Widespread Pesticide Distribution in the European Atmosphere Questions their Degradability in Air
s.n
Auteur moral
Auteur secondaire
Résumé
"Risk assessment of pesticide impacts on remote ecosystems makes use of model-estimated degradation in air. Recent studies suggest these degradation rates to be overestimated, questioning current pesticide regulation. Here, we investigated the concentrations of 76 pesticides in Europe at 29 rural, coastal, mountain, and polar sites during the agricultural application season. Overall, 58 pesticides were observed in the European atmosphere. Low spatial variation of 7 pesticides suggests continental-scale atmospheric dispersal. Based on concentrations in free tropospheric air and at Arctic sites, 22 pesticides were identified to be prone to long-range atmospheric transport, which included 15 substances approved for agricultural use in Europe and 7 banned ones. Comparison between concentrations at remote sites and those found at pesticide source areas suggests long atmospheric lifetimes of atrazine, cyprodinil, spiroxamine, tebuconazole, terbuthylazine, and thiacloprid. In general, our findings suggest that atmospheric transport and persistence of pesticides have been underestimated and that their risk assessment needs to be improved."
Editeur
Environmental Science & Technology
Descripteur Urbamet
eau
;pollution de l'air
;pollution de l'eau
;pollution atmosphérique
Descripteur écoplanete
pluie acide
Thème
Sciences de la terre
;Risques
;Santé
Texte intégral
Widespread Pesticide Distribution in the European Atmosphere
Questions their Degradability in Air
Ludovic Mayer,#### Céline Degrendele,*,#### Petr Senk, Jir? Kohoutek, Petra Pr?bylová, Petr Kukuc?a,
Lisa Melymuk, Amandine Durand, Sylvain Ravier, Andres Alastuey, Alex R. Baker, Urs Baltensperger,
Kathrin Baumann-Stanzer, Tobias Biermann, Pernilla Bohlin-Nizzetto, Darius Ceburnis, Sébastien Conil,
Cédric Couret, Anna Degórska, Evangelia Diapouli, Sabine Eckhardt, Konstantinos Eleftheriadis,
Grant L. Forster, Korbinian Freier, François Gheusi, Maria I. Gini, Heidi Hellén, Stephan Henne,
Hartmut Herrmann, Adéla Holubová Smejkalová, Urmas Hõrrak, Christoph Hüglin, Heikki Junninen,
Adam Kristensson, Laurent Langrene, Janne Levula, Marie Lothon, Elke Ludewig, Ulla Makkonen,
Jana Matejovic?vá, Nikolaos Mihalopoulos, Veronika Mináriková, Wolfgang Moche, Steffen M. Noe,
Noemí Pérez, Tuukka Petäjä, Véronique Pont, Laurent Poulain, Etienne Quivet, Gabriela Ratz,
Till Rehm, Stefan Reimann, Ivan Simmons, Jeroen E. Sonke, Mar Sorribas, Ronald Spoor,
Daan P. J. Swart, Vasiliki Vasilatou, Henri Wortham, Margarita Yela, Pavlos Zarmpas,
Claudia Zellweger Fäsi, Kjetil Tørseth, Paolo Laj, Jana Klánová, and Gerhard Lammel*
Cite This: Environ. Sci. Technol. 2024, 58, 3342?3352 Read Online
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ABSTRACT: Risk assessment of pesticide impacts on remote
ecosystems makes use of model-estimated degradation in air. Recent
studies suggest these degradation rates to be overestimated,
questioning current pesticide regulation. Here, we investigated the
concentrations of 76 pesticides in Europe at 29 rural, coastal,
mountain, and polar sites during the agricultural application season.
Overall, 58 pesticides were observed in the European atmosphere.
Low spatial variation of 7 pesticides suggests continental-scale
atmospheric dispersal. Based on concentrations in free tropospheric
air and at Arctic sites, 22 pesticides were identified to be prone to
long-range atmospheric transport, which included 15 substances
approved for agricultural use in Europe and 7 banned ones.
Comparison between concentrations at remote sites and those
found at pesticide source areas suggests long atmospheric lifetimes of atrazine, cyprodinil, spiroxamine, tebuconazole, terbuthylazine,
and thiacloprid. In general, our findings suggest that atmospheric transport and persistence of pesticides have been underestimated
and that their risk assessment needs to be improved.
KEYWORDS: pesticides, atmosphere, transport, degradation, risk assessment
? INTRODUCTION
Pesticides are synthetic chemicals used for their toxic effects.1
Their agricultural use has significantly increased globally from
2.4 million tons in 1990 to 4.1 million tons in 2020.2,3 Chemicals
authorized for pesticidal use vary widely in their chemical
structures and physicochemical properties.4,5 Since the 1960s,
growing environmental and health concerns have led to usage
restrictions of the previously dominant organochlorine
pesticides, to their substitution by more biodegradable ones,
and, where possible, to less intensive application.6 Because of the
toxicity of pesticides and their metabolites to nontarget
organisms, environmental exposure to pesticides is a concern.7,8
Upon bioaccumulation and biomagnification, lipophilic pesti-
cides (with an octanol?water partition coefficientKOW of > 105)
may reach effect levels in top predators and humans.9?11
Most pesticides are semivolatile organic compounds
(SVOCs).10 They enter the atmosphere upon application via
Received: October 14, 2023
Revised: January 24, 2024
Accepted: January 24, 2024
Published: February 7, 2024
Articlepubs.acs.org/est
© 2024 The Authors. Published by
American Chemical Society
3342
https://doi.org/10.1021/acs.est.3c08488
Environ. Sci. Technol. 2024, 58, 3342?3352
This article is licensed under CC-BY 4.0
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direct emission from spray drift, through wind erosion of soil
particles containing pesticides, and via volatilization from soil,
vegetation, or water surfaces.3,12?14 Currently used pesticides
have been found in rural air15?17 and ecosystems18,19 but have
also been observed far from the sources, at high mountains,20 in
the marine boundary layer,21,22 and in the Arctic.10,23,24 Such
observations have been sporadic because unlike organochlorine
pesticides, these pesticides are rarely included in air-monitoring
programs (in Europe apart from France and Sweden25).
Evidence for long-range transport to remote areas is one of the
criteria for a chemical to be considered a persistent organic
pollutant (POP).26,27 Unlike organochlorine pesticides (e.g.,
DDT, lindane) which are classified as POPs, it has been largely
considered that the new generation of pesticides, currently in use
globally, are not prone to long-range atmospheric transport
(LRAT) due to their short atmospheric half-lives (i.e., <2
days).27 The atmospheric lifetime of SVOCs is determined by
gas/particle partitioning and their reactivity in the gaseous and
particulate phases and, if degradation is resisted in Earth surface
compartments, might be enhanced by multiple cycles of
deposition and revolatilization (grasshopper effect).28,29 How-
ever, gas/particle partitioning of currently used pesticides is
incompletely understood and experimental data for reactions
with atmospheric oxidants are available for only few
substances.30?35 Without such data, degradability in air is
often assessed based on model-estimated reactivity with the
hydroxyl (OH) radical in the homogeneous gas phase.36
However, recent findings have shown the presence of pesticides
with theoretical persistence in air below the LRAT potential
threshold also in remote areas.22?24 This questions the accuracy
of the pesticide risk assessment in Europe to protect the
atmospheric environment and remote ecosystems, which
considers only the atmospheric half-life, for which only the
modeled reactivity with the OH radical in the gas phase is
considered.
Here, taking advantage of air-monitoring infrastructures, we
present the continental-scale distributions of 76 pesticides in the
atmosphere over Europe. To this end, 77 particulate and 17 gas-
phase samples were collected during the main pesticide
application period in spring 2020 at 29 rural, coastal, mountain,
and polar sites across Europe and the European Arctic (Figure
S1 and Table S1).
? MATERIALS AND METHODS
Sampling Sites. The contributing 29 sampling sites (Table
S1) are observational platforms of the Aerosol, Clouds and
Trace Gases Research Infrastructure (ACTRIS, www.actris.eu/)
and/or the Co-operative Programme for Monitoring and
Evaluation of the Long-range Transmission of Air Pollutants
in Europe (EMEP, www.emep.int/) and have long-term
expertise with atmospheric aerosol particle and trace gas
sampling. These 29 sampling sites are located in 17 different
European countries and in the European Arctic (Figure S1) and
were classified as rural (n = 16), coastal (n = 4), mountain (n =
6), and polar (n = 3) based on their geographical characteristics
and/or land use analysis. Indeed, the mountain and polar sites
were defined based on their geographical characteristics with,
respectively, an altitude of >2000 m a.s.l. and a latitude of
>67°N. In the second step, the type of land use surrounding each
sampling site (10 km radius) was characterized using the
CORINE Land Cover 2018 for all sites except the Zeppelin
Observatory for which the Global Land Cover 2000 was used
(Table S2).37 To this end, the many categories available from
these databases were grouped into more relevant ones
considering the aim of this study (Table S3). The coastal sites
were defined as those having >35% of their surrounding areas
(10 km radius) as water bodies, while for rural sites, it was >60%
of agricultural land, forest and shrub, and/or herbaceous
vegetation associations. In addition, the rural sites were
subcategorized as agricultural-adjacent (A.) or nonagricultural-
adjacent (N.A.) if their share of agricultural land in their
surrounding area was above or below 45%, respectively.
Sampling. Sampling took place simultaneously at all 29 sites
in the main pesticide application season in spring 2020 during
three 48 h sampling periods (namely, 28?30/04, 12?14/05,
and 26?28/05). Sampling was performed with active air
samplers (low or high volume, based on on-site availability,
Table S1). Due to Covid-19 epidemic-related restrictions in
some countries, only 22 sites collected samples during all three
sampling periods, while 4 and 3 sites collected samples during 2
and 1 sampling period, respectively (Table S1).
All sites collected the particulate phase on quartz fiber filters
(QFF, QM-A, Whatman, U.K.), preferentially (but not always)
with a PM10 inlet, as CUPs have previously been found in both
the fine and coarse particles.15 In addition, six sites (ADA, BKO,
KOS, SBO, UFS, and ZPO) sampled also the gaseous phase on a
sandwich sorbent (i.e., PUF/XAD2/PUF sandwich), consisting
of a polyurethane foam plug (PUF,Molitan a.s., Czech Republic,
density 0.030 g cm?3, 5 cm depth, diameter of 5.5/11 cm for the
low/high-volume air sampler), a layer of XAD resin (Supelpak-
2, Supelco), and another PUF plug, separated by cotton wool.
This sandwich configuration has been shown to be the most
efficient for the collection of gaseous pesticides.38 Prior to
sampling, PUFs and XAD2 were precleaned via Soxhlet
extraction with acetone for 8 h, followed by 8 h of extraction
in methanol. All sampling media were provided by RECETOX
and shipped to the sites. In total, 77 samples and 35 field blank
samples were collected (i.e., 77 QFFs and 17 PUF/XAD2/PUF
sandwiches) and kept in the freezer at ?18 °C until extraction.
Sample Preparation, Analysis, and QAQC. All samples
underwent spiking with labeled standards (Table S4) before
extraction. The extraction process involved using an automatic
extractor (Büchi Extraction System, B-811, Switzerland) with 5
mM ammonium acetate in methanol. The extraction process
consisted of 1 h of warm Soxhlet, followed by 1 h of solvent
rinsing, and a concentration step to 1 mL using nitrogen. After
centrifugation for 10 min (12,000 G, Z-36 HK, Hermle
Labortechnik, Germany) within polypropylene tubes (Corning
Costar Spin-X), the extracts were filtered (cellulose acetate
membrane and 0.22 ?m pore size) and further concentrated to
0.5 mL under nitrogen.
Postextraction, the samples were divided into three 100 ?L
aliquots, each undergoing a different analysis. The three analyses
allowed the quantification of 76 pesticides (35 herbicides, 22
insecticides, and 19 fungicides) (Table S5). Among these
pesticides, 40 are approved for agricultural use in Europe, 22 are
among the most globally used pesticides, 34 are characterized as
priority active ingredients to be monitored in France, 13 are
highly hazardous pesticides, and 25 are high-risk pesticides.
To ensure quality assurance, field blanks were analyzed
alongside air samples collected. Blank levels of most individual
analytes were generally below or low (Tables S6 and S7).
Procedural recoveries were assessed by spiking sampling media
with native standards and their corresponding isotopic-labeled
standards, followed by processing as per sample. Most
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procedural recoveries fell within the range of 60?120% with
standard deviations below 20%, except for a few exceptions.
Detailed information about the procedures is provided in the
Supporting Information.
Air Mass Origin. The Lagrangian particle dispersion model
FLEXPART39 was used to identify the potential source regions
by calculating the residence times in the surface layer of air
sampled.
The meteorological data used (0.5 and 1° and 3 h horizontal
and temporal resolutions, 137 vertical levels) were obtained
from the European Centre forMedium-RangeWeather Forecast
(www.ecmwf.int, last access: 21/06/2022). For each simulation,
100,000 particles were continuously released from the sites at
the ground level for the polar sites and at altitudes ranging 190?
210 m agl for mountain sites and were followed for 30 and 10
days backward in time at polar sites and mountain sites,
respectively (Figures S2?S5).
Advection to Mountain Sites. For the six high-mountain
sites, the advection was characterized using various combina-
tions of on-site tracer measurements and meteorological data
and modeling. For all mountain sites, the conclusions on the
planetary boundary layer (PBL) influence on the sampled air
were based on the site-specific experiences (Table S8).
At CPK, regional chemistry-transport modeling data
(ALADIN model, 2 km × 2 km horizontal resolution)40 were
used to judge whether the sampled air was within the free
troposphere (FT) or within the PBL. The CPK site was within
the FT duringmost of the sampling time. However, due to short-
term (<1 h) liftings of the inversion (which occurred 2, 10, and 2
times during the sampling periods 1, 2, and 3, respectively), PBL
air was mixed into all three air samples.
The model terrain is ca. 500 m below the true altitude.
Moreover, due to resolution limitations of the model, in
particular, in complex terrain, upslope movement of air from
valleys will be systematically underestimated. For HAC, the on-
site gaseous (i.e., CO, CO2) and aerosol tracer measurements,
meteorological parameters, and planetary boundary layer height
(obtained from ECMWF) were used.41?43 Air collected during
period 2 represented almost exclusively the FT. It was heavily
affected by Sahara dust long-range transport. Sampling period 3
was characterized by relatively low and stable concentrations of
specific tracers (i.e., aerosol absorption and particle number
concentration), but the station was mostly in clouds, indicating
conditions characteristic of the interface between FT and PBL.
PBL influence on air collected cannot be excluded. No sample
was collected during period 1. For JFJ, on-site Rn measure-
ments44 and data from a ceilometer, obtained at the foot of the
site (measured at Kleine Scheidegg, altitude difference of 1510
m; 6 km direct distance from JFJ),45 were used to judge free
tropospheric vs boundary layer air. JFJ was above the planetary
boundary layer during short periods in all three sampling
periods. The samples represent mixed FT and PBL air. At PDM,
the analysis of 222Rn measurements (?-detection) suggested
mixed FT and PBL air during sampling period 3. No samples
were collected during periods 1 and 2. For SBO, data from a
ceilometer (Vaisala CL51)46 obtained at the foot of the site
(measured at Kolm-Saigurn, altitude difference of 1466 m; 5 km
direct distance from SBO) were used to judge on FT vs PBL air.
Heights for measuring periods with signals under the detection
limit, which occurred during nighttime, were interpolated. The
derived heights of the PBL were below SBO during all three
sampling periods. No sample was collected during period 1. At
UFS, the 222Rn measurements (?-detection)47 suggested FT air
with some PBL influence during the sampling periods 1 and 2
and almost exclusively FT air during sampling period 3. The
attribution is supported by on-site measurements of humidity
and other meteorological parameters.48 In addition, advection
and possible collection of FT air were investigated for two other
elevated sites, i.e., RIG (Switzerland, 1031 m a.s.l.) and ZPO
(Svalbard, 474 m a.s.l.). In situ and ceilometer data,49
respectively, besides others, indicated that at both sites, the air
collected during the three sampling periods was PBL air or PBL
with little FT air mixed in.
Data Analysis. All the statistical analysis was performed
using software GraphPad Prism (v9.0.0). For these analyses,
when the concentration of a compound was lower than that of
iLOD, iLOQ, or LOQb, these values were not taken into
account. Substitutions of values below LOQ by LOQ/2 were
used to determine the relative standard deviation (Table 1).
Detailed information about the procedures is provided in the
Supporting Information.
? RESULTS AND DISCUSSION
European Distribution of Atmospheric Pesticides.Out
of the 76 pesticides targeted, 58 were found in the atmosphere,
including the European Arctic. In the atmospheric particulate
phase, 51, 38, 24, and 6 pesticides were found at rural, coastal,
mountain, and polar sites, respectively (Figures S6?S8).
Overall, the number of particulate pesticides decreases with
latitude and increases with the proximity to agricultural fields
(Figure 1). Among these 58 pesticides present in European air,
about 50% were rarely found (1?5 sites), while around 20%
were quantified in more than half of the sites investigated (Table
S9).
The concentrations of pesticides quantified on aerosol
particles were minimal at ZPO (Svalbard) with 24.5 fg m?3 on
average and ranged from 0.14 to 3.9 ng m?3 at agricultural sites
(CRA and OPE sites, respectively) (Figure 2). On an individual
substance point of view, cyprodinil, fenpropidin, prosulfocarb,
and spiroxamine were the pesticides with the highest
concentrations (i.e., up to 7.51, 3.53, 1.71, and 1.82 ng m?3,
Table 1. Spatial Homogeneity of Distributions:
Concentration Range (Expressed as log(cmax/cmin)), Relative
Standard Deviation (RSD; %) at All Sites and Comparison of
Mean Particulate Concentrations at Remote Sites, crs (Polar +
Free Tropospheric Mountain Sites) and Other Sites, cos
(Coastal + Nonfree Tropospheric Mountain + Rural Sites)a,b
crs
(pg m?3)
cos
(pg m?3)
log
(cos/crs)
log
(cmax/cmin)
RSD
(%)
2,4-D <LOQ 4.46 N.A.b 2.1 159
atrazine 0.11 0.30 0.4 1.6 107
cyprodinil 26.5 215 0.9 5.7 602
fenpropidin 7.30 127 1.2 4.5 548
fenpropimorph 2.37 46.1 1.3 3.6 199
metazachlor <LOQ 2.59 N.A.b 3.2 263
S-metolachlor 5.16 81.7 1.2 3.2 147
spiroxamine 11.9 78.3 0.8 4.0 378
tebuconazole 0.95 10.3 1.0 3.4 213
terbuthylazine 54.3 53.5 0.0 3.4 291
thiacloprid 0.24 1.14 0.7 1.7 103
aValues < LOQ not included. Substances with a quantification
frequency higher than 50% only. bN.A. = not applicable.
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respectively), while for all other pesticides, their concentrations
were mostly below 1 ng m?3.
8 out of 11 pesticides exhibiting a quantification frequency
exceeding 50% (Table S9) (i.e., cyprodinil, fenpropidin,
fenpropimorph, metazachlor, S-metolachlor, spiroxamine, tebu-
conazole, and terbuthylazine) had their particulate concen-
trations spanning 3 to 6 orders of magnitude (log(cmax/cmin) =
3?6), while the other three (i.e., 2,4-D, atrazine, and
thiacloprid) exhibited a more uniform distribution across the
continent (log(cmax/cmin) ? 2 and RSD < 200%) (Table 1 and
Figures S9 and S10). Moreover, for atrazine and thiacloprid, the
concentration gradient from the source areas was particularly
small: The average concentrations at remote sites (free
tropospheric mountain and Arctic) were within an order of
Figure 1.Number of pesticides quantified in the particulate phase: (A) latitudinal distribution (third-order polynomial regression) and (B) related to
agriculture (area fraction within 10 km, in %). On each figure, the gray line represents the regression and the dotted lines represent the 95% confidence
interval.
Figure 2. Pesticide mean concentrations quantified at each site in the particulate (all sites) and gaseous phases (6 sites).
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magnitude of the average concentrations at other sites (rural +
coastal + mountain) (log(cos/crs) < 1; Table 1). The same was
found for cyprodinil, spiroxamine, tebuconazole, and terbuthy-
lazine. Such uniform distributions suggest that the atmospheric
lifetime of the compounds is similarly long or its source
distribution is similarly wide as that of atrazine. Atrazine, an
herbicide banned since 2004,50 continues to be present in
European air, likely a consequence of its persistence and long-
range transport from regions where it is still used.3,51?53 Because
of its persistence, atrazine keeps cycling in air, even 25 years after
its ban in Europe. It is re-emitted from secondary sources, but
primary sources outside Europe may also contribute.54
Among these frequently observed pesticides, 8 are approved
for agricultural use in Europe, except for atrazine, fenpropi-
morph, and thiacloprid (Tables S5). Fenpropimorph is a
fungicide banned shortly before our sampling campaign but
remained authorized for use as a biocide until 2021.55
Thiacloprid, banned for agricultural use in May 2020, is another
exception. Among the less frequently found pesticides,
acetochlor, carbaryl, and simazine, their European approvals
had lapsed more than 9 years before our sampling. Interestingly,
concentrations of these substances at remote sites did not
significantly differ from those at rural sites bymore than an order
of magnitude (Table 1), indicating their persistence and long-
range transport from regions where they are still in use, such as
North America and Africa.
By hierarchical cluster analysis, we find a high degree of
similarity in particulate pesticide substance patterns between
sites far from application, i.e., polar and mountain sites,
particularly evident during the third sampling period (Figures
S11?S13).
Long-Range Atmospheric Transport (LRAT) of Pesti-
cides. The substances prone to long-range atmospheric
transport were identified using the samples collected at the
polar sites as well as those collected at high mountain sites from
free tropospheric air (see the Supporting Information for the
determination of free tropospheric conditions at each site).
Indeed, in the free troposphere, zonal and meridional transport
is more efficient due to higher wind speeds and longer
depositional lifetime.56
In the polar atmosphere, 19 pesticides were quantified,
including 15 for which this is the first evidence of their potential
to reach the Arctic. Out of these 19 pesticides, 12 were approved
for agricultural use in Europe in 2020. In particular, most of
these pesticides were quantified in the gas phase at the ZPO site,
Svalbard (78.9°N). 13 pesticides were found in the four samples
at mountain sites that were confirmed to have been collected
exclusively in free tropospheric air (Table S8). This included 10
approved for agricultural use and 10 that were also found at the
polar sites. Therefore, by combining the results from the polar
and free tropospheric air samples, 22 pesticides were identified
to be prone to LRAT (blue area in Figure 3), which included 15
approved for agricultural use in Europe.
Source regions, based on 30-day footprint analyses by the
FLEXPARTmodel, for the air collected from 28 to 30/04/2020
and 26?28/05/2020 at ZPO, Svalbard, are located in the North
Atlantic and the inner Arctic (Figure S2) and contained the
lowest number and concentrations of pesticides. Higher levels
were quantified in the air collected from 12 to 14/05/2020 at
ZPO, which originated from North America and the northern-
most agricultural regions of Russia (Figure S2). Similar behavior
has also been found for the two other polar sites, where higher
Figure 3. Pesticides identified as prone to long-range atmospheric transport (blue area, FT = free tropospheric), pesticides quantified in the planetary
boundary layer (white area), and pesticides never observed (gray area) ordered along model estimate of half-life in air.36 Not pictured is one pesticide
never observed, i.e., fluazinam, with a model-estimated half-life of 1956 h. Annual mean OH concentration of 7.5 × 105 cm?3 used for calculation of
half-life in air.
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numbers of pesticides were encountered in the samples, where
air masses were influenced by Scandinavia and the British Isles
(Figures S3 and S4). The origins of free tropospheric air
collected at mountain sites were all from continental Europe
(Figure S5).
Previous observations of more than 20 currently used
pesticides in the polar regions in recent years have highlighted
the LRAT potential of currently used pesticides10,22?24 (Table
S10). However, these studies have mainly focused on a limited
number of currently used pesticides. In this study, 19 pesticides
were found to be associated with LRAT at the polar sites. Out of
these, four substances, atrazine, chlorpyrifos, pendimethalin, and
triallate, had previously been reported in polar regions, whereas
we are establishing the first evidence of LRAT for 15 pesticides
that have previously not been encountered in these regions
(Figure 3). Three of these substances, atrazine, chlorpyrifos, and
diuron, are water policy-prioritized in the EU. The potential risk
for the environment and human health is also evidenced by the
fact that among the pesticides identified as prone to LRAT, 2 are
carcinogens, 6 are genotoxic, 10 are endocrine disruptors, and 9
are reprotoxic.10,57 In addition, the 22 long-range transported
pesticides belong to 16 different chemical classes57 and their
physicochemical properties range widely, i.e., saturation vapor
pressure ranging from 9.2 × 10?9 to 0.67 Pa with log KOW from
1.55 to 6.52 (Table S11), with chlorpyrifos, fenpropidin,
fenpropimorph, pendimethalin, S-metolachlor, and spiroxamine
potentially (logKow > 5) known to be bioaccumulative.
19
There was a considerable shift of the pesticides? gas/particle
partitioning from the continent to the Arctic, with a higher
gaseous fraction for 14 out of 15 pesticides observed at the polar
sites than at midlatitude sites. This trend was most prominent
for terbuthylazine, which was on average 99% in the particulate
phase at rural sites but >98% in the gaseous phase at polar sites.
The exception was triallate, which at one polar site was
quantified in the particulate phase only (>87%, Table S12). Our
observations suggest that pesticides which are predominantly
partitioning to the particulate phase in aerosols over Europe
tend to be found in the gaseous phase in the Arctic (Figure 2).
This pattern is consistent with previous studies, with pesticides
such as 2,6-dichlorobenzonitrile, chloroneb, dicofol, nitrapyrin,
and triallate observed only in the gas phase of Arctic air22,24
(Table S10), while in in this study, pesticides in continental
Europe preferentially partitioned to the particulate phase, as
suggested by the results from mountains and rural sites where
the gas phase was also collected.15
A preference for partitioning to the gas phase at polar sites can
be explained by low aerosol mass and surface concentrations and
the prevalence of hydrophilic particulate matter (PM)
components in particular seasalt.58 For example, at the central
European rural site KOS (Czech Republic), the concentration of
PM10 was 12.8 ?g m?3 on average during the study, while 4.3 ?g
m?3 was measured at the polar site ZPO, Svalbard.59 Organic
matter is a key constituent influencing the partitioning of
chemicals onto PM.60 In continental Europe, the fraction of
organic matter in PM is generally higher than that in the Arctic.
At the rural sites adjacent to agriculture, the particulate organic
carbon averaged 1.53 ?g m?3 (?12%), whereas at polar sites, it
wasmore than 10-fold lower, 0.11 ?gm?3 (?3%) on average. No
in-depth analysis of gas/particle partitioning is possible because
of the lack of particulate phase chemical composition data for
most of the sites. Another possible explanation could be
volatilization of CUPs frommelting snow, mixed into sample air
shortly before collection, i.e., before complete relaxation to
phase equilibrium. Volatilization from melting snow is expected
for organic substances, which within snowpacks would partition
significantly to the pore space,61 however, this does not apply for
the CUPs, which partitioning apparently shifted to the gas phase
(Table S12).
The three polar sites included in this study had similar
environmental conditions (temperature, PM concentration) but
are distanced from each other by >1000 km and were influenced
by different air masses (Figures S1?S5). Still, out of the 19
pesticides encountered at these sites, five were observed at more
than one polar site, which provides independent evidence of
long-range atmospheric transport. Moreover, we quantified 13
pesticides in free tropospheric air collected at three high
mountain sites, indicating that they are prone to LRAT. 11
pesticides identified at those mountain sites were also identified
at polar sites, thus providing strong evidence of their LRAT
potential.
Current Limitations Regarding Pesticide Environ-
mental Risk Assessments. Pesticide authorization in Europe
presupposes environmental risk assessment with criteria for
persistence, bioaccumulation potential, long-range transport
potential, and toxicity for soil and water. However, there is no
threshold value to consider a pesticide as persistent in the
atmosphere.27 The only parameter through which the
atmosphere is included in the risk assessment procedure is the
potential for long-range atmospheric transport. To assess this
potential, the atmospheric half-life is used as a proxy. For this,
only the reactivity with the OH radical in the gas phase is
considered, using global and annual mean OH radical
concentrations.62 A pesticide exhibiting a half-life higher than
2 days is considered as prone to LRAT.
However, all 22 pesticides identified as prone to LRAT in this
study have been estimated to have atmospheric half-lives shorter
than 2 days based on the model currently used in the risk
assessment36 (Table S11). But OH concentrations can be much
lower seasonally, at high latitudes, as well as during nighttime or
in the polar night.63 In these cases, degradation processes are
substantially reduced, with correspondingly longer effective
atmospheric half-lives and travel distances.24 For instance, the
atmospheric and total environmental lifetimes of atrazine are
almost 1 order of magnitude longer for midlatitude winter than
in summer64 and the characteristic travel distance (CTD) of
chlorpyrifos increases from 30 to 290 km with a 10-fold reduced
OH concentration.52 CTD is an indicator of a chemical?s long-
range transport potential in a generic multicompartment
environment under steady-state conditions and is influenced
by also lifetime in soil and water.52,65 It is defined as the distance
from the source region at which the concentration is reduced by
63%.66 Note that because of the generic nature of the underlying
multimedia model, CTD is not suitable to test substance fate or
should not be interpreted in absolute terms (km). CTDs of the
targeted pesticides are estimated mostly below 100 km (median
is 92 km) and are estimated even somewhat lower with a median
of 68 km for the substances identified as prone to LRAT,
suggesting that these chemicals are unlikely to reach remote
locations. The CTD values or their ranking do not correspond
with substances suggested from this or earlier studies to have
high long-range transport potential, with only one exception, i.e.,
thiacloprid (Figure S14 and Table S11).
Moreover, for pesticides transported in the particulate phase,
degradation is expected to be slower than in the gas phase due to
diffusion limitation in low-viscosity aerosol particles.33,67
Experiments on degradation rate coefficients with OH in the
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https://pubs.acs.org/doi/suppl/10.1021/acs.est.3c08488/suppl_file/es3c08488_si_001.pdf
https://pubs.acs.org/doi/suppl/10.1021/acs.est.3c08488/suppl_file/es3c08488_si_001.pdf
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particulate phase suggest atmospheric half-lives of weeks (given
global mean OH radical concentration).33,34 Oxidation is
particularly slow in aerosols transported at high altitudes or to
high latitudes and expectedly most relevant for moderately polar
pesticides such as carbamates, triazines, thiophosphoric acid
esters, phenols, and anilines.34,67 As confirmed in this study,
pesticides tend to have higher particle-bound mass fractions in
continental air than in polar air, and their persistence in air is
therefore likely underestimated. This aspect is neglected by the
current risk assessment practice.
Furthermore, the effective atmospheric lifetime of semi-
volatiles resisting degradation in soils and surface water can be
much longer than the residence time in air based on degradation
kinetics because of several cycles of revolatilization and
deposition enhancing the LRAT potential (multihopping).28
In addition to the lack of information about active ingredients,
the influence of application methods, formulants, and adjuvants
on CUP emissions is not well known. While aerial application is
banned in Europe, spraying of soil and plant,12 volatilization,68,69
and also pellet application to soil and seed treatment contribute
to pesticide emissions.70 Formulants and adjuvants are used to
improve the effectiveness of application but can modify their
effective vapor pressure and atmospheric half-lives.71 A recent
experimental study suggested that the reactivity of the
chlorpyrifos with OH radicals was different in a commercial
formulation than that of the substance alone.35
This study shows the limits of the risk assessment in place in
the regulatory process on the atmospheric fate of pesticides and,
in particular, their potential for LRAT, by providing empirical
evidence in direct contrast to current model predictions. There
is a real need to revise the current methods used for
environmentally relevant conditions (different temperature
and/or OH concentrations) as well as to obtain more
experimental data on atmospheric degradability of pesticides
including pesticide formulations and preparations, in addition to
data from monitoring studies. Currently, the framework does
not consider partitioning into the particulate phase or slowed
degradation in soil/water during the multihopping. More
realistic modeling is extremely important if we want to ensure
that the pesticides authorized for agricultural use in Europe (and
elsewhere) do not contaminate the environment and pose health
risks hundreds of thousands of kilometers away from the source
areas.
? ASSOCIATED CONTENT
*si Supporting Information
The Supporting Information is available free of charge at
https://pubs.acs.org/doi/10.1021/acs.est.3c08488.
Materials and methods, map of the 29 sites, 30-days
footprint sensitivities and 10-day backward trajectories
(FLEXPART model), CUPs physico-chemical parame-
ters, detailed site results, gas-particle partitioning,
hierarchical cluster analysis, sampling methodology,
land-use analysis, internal standards and chemical
analyses information, recoveries, information on previous
CUPs found in Arctic and high-mountain sites (PDF)
? AUTHOR INFORMATION
Corresponding Authors
Céline Degrendele ? Faculty of Science, RECETOX, Masaryk
University, Brno 602 00, Czech Republic; Laboratory of
Chemistry and Environment (LCE), CNRS, Aix-Marseille
University, Marseille 13003, France; Present Address: Celine
Degrendele; now unemployed; Email: celine.degrendele@
recetox.muni.cz
Gerhard Lammel ? Faculty of Science, RECETOX, Masaryk
University, Brno 602 00, Czech Republic; Multiphase
Chemistry Department, Max Planck Institute for Chemistry,
Mainz 55128, Germany; orcid.org/0000-0003-2313-
0628; Email: gerhard.lammel@recetox.muni.cz
Authors
Ludovic Mayer ? Faculty of Science, RECETOX, Masaryk
University, Brno 602 00, Czech Republic; orcid.org/0000-
0002-6049-0860
Petr Senk? Faculty of Science, RECETOX,Masaryk University,
Brno 602 00, Czech Republic
Jir? Kohoutek ? Faculty of Science, RECETOX, Masaryk
University, Brno 602 00, Czech Republic
Petra Pr?bylová ? Faculty of Science, RECETOX, Masaryk
University, Brno 602 00, Czech Republic
Petr Kukuc?a ? Faculty of Science, RECETOX, Masaryk
University, Brno 602 00, Czech Republic
Lisa Melymuk ? Faculty of Science, RECETOX, Masaryk
University, Brno 602 00, Czech Republic
Amandine Durand ? Laboratory of Chemistry and
Environment (LCE), CNRS, Aix-Marseille University,
Marseille 13003, France
Sylvain Ravier ? Laboratory of Chemistry and Environment
(LCE), CNRS, Aix-Marseille University, Marseille 13003,
France
Andres Alastuey ? Spanish Research Council (CSIC), Institute
of Environmental Assessment and Water Research (IDAEA),
Barcelona 08034, Spain; orcid.org/0000-0002-5453-
5495
Alex R. Baker ? Centre for Ocean and Atmospheric Sciences,
University of East Anglia, Norwich NR4 7TJ, United Kingdom
Urs Baltensperger ? Laboratory of Atmospheric Chemistry,
Paul Scherrer Institute, Villigen 5232, Switzerland
Kathrin Baumann-Stanzer ? GeoSphere Austria, Wien 1190,
Austria
Tobias Biermann ? Centre for Environmental and Climate
Research, Lund University, Lund 223 62, Sweden
Pernilla Bohlin-Nizzetto ? Norwegian Institute for Air
Research (NILU), Kjeller 2007, Norway
Darius Ceburnis ? School of Natural Sciences and Centre for
Climate and Air Pollution Studies, Ryan Institute, University of
Galway, Galway H91 CF50, Ireland; orcid.org/0000-
0003-0231-5324
Sébastien Conil ? DRD/GES Observatoire Pérenne de
l?Environnement, ANDRA, Bure 55290, France
Cédric Couret ? German Environment Agency (UBA),
Zugspitze 82475, Germany
Anna Degórska ? Institute of Environmental Protection,
National Research Institute, Warsaw 02-170, Poland
Evangelia Diapouli ? National Centre of Scientific Research
?Demokritos?, Institute of Nuclear Radiological Science
Technology, Energy and Safety, ENRACT, Agia Paraskevi
15310, Greece
Sabine Eckhardt ? Norwegian Institute for Air Research
(NILU), Kjeller 2007, Norway
Konstantinos Eleftheriadis ? National Centre of Scientific
Research ?Demokritos?, Institute of Nuclear Radiological
Science Technology, Energy and Safety, ENRACT, Agia
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Paraskevi 15310, Greece; orcid.org/0000-0003-2265-
4905
Grant L. Forster ? Centre for Ocean and Atmospheric Sciences
and National Centre for Atmospheric Sciences, University of
East Anglia, Norwich NR4 7TJ, United Kingdom
Korbinian Freier ? Bavarian Environment Agency, Augsburg
86179, Germany
Franco?is Gheusi ? Laboratoire d?Aérologie, CNRS/IRD,
University of Toulouse, Toulouse 31400, France
Maria I. Gini ? National Centre of Scientific Research
?Demokritos?, Institute of Nuclear Radiological Science
Technology, Energy and Safety, ENRACT, Agia Paraskevi
15310, Greece
Heidi Hellén ? Finnish Meteorological Institute, Helsinki
00560, Finland; orcid.org/0000-0001-7022-3857
Stephan Henne ? Swiss Federal Laboratories for Materials
Science and Technology (Empa), Dübendorf 8600,
Switzerland
Hartmut Herrmann ? Atmospheric Chemistry Department,
Leibniz Institute for Tropospheric Research (TROPOS),
Leipzig 04318, Germany
Adéla Holubová Smejkalová ? National Atmospheric
Observatory Kosetice, KoseticeCzech Hydrometeorological
Institute, Kosetice 395 01, Czech Republic
Urmas Hõrrak? Institute of Physics, University of Tartu, Tartu
50411, Estonia
Christoph Hüglin ? Swiss Federal Laboratories for Materials
Science and Technology (Empa), Dübendorf 8600,
Switzerland
Heikki Junninen ? Institute of Physics, University of Tartu,
Tartu 50411, Estonia
Adam Kristensson ? Department of Physics, Lund University,
Lund 223 63, Sweden
Laurent Langrene ? DRD/GES Observatoire Pérenne de
l?Environnement, ANDRA, Bure 55290, France
Janne Levula ? Institute for Atmospheric and Earth System
Research (INAR), University of Helsinki, Helsinki 00100,
Finland
Marie Lothon ? Laboratoire d?Aérologie, CNRS/IRD,
University of Toulouse, Toulouse 31400, France
Elke Ludewig ? GeoSphere Austria, Wien 1190, Austria
Ulla Makkonen ? Finnish Meteorological Institute, Helsinki
00560, Finland
Jana Matejovic?vá ? Slovak Hydrometeorological Institute,
Bratislava 833 15, Slovakia
NikolaosMihalopoulos?Department of Chemistry, University
of Crete, Heraklion 715 00, Greece
Veronika Mináriková ? Slovak Hydrometeorological Institute,
Bratislava 833 15, Slovakia
Wolfgang Moche ? Environment Agency Austria, Wien 1090,
Austria
SteffenM. Noe? Institute of Forestry and Engineering, Estonian
University of Life Sciences, Tartu 51014, Estonia
Noemí Pérez ? Spanish Research Council (CSIC), Institute of
Environmental Assessment and Water Research (IDAEA),
Barcelona 08034, Spain
Tuukka Petäjä ? Institute for Atmospheric and Earth System
Research (INAR), University of Helsinki, Helsinki 00100,
Finland
Véronique Pont ? Laboratoire d?Aérologie, CNRS/IRD,
University of Toulouse, Toulouse 31400, France
Laurent Poulain ? Atmospheric Chemistry Department,
Leibniz Institute for Tropospheric Research (TROPOS),
Leipzig 04318, Germany
Etienne Quivet ? Laboratory of Chemistry and Environment
(LCE), CNRS, Aix-Marseille University, Marseille 13003,
France
Gabriela Ratz ? Bavarian Environment Agency, Augsburg
86179, Germany
Till Rehm ? Environmental Research Station Schneefernerhaus
(UFS), Zugspitze 82475, Germany
Stefan Reimann ? Swiss Federal Laboratories for Materials
Science and Technology (Empa), Dübendorf 8600,
Switzerland
Ivan Simmons ? UK Centre for Ecology and Hydrology,
Penicuik EH260QB, United Kingdom
Jeroen E. Sonke ? Géosciences Environnement Toulouse,
CNRS/IRD, University of Toulouse, Toulouse 31400, France;
orcid.org/0000-0001-7146-3035
Mar Sorribas ? Atmospheric Sounding Station El Arenosillo,
National Institute for Aerospace Technology (INTA), Huelva
21130, Spain
Ronald Spoor ? National Institute for Public Health and the
Environment (RIVM), Bilthoven 3721 MA, the Netherlands
Daan P. J. Swart ? National Institute for Public Health and the
Environment (RIVM), Bilthoven 3721 MA, the Netherlands
Vasiliki Vasilatou ? National Centre of Scientific Research
?Demokritos?, Institute of Nuclear Radiological Science
Technology, Energy and Safety, ENRACT, Agia Paraskevi
15310, Greece
Henri Wortham ? Laboratory of Chemistry and Environment
(LCE), CNRS, Aix-Marseille University, Marseille 13003,
France
Margarita Yela ? Atmospheric Sounding Station El Arenosillo,
National Institute for Aerospace Technology (INTA), Huelva
21130, Spain
Pavlos Zarmpas ? Department of Chemistry, University of
Crete, Heraklion 715 00, Greece
Claudia Zellweger Fäsi ? Swiss Federal Laboratories for
Materials Science and Technology (Empa), Dübendorf 8600,
Switzerland
Kjetil Tørseth ?Norwegian Institute for Air Research (NILU),
Kjeller 2007, Norway
Paolo Laj ? Institut des Géoscience de l?Environnement,
University Grenoble Alpes, Grenoble 38058, France; Institute
for Atmospheric and Earth System Research (INAR),
University of Helsinki, Helsinki 00100, Finland
Jana Klánová ? Faculty of Science, RECETOX, Masaryk
University, Brno 602 00, Czech Republic
Complete contact information is available at:
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Author Contributions
####L.M. and C.D. contributed equally to this work. Con-
ceptualization and methodology: C.D. and G.L. Validation:
L.M., P.S., A.Du., and C.D. Formal analysis: L.M., P.S., P.K.,
A.Du., S.Ra., K.B.-S., S.E., F.G., S.H., and J.M. Investigation:
L.M., J.Ko., P.S., P.K., P.P., S.Ra., A.Du., G.L., C.D., K.B.-S., S.E.,
S.H., F.G., J.E.S., J.M., P.B.-N., C.C., DC. S.C., A.De., G.L.F.,
M.I.G., V.V., K.E., U.H., H.J., A.K., P.L., E.L., U.M., V.M., L.P.,
M.S., and U.B. Writing?original draft: L.M., C.D., and G.L.
Writing?review and editing: L.M., G.L., L.E.M., and U.B. All
visualization: L.M. and S.E. Supervision: G.L. and C.D. Project
Environmental Science & Technology pubs.acs.org/est Article
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administration: G.L., J.Kl., and C.D. Funding acquisition: J.Kl.,
G.L., P.P., and H.W. The article was written through
contributions of all authors. All authors have given approval to
the final version of the article.
Funding
This work was supported by the European Union?s Horizon
2020 research and innovation program (857560); the Czech
Ministry of Education, Youth and Sports through RECETOX
Research Infrastructure (LM2023069), ACTRIS-CZ RI
(LM2023030) and CETOCOEN EXCELLENCE
(CZ.02.1.01/0.0/0.0/17_043/0009632); the Brno City Munic-
ipality and the South Moravian Centre for International
Mobility (JCMM, fellowship award to L.M.); the Czech Science
Foundation (20?07117S); the Estonian Research Council
(PRG714, PRG1674); the General Secretariat of Research and
Innovation of the Greek Ministry of Development and
Investments, Public Investment Program, through the National
Network on Climate Change and Its Impacts; the Norwegian
Fram Center (CLEAN-FRAM) and COPE (NFR #28114); and
the Swedish Research Council (ACTRIS_SE RI 2021?00177).
This publication reflects only the author?s view and the
European Commission is not responsible for any use that may
be made of the information it contains.
Notes
The authors declare no competing financial interest.
? ACKNOWLEDGMENTS
The authors thank Yannick Bezombes, Jean-Marc Fort, Achim
Grüner, Hilja Iher, Marcin Jackowicz-Korczynski, Olav Lien,
Reidar Lyngra, Helge T. Markussen, Eric Pique, René Rabe, and
Tomás ? Istok for on-site help, Cecilia Akselsson, Jenny Kreuger,
and Cornelius Zetzsch for discussion, and Franz Conen,
Gabriele Frank, Radovan Krejci, Thomas Werner, Paul Zieger,
and MeteoSwiss for supporting field data. The study received
support from the National Facilities of the ACTRIS (Aerosol,
Clouds and Trace gases Research Infrastructure) and EMEP
(Co-operative Programme for Monitoring and Evaluation of the
Long-range Transmission of Air Pollutants in Europe) network
of platforms. The ARN and MSY sites were supported by the
European Regional Development Fund in Spain related to
LifeWatch ERIC (INDALO, LIFEWATCH-2019-04-AMA-
01). The HTM site was supported by the Swedish Environ-
mental Protection Agency, Lund University, and the Swedish
Research Council through ICOS Sweden. The MEL site was
supported by the H2020 RIs ACTRIS 262254 and ACTRIS-2
654109. The MHD site was supported by EPA Ireland through
the Atmosphere Chemistry and Climate Change (AC3)
network. The PDM site received technical support from the
UMS 831 Pic du Midi observatory team and the Pyrenean
Platform for Atmospheric Observations (P2OA), funded by
CNRS-INSU. The SME and THK sites were supported by the
Estonian Environmental Observatory (KKOBS 2014-
2020.4.01.20-0281) and the Estonian Environmental Agency
and ACTRIS IMP (871115). The WEY site was supported by
the Natural Environmental Research Council?s Atmospheric
Measurement and Observat ion Faci l i ty (AMOF,
AMF_20022020084418).
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