volatility range.
2. Experimental
2.1. Analytes
Compounds included in this study were 11 commer-
cially available SQT hydrocarbons, two SQT ketones/
oxides and five SQT alcohols. Furthermore, geranyla-
cetone, another frequently identified BVOC emission
and three aromatic VOC (1,3,5-tri-isopropylbenzene,
diphenylmethane, nonylbenzene), were investigated for
comparison with SQT. Physicochemical parameters and
suppliers of all of the standards have been given
previously (Helmig et al., 2003).
2.2. Capillary diffusion system
SQT standards were generated using a 10-channel
capillary diffusion system (CDS). This instrument has
recently been described in detail (Helmig et al., 2003), so
only a brief summary is given here. SQT gas standards
are prepared by diffusion of SQT from a liquid reservoir
into a nitrogen gas flow. Diffusion rates are controlled
by proper selection of length and diameter of glass
capillary resistors and by temperature. Diffusion rates of
SQT were quantified with a median B5–6% precision
and B10% accuracy by the gravimetric weight loss of
the SQT reservoirs as well as by a quantitative on-line
GC-flame ionization detection (FID) method. Agree-
ment between these independent methods generally was
>90%. The CDS allows investigating individual as well
Table 1
Properties of solid adsorbent materials and filling weight of adsorben
Adsorbent Filling
weight (g)
Conditioning
temperature (�C)
Maximum
temperature (�
Tenax TA 0.25 330 350
Tenax GR 0.25 330 350
Carbotrap 0.40 330 400
Carbotrap C 0.30 350 350
Unibeads 0.30 300 n/a
Glass Beads
DMCS treatded
1.00 300 n/a
aLiterature and suppliers information.
as mixtures of SQT. With an integrated dilution system,
the output mixing ratios can be varied between
B100 pptv (parts-per-trillion volume) to 2000 ppbv
(parts-per-billion volume). Potential analytical interfer-
ences from water vapor and ozone can be simulated by
adding either of these two gases. For the experiments
described in this research, the output mixing ratios of
individual channels were isopropylbenzene 718 ppbv,
longipinene 1020 ppbv, a-copaene 528 ppbv, isolongifo-
lene 879 ppbv, d-neoclovene 727 ppbv, longifolene
592 ppbv, diphenylmethane 416 ppbv, isocaryophyllene
785 ppbv, cedrene 555 ppbv, caryophyllene 1690 ppbv,
aromadendrene 560 ppbv, humulene 417 ppbv, gerany-
lacetone 938 ppbv, cis-nerolidol 126 ppbv, caryophyllene
oxide 247 ppbv, trans-nerolidol 136 ppbv, nonylbenzene
444 ppbv, cedrol 241 ppbv, isolongifolen-9-one
390 ppbv, bisabolol 63 ppbv and farnesol 10 ppbv. By
combining all ten channels, the above mixing ratios are
diluted by a factor of B10. For a second dilution step, a
fraction of the combined output was split off and mixed
with scrubbed zero air. This resulted in an overall
dilution factor of B420 (for humidity and recovery
experiments) and B800 (for linearity tests).
2.3. Adsorbent cartridges
Four common solid adsorbents as well as two
activated glass materials (Unibeads and dimethyldi-
chlorosilane-treated Glass Beads) were tested for analyte
collection and enrichment. All of these adsorbents
have previously been characterized as relatively ‘weak’
(i.e. low surface area) materials and were therefore
expected to be suitable for the sampling of the semi-
volatile SQT with thermal desorption analysis. The
adsorbents, their properties and sources are given in
Table 1. Adsorbent tubes were prepared from borosili-
cate glass tubing (0.63 cm o.d., 0.36 cm i.d., Wale
Apparatus, Hellertown, PA), which was cut to 9 cm
long pieces. Tubes were cleaned by sonicating in
methanol, marked with heat resistant labels and baked
t cartridges used in this study
C)
Mesh size Surface area
(m2/g)aVendor
60/80 35 Alltech, Deerfield, II
20/35 24 Alltech, Deerfield, II
20/40 100 Supelco, Bellefonte, PA
20/40 10 Supeteo, Bellefonte, PA
60/80 n/a Alltech, Deerfield, II
60/80 n/a Alltech, Deerfield, II
ARTICLE IN PRESSD. Helmig et al. / Atmospheric Environment 38 (2004) 557–572560
at 600�C for 20min prior to filling. Glass tubes were
filled for a total length of 6 cm with the respective
adsorbent material (see Table 1 for adsorbent weights).
The adsorbent was held in place by glass wool plugs on
both sides, a spring made of 3 cm nickel wire (>99.99%
purity, Sigma-Aldrich, Milwaukee, WI) on the sampling
(inlet) side and a stainless steel spring on the other side.
Adsorbent cartridges were conditioned by heating and
purging with purified nitrogen (ultra-high purity grade,
Airgas, Denver, CO) at a flow rate of 70–80mlmin�1 for
120min. The nitrogen purge gas was further purified by
a hydrocarbon scrubber (N930-1192, Perkin-Elmer,
Shelton, CT) and an oxygen trap (Oxytrap, Alltech,
Deerfield, IL). Cartridge bakeout temperatures are
included in Table 1.
2.4. Adsorbent cartridge sampling
A custom-made automated sampler (Fig. 1) was
used for the consecutive sampling of up to 10 cartridges
under temperature and flow controlled conditions. The
principal sampler components are one 0.32 cm two-
position four-port valve and one 0.32 cm multiposition
ten-port valve (VICI, Houston, TX). All tubing
and valve components can be continuously purged
prior to and between the switching of adsorbent
cartridges into the flow path for sample collection. All
tubing was made of 3.2mm o.d. Silicosteel (Restek,
Bellefonte, PA). Valves and all tubing were maintained
at 50�C, adsorbent tubes were kept at room temperature
(25�C) during sampling. A 90 cm long 0.32 cm o.d.
Teflon (PTFE) sampling line from the cartridge
sampler to the outlet of the SQT capillary diffusion
system was also heated to 50�C. The sampler is
computer controlled by a custom program written in
Basic which allows any desired variation of purging and
sampling times.
Fig. 1. Schematic of the automated solid adsorbent cartridge sample
valve) as well as all tubing were heated to 50�C.
2.5. GC analysis
Adsorbent cartridges were analyzed with a Perkin-
Elmer ATD-400 automated cartridge desorber and a
Perkin-Elmer AutoSystem XL GC/FID instrument. The
following ATD 400-parameter were used: He purge flow
37mlmin�1, primary desorption temperature 325�C,
primary desorption time 12.5min, second stage trap
temperature during primary desorption: �22�C, second
stage trap desorption temperature 350�C, hold time
5min. The second stage trap was filled with Unibeads.
Outlet split flow during the second stage desorption was
7.7mlmin�1. Adsorbent cartridges were backflushed
during thermal desorption. GC parameters were as
follows: FID hydrogen 60mlmin�1, FID air
350mlmin�1, He carrier gas flow 2.5mlmin�1; GC
oven program: 40�C for 5min, 20�Cmin�1 to 100�C,
2�Cmin�1 to 160�C, 40�Cmin�1 to 250�C, final time
5min. GC column details are given in Table 2.
2.6. GC-MS/FID
A GC/MS (Hewlett-Packard 5890/5970) with addi-
tional FID detector was used for compound identifica-
tion and additional quantitative experiments. This
instrument was equipped with a custom-made inlet
system (2-position 6-port valve [VICI]) for thermal
desorption. First, cartridges were purged at ambient
temperature with He in the sampling flow direction to
remove water and air for 5min at 30mlmin�1. For
thermal desorption, the flow direction was reversed and
cartridges were backflushed directly onto the GC
column as they were heated to 325�C over 3min. He
desorption flow was 7mlmin�1. The switching valve and
transfer line (0.16mm o.d. Silicosteel) were heated to
150oC. The GC column was kept at 40�C during
the desorption step. Under these conditions SQT are
r. All valves (2-position 4-port valve and 10-position sampling
ARTIC
LEIN
PRES
S
Table 2
Sesquiterpene retention indices on three GC systems and mass spectral fragmentation
Retention-index
Compound GC-type: On-line GC-FID PE GC-FID HP-GC-FID/MS Mass fragments from HP-GC-FID/MS m/z (% abundance)
Column: DB-1 DB-1 CPSIL5CB
Inner diameter: 0.320mm 0.320mm 0.320mm
Length: 30m 30m 60m
Film-thickness: 0.1 mm 0.25mm 0.25mmManufacturer: J. & W. Scientific J. & W. Scientific Chrompack
n-Tridecane 1300.0 1300.0 1300.0
1,3,5-Tri-isopropylbenzene 1322.670.2 1322.870.9 1324.370.6 189 (100); 161 (58); 91 (36); 204 (26); 105 (25), 190 (15)
a-Longipinene 1326.670.3 1338.670.5 1348.870.9 119 (100); 93 (41); 91 (40); 133 (37); 92 (22); 120 (20)
a-Copaene 1354.070.2 1363.570.7 1375.770.8 161 (100); 119 (99); 105 (88); 159 (57); 93 (47); 91 (41)
Isolongifolene 1357.970.1 1372.871.0 1390.071.0 161 (100); 133 (49); 148 (49); 175 (45); 119 (38); 204 (21)
d–Neoclovene 1370.970.3 1389.670.8 1406.270.5 105 (100); 120 (96); 119 (93); 121 (72); 91 (68); 107 (63)
Longifolene 1373.970.5 1389.670.8 1406.370.5 91 (100); 94 (88); 93 (83); 161 (83); 107 (80); 79 (69)
Diphenylmethane 1380.170.2 1389.670.8 1403.970.5 167 (100); 169 (100); 165 (37); 152 (25); 153 (23)
Isocaryophyllene 1380.670.2 1389.670.8 1405.370.5 93 (100); 91(84); 69 (82); 79 (78); 133 (63); 105 (51)
a-Cedrene 1383.170.2 1396.970.7 1413.070.6 119 (100); 93 (46); 105 (32); 91 (30); 77 (23); 92 (18)
b–Caryophyllene 1391.870.2 1404.370.2 1417.170.9 69 (100); 93 (100); 91 (87); 79 (84); 133 (72); 105 (53)
n-Tetradecane 1400.0 1400.0 1400.0
Aromadendrene 1410.070.1 1423.770.2 1435.970.7 91 (100); 93 (91); 105 (87); 79 (86); 107 (81); 161 (75)
a-Humulene 1421.870.1 1433.170.4 1448.070.8 93 (100); 80 (36); 121 (25); 91 (23); 92 (23); 147 (14)
Geranylacetone 1423.070.1 1421.570.7 1427.170.8 69 (100); 107 (28); 151 (23); 67 (22); 136 (20); 93 (16)
n-Pentadecane 1500.0 1500.0 1500.0 161 (100); 119 (55); 134 (54); 204 (51); 105 (39); 91 (25)
d-Cadinene 1478270.1 n.a. 1507.170.8
cis-Nerolidol 1510.470.1 1512.270.1 1516.170.6 69 (100); 93 (61); 55 (37); 107 (29); 81 (28); 79 (18)
Caryophyllene Oxide 1534.170.1 n.a. n.a. 79 (100); 93 (80); 55 (75); 81 (72); 107 (72); 95 (63)
trans-Nerolidol 1538.57 0.1 1541.370.5 1545.270.7 69 (100); 93 (54); 107 (34); 71 (34); 55 (32); 70 (24)
Nonylbenzene 1542.870.1 1547.770.4 1554.170.8 92 (100); 91 (81); 204 (14); 133 (6); 71 (6)
Cedrol 1548.17 0.3 1561.870.2 1583.070.8 95 (100); 150 (86); 151 (64); 81 (37); 135 (31); 93 (28)
n-Hexadecane 1600.0 1600.0 1600.0
lsolongifolen-9-one 1627.970.1 1645.070.8 1663.970.9 175 (100); 147 (78); 162 (75); 176 (49); 119 (42); 218 (42)
Bisabolola 1646.470.3 1658.572.1 n.a. n.a.
Bisabololb 1649.070.2 n.a. n.a. n.a.
n-Heptadecane 1700.0 1700.0 1700.0
Farnesol 1775.970.2 n.a. n.a. n.a.
a,bTwo unidentified isomers.
D.
Helm
iget
al.
/A
tmo
sph
ericE
nviro
nm
ent
38
(2
00
4)
55
7–
57
2561
ARTICLE IN PRESSD. Helmig et al. / Atmospheric Environment 38 (2004) 557–572562
pre-focused on the column head. The final desorption
time was 12.5min. Then, the injection valve was
switched back and the GC carrier gas flow was reduced
to 1.7mlmin�1 for GC analysis. The column flow was
split and directed to two detectors. The minor fraction
(30%) eluted into the MS for compound identification,
the remaining 70% were directed to the FID for
quantitative analysis. The GC column is described in
Table 2. The FID flow rates were 60mlmin�1 H2 and
350mlmin�1 air. The GC oven temperature program
was: initial temperature 40�C held for 1min, 25�Cmin�1
to 120�C; 2�Cmin�1 to 190�C; 25�Cmin�1 to 250�C;
250�C held for 5min.
3. Experiments and results
3.1. Compound identification
Analytes were identified by their mass spectral
fragmentation (MS) and linear programmed GC reten-
tion indices (RI) (Van den Dool and Kratz, 1963). MS
fragmentation data (determined by averaging of 4–6
scans around the GC peak maximum) and RI on two
stationary phases (three GC columns total) are sum-
marized in Table 2. When using the relatively unpolar
methylsilicone column phases, hydrocarbon SQT
(C15H24) RI lie within the range of 1325–1500, and the
more polar and less volatile SQT ketones and alcohols
elute between RI B1525–1775. Several pairs of analytes
0
20
40
60
80
100
120
140
160
1300 1350 1400 1450 15
Retentio
Rec
ove
ry (
%)
Fig. 2. Recovery of analytes during sampling with the automated car
the outlet of the CDS. The compound recovery is plotted against the
means from 3 parallel sampling experiments; error bars represent
individual standard deviation of the direct sampling and the sampler
were co-eluting on these GC columns (e.g. diphenyl-
methane and longifolene, aromadendrene and gerany-
lacetone) and consequently experimental results are
reported for the total of these two analytes combined,
or one of the co-eluting analytes was excluded from
experiments, respectively.
3.2. Automated sampler testing
Potential losses of SQT in the automated cartridge
sampler were investigated by parallel sampling. Two
adsorbent-cartridges (Tenax TA) were loaded under the
exact same sampling time and flow rate (10min at
206.8mlmin�1 (all flows reported are converted to
standard pressure and temperature, STP)) at a 1:420
dilution (B0.19–3.76 ppbv SQT). One cartridge was
loaded directly at the diffusion system outlet and the
second cartridge was loaded by sampling the standard
from the same outlet through the sampling line with the
cartridge sampler (Fig. 1). The sampling line and
switching valve of the sampler were purged for a
minimum of 10min before the first sample was loaded.
The recovery rates for the SQT are within the range of
90–110% (Fig. 2). However, with increasing RI (lower
volatility) the deviations from 100% as well as the
relative standard deviations increase significantly. Re-
sults for the oxygenated SQT (higher RI (Table 2)) are
worse than for the hydrocarbon SQT. Higher tempera-
tures for the sampler components may help to improve
upon the data for the less volatile compounds, but
00 1550 1600 1650 1700
n Index
tridge sampler in comparison with direct sample collection from
analyte DB-1 retention index (Table 2). Recovery rates are the
the standard deviation ðn ¼ 5Þ and were calculated from the
data by error propagation.
ARTICLE IN PRESSD. Helmig et al. / Atmospheric Environment 38 (2004) 557–572 563
unfortunately 50�C was the temperature limit of several
components that were part of our sampler. It should
also be noted that these results reflect the total sampling
plus analysis precision and that a significant contribu-
tion to the error arises from the GC analysis step (see
adsorbent testing results below). These data demon-
strated that SQT losses in the sampler were not
significant and the sampler was subsequently used in
the experiments described in the following.
3.3. Adsorbent testing–recovery ratio
The recovery ratios from the six adsorbents were
determined in two experiments. First, samples were
collected at high concentration and low sampling volume
(1min sample collection, flow rate 108mlmin�1; dilution
factor 1:10; SQT mixing ratio between B1–160 ppbv).
For the second experiment, the SQT standard was
diluted and cartridges were loaded for 10min (dilution
factor 1:420, flow rate 206.8mlmin�1; SQT mixing ratio
between 0.19–3.76 ppbv). Desorption efficiency was
determined by performing repeated desorptions on each
adsorption tube. Desorption temperature was 325�C in
all cases. This temperature may be higher than required
for some of the adsorbent materials, but was found to
overall give the best results. During the adsorption step
cartridges are continuously purged and gradually heated
up from room temperature. Consequently, SQT will be
desorbed and purged off the adsorbent bed when their
respective desorption temperature is reached, which may
Table 3
Results of second desorption experiments at 100ml and 2.11 samplin
Tenax TA Tenax GR
Compound 100ml 2.1 l 100ml 2.1 l
Isopropylbenzene >99.9 >99.9 >99.9 >99.6
Longipinene >99.9 >99.9 >99.9 99.2
a-Copaene >99.9 >99.9 >99.9 >99.4
Isotongifolene >99.9 >99.9 >99.9 >99.6
Diphenylmethane + Longifoleneb >99.9 >99.9 >99.9 >99.7
a-Cedrene >99.9 >99.9 >99.9 >99.4
Caryophyllene >99.9 >99.9 >99.9 >99.8
Geranylacetone >99.9 >99.9 >99.9 >99.3
Aromadendrene >99.9 >99.9 >99.9 99.6
a-Humulene >99.9 >99.8 >99.9 >99.1
cis-Nerolidol >99.8 >99.6 >99.5 >97.9
trans-Nerolidol >99.8 98.0 >99.7 >98.6
Nonylbenzene+Caryophyllene-Oxideb >99.9 99.8 >99.9 >99.6
Cedrol >99.9 >99.8 >99.8 >98.9
lsotongifolen-9-one >99.9 97.7 >99.8 >98.7
Bisabolol >99.8 >99.2 >99.6 >99.1
Data are the percentage of analytes that were recovered in the first des
step under the analytical conditions described in the experimental secaBreakthrough.bCoeluting peaks.
be at substantially lower temperatures than the final
desorption temperature of 325oC. After the first
desorption, the cartridge was sealed and cooled down
to ambient temperature and was then desorbed again
directly under the same conditions. The analytes should
ideally be desorbed completely during the first deso-
rption step. The amounts recovered in the first
desorption as a percentage of the total recovered
amount (all desorptions combined) are displayed in
Table 3. Most of the data for the 108ml volume samples
demonstrate a quantitative desorption of >99% for all
tested adsorbent types during the first desorption step.
For the larger 2.1 l volume samples, the desorption
efficiency decreases somewhat, but in most cases is still
within B99%. The relatively lower recoveries for the
higher sampling volumes may also reflect a (partial)
adsorption/desorption on the glass wool plug in contrast
to the further (deeper) transport of the analytes into the
adsorbent bed at higher sampling volumes. The amounts
of analytes retrieved from the 2.1 l samples collected on
Glass Beads were substantially diminished. Therefore, a
series of breakthrough experiments was conducted with
increasing sampling volumes. A Tenax TA cartridge was
used as a backup of the primary Glass Bead cartridge.
These experiments confirmed that these results stem
from breakthrough that occurs at sampling volumes in
excess of a few hundred ml. Because of these low
breakthrough volumes, Glass Beads were deemed to be
unsuitable under typical experimental conditions and
were excluded from subsequent experiments.
g volume
Carbotrap Carbotrap C Unibeads Glass Beads
100ml 2.1 l 100ml 2.1 l 100ml 2.1 l 100ml 2.1 l
>99.9 86.5 >99.9 >99.9 >99.9 >99.8 >99.9 b.ta
>99.9 99.1 >99.9 97.5 >99.9 >99.8 >99.8 b.t
>99.9 >99.6 >99.9 >99.9 >99.9 >99.8 >99.8 b.t
>99.9 >97.4 >99.9 >99.9 >99.9 >99.9 >99.8 b.t
>99.9 93.7 >99.9 98.7 >99.9 >99.9 >99.9 b.t
>99.9 94.9 >99.9 >99.9 >99.9 >99.9 >99.8 b.t
>99.9 >99.9 >99.9 >99.9 >99.9 >99.9 >99.9 b.t
>99.9 >99.6 >99.9 >99.9 >99.9 >99.9 >99.9 b.t
>99.9 97.7 >99.9 >99.9 >99.9 >99.9 >99.9 b.t
>99.9 >99.6 >99.8 >99.8 >99.9 >99.9 >99.9 b.t
>99.6 >98.6 >99.4 >99.5 >99.8 >99.9 >99.9 b.t
>99.7 >99.1 >99.6 >99.7 >99.9 >99.9 >99.9 b.t
>99.9 >99.8 >99.9 >99.9 >99.9 >99.9 >99.9 b.t
>99.8 92.9 >99.8 >99.7 >99.9 >99.9 >99.8 b.t
>99.9 >99.3 >99.7 >99.7 >99.9 >99.9 >99.9 b.t
>99.6 >99.4 >99.6 >99.6 >99.8 >99.9 >99.7 b.t
orption in relation to the total of the first and second desorption
tion.
ARTICLE IN PRESS
Table 4
Recovery rate of analytes from five adsorbent materials (mean of 5 repeats with standard deviation)
Compound Recovery (%)
Tenax TA Tenax GR Carbotrap Carbotrap C Unibeads
Isopropylbenzene 102.971.4 96.571.3 97.871.1 89.973.1 102.472.0
Longipinene 96.470.9 88.077.4 92.975.0 78.073.4 89.071.1
a-Copaene 101.970.8 93.873.3 96.570.9 80.775.6 98.971.9
Isolongifolene 97.170.4 87.976.2 93.271.0 83.072.4 91.071.0
Diphenylmethane+Longifolenea 94.871.4 91.377.5 92.571.2 83.572.5 111.373.5
a-Cedrene 105.371.1 99.274.1 104.377.3 92.577.2 115.773.0
Caryophyllene 110.070.7 102.971.2 103.972.0 88.273.5 111.771.6
Geranylacetone+Aromadendrenea 89.574.0 86.174.7 86.772.6 70.974.9 94.771.9
a-Humulene 94.772.2 90.171.8 95.476.0 76.573.4 95.472.5
cis-Nerolidol 98.774.1 83.175.8 89.772.7 74.573.6 81.577.7
trans-Nerolidol 122.378.1 128.4714.0 135.278.8 100.174.1 142.179.0
Nonylbenzene+Caryophyllene-Oxidea 103.973.2 93.677.1 94.075.5 81.676.0 84.677.2
Cedrol 116.278.5 102.574.3 103.372.9 88.973.6 67.6714.4
lsolongifolen-9-one 56.870.9 54.474.9 52.671.7 47.072.1 43.873.7
aCoeluting peaks.
D. Helmig et al. / Atmospheric Environment 38 (2004) 557–572564
The reproducibility of analyte sampling and analysis
was investigated by loading 4–6 cartridges of each
adsorbent with 2.1 l at a 1:420 dilution (mixing ratios of
0.19–3.76 ppbv). For quantifying SQT analytes, GC-
FID response factors were determined by analysis of a
gas-phase, gravimetrically prepared multi-component
n-alkane reference standard (Helmig et al., 2003).
Recovery ratios were calculated in reference to the
SQT diffusion rates from the on-line GC determination.
Results from these tests are shown in Table 4. Recovery
rates are usually >90%, and are quite consistent among
the different adsorbents tested. Generally, an increase in
the standard deviation is observed with decreasing
volatility, e.g. standard deviations for oxygenated SQT
are usually two to three times higher than for the
hydrocarbon SQT.
3.4. SQT recoveries at varying humidity
As a result of plant respiration, sample air humidity
during enclosure studies can reach high levels. Recov-
eries of analytes from five adsorbent materials were
tested under conditions of varying humidity. Cartridges
were loaded for 10min at a flow rate of 206.8mlmin�1
at 1:420 dilution. Analytes were then quantified based
on their peak areas and effective carbon numbers
(Helmig et al., 2003). Sample humidity was monitored
with two Oakton thermohygrometer probes (3–5%
accuracy, Cole Parmer Instruments Co, Vernon Hills,
IL). Experiments were performed at room temperature
with relative humidities of 20%, 40%, 60%, 80% and
100%. Dilution factor and analyte mixing ratios were
the same as for the adsorbent tests.
Data for four representative SQT are shown in Fig. 3.
These data confirm the above observation that the
precision of analysis is better for SQT hydrocarbons
than for the oxygenated compounds. For Tenax TA,
Tenax GR, Carbotrap and Carbotrap C, no significant
difference was observed in the data at different
humidities; obviously the humidity did not interfere
with the sampling and analysis process. In contrast,
consistently lower recoveries were found on Unibeads
with increasing humidities. These results were surprising
and this effect was investigated more carefully, but the
reason for this behavior could not be determined.
Sampling flow rates did not change during the sampling
period. The loss of analytes could neither be accounted
for in backup cartridges nor in second desorption runs.
Because of these results, it was concluded that Unibeads
were unsuitable for use in enclosure studies and this
adsorbent was excluded from further experiments.
3.5. Adsorbent testing–linearity experiments
The linearity of the sampling/analysis procedure was
tested by sampling of increasing volumes from 0.38 to
97.3 l at 1:800 dilution (0.01 ppbv (bisabolol) to
1.91 ppbv (caryophyllene)). The results of these experi-
ments (Fig. 4) show a linear dependency of the sample
volume for the adsorbents Carbotrap and Carbotrap C.
For Tenax TA and Tenax GR, linearity is observed for
the first B40 l, but results for the 48.6 and 97.3 l samples
appear to be slightly diminished.
3.6. Adsorbent testing—detection limits
The linearity experiments were also used to estimate
the detection limits of the PE GC-FID method. The
signals observed in the lowest volume samples (0.5 l)
were used to calculate for each analyte the smallest peak
ARTIC
LEIN
PRES
S
Fig. 3. Recovery of four SQT compounds on Tenax TA, Tenax GR, Carbotrap, Carbotrap C and Unibeads as a function of relative humidity at room temperature. Data are mean
values; error bars represent standard deviation of five repetitions for 0% humidity, and three repetitions for experiments with added humidity.
D.
Helm
iget
al.
/A
tmo
sph
ericE
nviro
nm
ent
38
(2
00
4)
55
7–
57
2565
ARTICLE IN PRESS
0
1
2
3
4
5
6
7
8
9
10
0 20 40 60 80 100
Sample Volume (l)
Are
a C
ou
nts
(V*s
)
CaryophylleneLongipineneIsolongifoleneCedrolIsolongifolene-9-one
Tenax TA Tenax GR
0
1
2
3
4
5
6
7
8
9
10
0 20 40 60 80 100
Sample Volume (l)
Are
a C
ou
nts
(V
*s)
CaryophylleneLongipineneIsolongifoleneCedrolIsolongifolene-9-one
Carbotrap
0
1
2
3
4
5
6
7
8
9
10
0 20 40 60 80 100Sample Volume (l)
Are
a C
ou
nts
(V*s
)
CaryophylleneLongipineneIsolongifoleneCedrolIsolongifolene-9-one
Carbotrap C
0
1
2
3
4
5
6
7
8
9
10
0 20 40 60 80 100Sample Volume (l)
Are
a C
ou
nts
(V
*s)
CaryophylleneLongipineneIsolongifoleneCedrolIsolongifolene-9-one
Fig. 4. Results for five selected SQT (in FID area counts) in increasing sampling volumes. SQT mixing ratios in the multi-component
test samples were longipinene 1.61 ppbv, isolongifolene 1.28 ppbv, caryophyllene 2.23 ppbv, cedrol 0.37 ppbv and isolongifolen-9-one
0.61 ppbv, respectively.
D. Helmig et al. / Atmospheric Environment 38 (2004) 557–572566
area that can be integrated and quantified. The
minimum detectable analyte amounts were estimated
to be in the range of 0.19–0.36 ng, equivalent to analyte
mixing ratios of 20–40 pptv in a 1 l sample volume.
3.7. Testing of tubing materials
A series of different tubing materials were tested for
their possible retention of SQT. The tested materials were
flexible silicone tubing (4.8mm o.d., 4.70m length; Cole
Parmer), stainless steel (3.2mm o.d., 2.20m length;
Alltech), copper tubing (3.2mm o.d., 2.80m length;
Alltech), Teflon (PTFE, 3.2mm o.d., 3.7m length; Cole
Parmer) and Silicosteel (3.2mm o.d., 1.8m length; Rest-
ek). These tubing materials were inserted into the flow
path of the CDS before the valve switching compartment
(Helmig et al., 2003). Tubing was kept outside the CDS at
room temperature. The total SQT sample flow rate was
B108ml min�1, resulting in SQT mixing ratios of
B6ppbv (bisabolol) to 170ppbv (caryophyllene). After
passing through the tubing quantification was achieved by
loop-injection of 1ml samples onto the on-line GC-FID
system (Helmig et al., 2003).
In a first set of experiments with increasing purge
times, it was found that purging for B10min was
required (B1 l of sample air) before steady-state
conditions were achieved. All subsequent tests were
performed with at least 15min purge times. Results for
stainless steel, copper, Teflon and Silicosteel are shown
in Fig. 5. None of the analytes were recovered after
passing through the silicone tubing, most likely a result
of loss/adsorption to the silicone tubing walls. Recov-
eries for all other materials generally were >90%,
results for oxygenated SQT are somewhat lower
(B80–90%), but still within a usable range for
quantitative analysis (except for bisabolol and farnesol
through Teflon tubing).
3.8. Storage in sampling bags
Teflon film materials have been a favorite material
used for bag enclosure experiments (Enders et al., 1992;
Helmig et al., 1999a; Cao and Hewitt, 1999; Komenda
et al., 2001). The stability of a SQT gas mixture in a
Teflon gas sampling bag (10 l Teflon bag, Type L Teflon
film; Alltech) was investigated for possible losses of SQT
to the bag material. In a series of experiments, the outlet
of the CDS was diluted with dry and humidified
nitrogen, respectively, and flown into the bag. The
overall dilution factor was B1:23 resulting in analyte
ARTICLE IN PRESS
0
20
40
60
80
100
120
LPNCO
PIS
O LFCNE
CRY
ARO
CRYO
CROL
ISO
ON
BIS
FAR
Re
co
ve
ry (
%)
Copper
0
20
40
60
80
100
120
LPNCO
PIS
O LFCNE
CRY
ARO
CRYO
CROL
ISO
ON
BIS
FAR
Re
co
ve
ry (
%)
Stainless Steel
PTFE Teflon
0
20
40
60
80
100
120
LPNCOP
ISO LF
CNE
CRY
ARO
CRYO
CRO
LIS
OON
BIS
FAR
Re
co
ve
ry (
%)
Silicosteel
0
20
40
60
80
100
120
LPNCOP
ISO LF
CNE
CRY
ARO
CRYO
CRO
LIS
OON
BIS
FAR
Re
co
ve
ry (
%)
Fig. 5. Recovery of a series of SQT after sampling through different tubing materials. Recovery and respective standard deviation
(n ¼ 4–10) are presented for each compound. Abbreviated compounds are (in alphabetical order): ARO: aromadendrene; BIS:
bisabolol; COP: a-copaene; CNE: cedrene; CROL: cedrol; CRY: b-caryophyllene; CRYO: caryophyllene oxide; FAR: farnesol; ISO:
isolongifolene; ISOON: isolongifolen-9-one; LF: longifolene; LPN: longipinene.
0102030405060708090
100
0 5 10 15 20 25 30Time after filling (hours)
Rec
ove
ry (%
)
IPB
LPN
COP
ISO
LF
CNE
CRY
ARO
Fig. 6. Storage of SQT in a Teflon bag at room temperature
and B45–48% RH. Abbreviated compounds are (in alphabe-
tical order): ARO: aromadendrene; COP: a-copaene; CNE:
cedrene; CRY: b-caryophyllene; IPB: 1,3,5-tri-isopropylben-
zene; ISO: isolongifolene; LF: longifolene; LPN: longipinene.
D. Helmig et al. / Atmospheric Environment 38 (2004) 557–572 567
mixing ratios of B10–70 ppbv. The sample relative
humidity range was 0–49%. The bag was filled over
B30min while it was kept at room temperature.
Immediately after the bag was filled, samples were
drawn out of the bag and analyzed with the on-line GC.
The sample withdrawal was interrupted during GC runs
and resumed for a 5min purge prior to the subsequent
injection. In this manner, the experiment was continued
until the 10 l Teflon bag was totally emptied (26 h).
The results from one of these experiments at B45–
48% sample RH are presented in Fig. 6. SQT hydro-
carbons show initial recovery rates on the order of
70–90%. It needs to be realized that at the time of the
first sample withdrawal B35min had passed from the
beginning of the bag filling. SQT losses seem to be faster
in the first few hours. After one day of sample storage,
the hydrocarbon SQT mixing ratios had dropped to
B10–30% of their initial values. From this loss, an
average decay rate of B4% per hour was calculated for
these 8 non-oxygenated compounds. None of the
oxygenated SQT could be recovered from the bag.
3.9. Leaf cuvettes
Two leaf cuvettes, one made of stainless steel, with a
borosilicate glass window (volume of 0.44 l), and the
other cuvette made of Delrins acetal resin, also with a
glass window (volume of 0.63 l) (Fig. 7) were tested.
These cuvettes have 2–3 bulkhead sampling ports for
intake air and sample withdrawal. The CDS output was
diluted with humidified nitrogen resulting in a total flow
of B250mlmin�1. This SQT standard was flown into
the cuvette through one of the sampling ports. A
sampling flow of 55mlmin�1 was continuously with-
drawn from the cuvette through one of the other ports
ARTICLE IN PRESSD. Helmig et al. / Atmospheric Environment 38 (2004) 557–572568
and analyzed with the on-line GC. Neither cuvette was
vacuum tight, so the remainder of the excessive inlet
flow (B195mlmin�1) leaked out through the seal of the
glass window. The experiment was performed in three
steps. First, only the humidified nitrogen was purged
through the cuvette for 2 h. Next, the SQT were added
instantaneously. In the third step the cuvettes were again
purged with SQT-free humidified nitrogen. Reference
measurements (100% recovery rate) were done by
performing the same experiment with a 0.32 cm stainlees
steel Swagelok tee (heated to 50�C) in place of the leaf
cuvette.
Results for both cuvette experiments at 60% RH are
illustrated in Fig. 8. The theoretically expected mixing
ratio (calculated from the cuvette volume and the purge
Fig. 7. Two leaf cuvettes tested: stainless steel to the left,
Delrins acetal resin to the right. The glass window was sealed
against the cuvette body with a white closed cell foam gasket
(steel cuvette) and with Teflon tape (Delrin cuvette), respec-
tively.
0
20
40
60
80
100
120
0 5 10 15 20 25 30Time (hours)
Rec
ove
ry (%
)
IPBLPNCOPISOLFCNECRYAROCRYOCROLTheory
<- SQT on
<- SQT off
Rec
ove
ry (%
)
Fig. 8. Recovery of test compound standard mixture from a stainless
B55% RH. The theoretically expected recovery from the gas mixing
sets). Abbreviated compounds are (in alphabetical order): ARO: aro
CRY: b-caryophyllene; CRYO: caryophyllene oxide; IPB: 1,3,5-tri-
longipinene. SQT on/off illustrates the times when the SQT were add
b-caryophyllene were not included in the Delrin cuvette experiment. A
completely lost in the Delrins leaf cuvette.
flow rate) is added to these figures (solid line) in order to
better illustrate the analyte losses. For both cuvettes,
substantial analyte losses were found in the initial phase
of the experiment. Equilibration time in excess of 5 h
were required before recovery rates of >80% were
achieved for the non-oxygenated SQT. In the stainless
steel cuvette, oxygenated SQT, e.g. cedrol and caryo-
phyllene oxide, could only be partially retrieved
(B60%). Nerolidol, geranylacetone, isolongifolen-9-
one were completely lost. None of the oxygenated
SQT were recovered from the Delrins acetal resin
cuvette. After the SQT flow was turned off, they were
present in the sample air for many hours with a slow and
gradual decline. Cuvette experiments performed at
B0%, 20% and 45% RH levels gave similar results.
These data show that in both cuvettes, significant SQT
surface losses occurred and long equilibration times (i.e.
large purge volumes) were required before steady state
conditions were achieved. Memory effects were clearly
evident, and it took many hours of continuous purging
to remove the analytes from the walls of the cuvettes.
4. Discussion
Hundreds of SQT have been identified and character-
ized in plant materials (Joulain and K .onig, 1998). The
number of identified SQT in volatile emissions from
vegetation is substantially lower. The identification of
SQT is often hindered by the lack of reference mass
spectra and/or GC retention data. The MS and RI data
of the eleven SQT and seven oxygenated SQT included
in this study will facilitate their future identification.
However, rather substantial deviations (up to B25 RI
units) were seen in the RI of SQT on the two DB-1
columns included in this study. Possible reasons for this
0
20
40
60
80
100
120
0 5 10 15 20 25 30 35 40Time (hours)
LPN
COP
ISO
LF
CNE
ARO
Theory
<- SQT on
<- SQT off
steel leaf cuvette (left) and from a Delrins leaf cuvette (right) at
in the cuvette (assuming no analyte loss) is added to both data
madendrene; COP: a-copaene; CNE: cedrene; CROL: cedrol;
isopropylbenzene; ISO: isolongifolene; LF: longifolene; LPN:
ed and turned off, respectively. 1,3,5-tri-isopropylbenzene and
ll of the oxygenated SQT were included in this experiment but
ARTICLE IN PRESSD. Helmig et al. / Atmospheric Environment 38 (2004) 557–572 569
discrepancy include different column phase thicknesses
(0.25 vs. 1mm), the different injection techniques (on-line
loop injection versus thermal desorption from adsorbent
cartridges) or the different, previous uses of the
individual columns. Conclusively, these data show that
unequivocal identification of SQT by RI comparison
alone is troublesome unless the GC retention can be
confirmed by GC analysis of the respective SQT
standard. Tentative MS identification of an unknown
compound as SQT can be accomplished by observing
characteristic ions, such as at m=z ¼ 204; 175, 161, 121,93. However, mass spectra of different SQT can be quite
similar, so the unequivocal identification requires the
respective SQT standard.
Automated sampling of vegetation emission samples
has many advantages over manual procedures. The
results with the sampler used in this study demonstrate
the feasibility of automated sampling. Critical para-
meters that need to be considered are the permanent
flushing of all valve and tubing components with the
sample gas, sufficient purge times prior to sample
collection and elevated temperatures (50�C) for valves
and tubing in the sample flow.
Tenax TA, Tenax GR, Carbotrap and Carbotrap C
all proved to be good adsorbent choices for enrichment
of SQT hydrocarbons from air samples. No significant
losses from breakthrough or incomplete desorption were
observed for SQT hydrocarbons. Precision and accuracy
of usually better than 10% were achieved with careful
control of sampling and analysis procedures. None of
these adsorbents showed interferences from sample
humidity, which is in agreement with their low water
uptake rates reported previously (Helmig and Vierling,
1995). Analytical problems from rearrangement reac-
tions during solid adsorbent sampling/analysis have
previously been reported for the monoterpene b-pinene(Cao and Hewitt, 1993; Arnts et al., 1995). SQT
rearrangement reactions were not observed during any
of the experiments performed in these studies. Analysis
of oxygenated SQT poses a bigger challenge stemming
from the higher polarity, respectively lower volatility of
these compounds. Precision and accuracy on the order
of B25% were achieved for the more volatile com-
pounds in this group (RI 1500–1650), which demon-
strates that these compounds can still be analyzed by
solid adsorbent techniques with reasonable success. In
contrast, the less volatile farnesol (RI 1775) was rarely
recovered in any of these experiments.
A potential problem of Tenax TA is the observed
volume loss (shrinking) of the material from repeated
sampling/thermal desorption cycles (B10% loss of
volume after 20 cycles). The gaps in the adsorbent bed
that would form after a number of cycles were
eliminated by carefully pushing the adsorbent further
into the cartridge. Potential changes in the analyte
retention from this shrinking were not investigated in
the course of this study. Retention of SQT on Glass
Beads was weak. This material may be useful for
secondary focussing traps, but breakthrough volumes
are too low for collection of SQT in emission samples.
Similarly, the interference from water vapor found on
Unibeads appears prohibitive for emission sample
collection.
5. Conclusions
The experiments performed on different tubing
materials, sampling bags and leaf cuvettes conclusively
showed that SQT rapidly adsorb on material surfaces. A
number of precautions needs to be followed in order to
prevent substantial analytical errors. Long purge times
are required to passivate surfaces, reach equilibrium and
minimize analytical losses. For B0.5 l leaf cuvettes with
B250ml inlet flow rate, required purge times are on the
order of 5–10 h. These results confirm earlier observa-
tions in experiments on injection loop materials and
loop temperatures for the on-line GC (Helmig et al.,
2003), where temperatures in excess of 90�C were
required to eliminate SQT wall losses on glass, nickel,
stainless steel and Silicosteel. Even under careful
consideration of these conditions, oxygenated SQT
could not be quantitatively recovered in the cuvette
experiments.
Included aromatic compounds as well as geranylace-
tone gave similar results as the SQT. Therefore, it can be
concluded that our findings were mostly related to the
analyte volatility and polarity, rather than specific for
SQT. Consequently, this study will be applicable and
beneficial for analysis of other VOC in the C13–C17
volatility range (e.g. polycyclic aromatic hydrocarbons)
in air samples and by solid adsorbent sampling with
thermodesorption GC.
The data further demonstrate the difficulties in SQT
analysis. It is likely that SQT emissions from vegetation
have been overlooked in many previous studies because
of the analytical challenges posed by these compounds.
SQT flux experiments by techniques such as eddy
correlation, relaxed eddy accumulation, and disjunct
eddy sampling do not appear promising, since all of
these methods rely on the capture of rapid changes in
atmospheric concentrations. The long times needed for
reaching equilibrium between sampling lines, valves, and
other sampling apparatus components with the SQT in a
gas-phase sample will significantly blur and decrease
changes in atmospheric fluctuations, which compro-
mises the applicability of these flux techniques.
Enclosure chambers are a frequently used technique
in the research on chemically mediated plant–insect
interactions. Most of these published experiments
rely on qualitative observations and relatively little
attention has been paid to experimental requirements for
ARTICLE IN PRESSD. Helmig et al. / Atmospheric Environment 38 (2004) 557–572570
quantitative measurements. This study demonstrate the
limitations for detection and accurate quantification of
SQT, in particular for oxygenated SQT, in headspace
sampling and enclosure experiments. These findings and
recommendations will facilitate improved experimental
designs in research on plant-insect communication and a
better (quantitative) interpretation of SQT observations.
Because of SQT are easily lost to materials surfaces, it
appears likely that within a forest environment, SQT are
similarly adsorbed by soils and vegetation surfaces. This
process may be another important sink in addition to
the fast losses from atmospheric reactions and uptake to
aerosols. Due to these multiple sinks, only a fraction of
the emitted SQT will escape the forest and be observable
by above canopy flux measurement techniques.
Therefore, the results from this study re-emphasize
that enclosure studies are the most promising experi-
mental approach for capturing SQT emissions from
vegetation. Following the guidelines developed in this
research, both leaf cuvette and bag enclosure experi-
ments with solid adsorbent sampling will yield quality
leaf and branch level emission rate data for non-
oxygenated SQT. Oxygenated SQT, however, undergo
substantial, fast and irreversible losses to enclosure
materials. This makes their quantitative analysis
by these methods impractical and may explain the
scarcity of observations with identified oxygenated
SQT emissions in previous vegetation enclosure
studies.
Acknowledgements
Peter Harley and Alex Guenther, National Center for
Atmospheric Research, Boulder, provided the leaf
cuvettes. J.P. was supported by a fellowship stipend
from the Deutsche Akademische Austauschdienst. John
Ortega, University of Colorado and an anonymous
reviewer gave helpful comments on the manuscript. This
research was supported through a grant from the
National Science Foundation, Atmospheric Chemistry
Program, ATM-9911186.
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