Dispersion of Short- and Medium-Chain Chlorinated Paraffins (CPs

Nov 2, 2016 - Chlorinated paraffin (CP) production is one important emission source for short- and medium-chain CPs (SCCPs and MCCPs) in the environme...
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Dispersion of short- and medium-chain chlorinated paraffins (CPs) from a CP production plant to the surrounding surface soils and coniferous leaves Jiazhi Xu, Yuan Gao, Haijun Zhang, Faqiang Zhan, and Jiping Chen Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.6b03595 • Publication Date (Web): 02 Nov 2016 Downloaded from http://pubs.acs.org on November 2, 2016

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Environmental Science & Technology

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Dispersion of short- and medium-chain chlorinated

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paraffins (CPs) from a CP production plant to the

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surrounding surface soils and coniferous leaves

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Jiazhi Xu,

5 6 7 8

†,‡



†,*

Yuan Gao, Haijun Zhang,

Faqiang Zhan,

†,‡

Jiping Chen†

,*



Key Laboratory of Separation Science for Analytical Chemistry, Dalian Institute of Chemical Physics, Chinese Academy of Sciences, Dalian, 116023, China ‡

University of Chinese Academy of Sciences, Beijing 100049, China

TOC/Abstract Art Atmospereic dispersion

CP production

SCCPs CP storage

MCCPs

deposition

9 10 11 12 13 14 15

*Corresponding Authors

16

Phone: +86-411-8437-9972, fax: +86-411-8437-9562; e-mail: [email protected].

17

Phone/fax: +86-411-8437-9562; e-mail: [email protected].

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ABSTRACT

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Chlorinated paraffin (CP) production is one important emission source for short- and

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medium-chain CPs (SCCPs and MCCPs) in the environment. In this study, 48 CP congener

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groups were measured in the surface soils and coniferous leaves collected from the inner

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and surrounding environment of a CP production plant that run has been operation for more

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than 30 years to investigate the dispersion and deposition behavior of SCCPs and MCCPs.

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The average concentrations of the sum of SCCPs and MCCPs in the in-plant coniferous

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leaves and surface soils were 4548.7 ng g–1 dry weight (dw) and 3481.8 ng g–1 dw, which

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were 2-fold and10-fold higher than those in the surrounding environment, respectively. The

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Gaussian air pollution model explained the spatial distribution of CPs in the coniferous

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leaves, whereas the dispersion of CPs to the surrounding surface soils fit the Boltzmann

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equation well. Significant fractionation effect was observed for the atmospheric dispersion

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of CPs from the production plant. CP congener groups with higher octanol-air partitioning

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coefficients (KOA) were more predominant in the in-plant environment, whereas ones with

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lower KOA values had the elevated proportion in the surrounding environment. A radius of

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approximately 4-km from the CP production plant was influenced by the atmospheric

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dispersion and deposition of CPs.

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INTRODUCTION

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Chlorinated paraffins (CPs) are complex mixtures of polychlorinated n-alkanes with

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chain lengths between 10 and 30 carbon atoms, containing thousands of congeners, isomers,

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enantiomers and diastereomers.1,2 They are widely used as flame retardants and plasticizers

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in plastics and sealants and as additives in metal-working fluids, lubricants, paints and

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coatings.3 The commercial CP formulations are sub-divided according to their carbon chain

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length into three categories: short-chain CPs (SCCPs, C10–13), medium-chain CPs (MCCPs,

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C14–17) and long-chain CPs (LCCPs, C>17). Among them, SCCPs have been listed as a group

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of candidate persistent organic pollutants (POPs) because of their environmental ACS Paragon Plus Environment

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persistence, long-range transport potential, tendency to bioaccumulate, and high toxicity to

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aquatic organisms.4–7 MCCPs should also be of concern because of their similarities to

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SCCPs with respect to chemical and physical properties.8, 9

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In the last decade, SCCPs and MCCPs have been ubiquitously found in natural

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environmental compartments such as air, water, soil and sediment.10–12 However, the

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understanding of how CPs are released into the environment is still limited. CPs cannot be

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formed naturally, and thus, almost all SCCPs and MCCPs in the environmental matrix are

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emitted from the CP product life cycle, including the production, storage, transport and

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industrial use of CPs, as well as the routine use and waste-disposal of products containing

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CPs.13,14 An emission inventory prediction indicated that the total emission of SCCPs into

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the environment in China was as high as 1789 tons in 2011.15 Therefore, it is urgent to

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investigate the pollution levels of SCCPs and MCCPs in the environments surrounding

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important sources, along with their potential ecological risks.

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CP production is regarded as one important source of SCCPs in the environment. 15, 16 In

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China, a larger quantity of commercial CP mixtures were produced without been classified

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by the carbon chain length. However, the survey data on the emission levels of SCCPs and

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MCCPs from the CP production plant and their levels in the surrounding environment are

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still scarce. CPs are produced by the direct free radical reaction of chlorine with selected

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n-alkanes from petroleum distillation, in which almost no wastewater is discharged and

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only a small volume of waste gas is emitted after a cleaning treatment. Therefore, the

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emission of SCCPs and MCCPs from a CP production plant should mainly occur through

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volatilization and dust drift. The volatilized CPs can partition between the gaseous and

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particulate phases in the atmosphere, which is an important process that affects the

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deposition, degradation and long-range transportation. The wind-blowing dust and larger

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particles bound with CPs tend to be deposited in the ambient environment, which would

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result in the higher pollution levels of SCCPs and MCCPs in the soils surrounding the CP ACS Paragon Plus Environment

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production plant according to Level III fugacity modeling.17 Coniferous leaves, with

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lipid-rich cuticle and stomata structures on its surfaces, are found to have a higher ability to

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trap and accumulate CPs,18–20 and therefore they can be employed as good indicators of

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pollution dispersion of SCCPs and MCCPs from the CPs production plant.

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Although the atmospheric occurrence and deposition of semi-volatile hydrophobic

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organic pollutants (HOCs) in the industrial, urban and suburban sites have been extensively

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investigated, only a few studies modeled the atmospheric dispersion of semi-volatile HOCs

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from the point sources and metropolitan areas.21–23 It was found that the one-dimensional

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Gaussion diffusion model could explain the long-range atmospheric transport of

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semi-volatile HOCs from urban area to the surrounding environment, which was mainly

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driven by wind.21,

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dispersion and the rapid deposition of particle-associated chemical pollutants might be not

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negligible. To our knowledge, the dispersion behavior of semi-volatile HOCs from a single

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non-combustion point source in small scale has been never specifically characterized under

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well-controlled environmental conditions.

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However, in the small area near the pollution source, the lateral

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In the present study, surface soil and coniferous leaf samples were collected from the

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inner and surrounding environment of a CP production plant in China with a history of CP

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production that exceeded 30 years. The test CP production plant is far away from urban

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areas and other factories. The objectives of this study were to characterize the

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environmental pollution caused by the production of CPs, and to explore the dispersion and

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deposition mechanism of CPs from the CP production plant to the surrounding environment.

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The obtained results will also help understand the short-range dispersion behavior of other

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semi-volatile HOCs from a point source mainly via atmospheric transport.

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EXPERIMENTAL SECTION

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Chemicals and Materials. The standard stock solutions of the SCCPs and MCCPs with

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different chlorine contents were obtained from Dr. Ehrenstorfer GmbH (Augsburg, ACS Paragon Plus Environment

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Germany). An internal standard solution of 13C6-δ-hexachlorocyclohexane (13C6-δ-HCH) in

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n-nonane (100 µg/L) and an recovery standard solution of

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(13C10-trans-CD) in n-nonane (100 µg/L) were both provided by Cambridge Isotope

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Laboratories (Andover, MA, USA). Silica gel (63–100 µm) and basic alumina (Activity

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Super I, 63–200 µm, pH 10) were purchased from Sunchrom (Friedrichshafen, Germany)

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and MP Biomedicals (Eschwege, Germany), respectively. All of the solvents, including

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n-hexane, dichloromethane and n-nonane, were of pesticide residue grade and were

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obtained from J. T. Baker (Phillipsburg, USA).

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Basic Information on the CP Production Plant. The investigated CP production

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plant is located in Dalian city, northeast China. It has a history of CP production that

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exceeds 30 years, and the annual CP production is approximately 50,000 tons. CP mixtures

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are produced from C9–28-n-alkanes using the method of photochemical-thermal chlorination,

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in which no wastewater or solid waste is emitted. The hydrogen chloride produced from

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chlorination together with the unreacted chlorine gas is recovered by a two-stage falling

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film absorber combined with an alkali absorption tower, and then the tail gas is emitted to

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the atmosphere. Commercial CP mixtures, CP-42 (CPs with a chlorine content of 42%),

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CP-52 and CP-70, are mainly produced. SCCPs in these industrial CP mixtures, sampled

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from the plant in 2014, were analyzed using carbon skeleton gas chromatography method

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described by Koh et al.

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1.3 mg/g, 114.0 mg/g and 200.5 mg/g in CP-42, CP-52 and CP-70, respectively.

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Sample Collection. A total of 50 environmental samples, including 25 surface soil

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samples, 16 pine (Pinus thunbergii) needle samples, 7 cypress (Sabina chinensis) leaf

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samples and 2 spruce (Picea koraiensis) needle samples, were collected from the inner and

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surrounding environment of the investigated CP production plant from October 2013 to

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April 2014. The spatial distribution of the sampling sites is shown in Figure 1. The soil

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samples were collected from uncultivated land. Five separate soil subsamples at a depth of

24

13

C10-trans-chlordane

The total SCCP (ΣSCCPs) concentrations were determined to be

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0–5 cm were taken using a stainless steel scoop and were then mixed together to form a

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composite sample. Pine and spruce needles as well as cypress leaves were collected at the

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heights of 2–4 m and 0.7–1.2 m above the ground level, respectively. Several small

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branches were cut off of a tree using steel scissors, and all of the coniferous leaves on the

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branches were collected without distinguishing ages. The coniferous leaves were sampled

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from 4–6 trees and then mixed to form a composite sample. The collected samples were

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packed in pre-cleaned self-sealing polyethylene bags with zippers, and transported to the

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laboratory. Surface soil samples were freeze-dried, ground and homogenized by passing a

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stainless steel 60-mesh sieve. Leaf samples were freeze-dried and ground under a liquid

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nitrogen atmosphere. The lyophilized samples of the surface soils and tree leaves were

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stored in pre-cleaned brown glass bottles at –20 °C until analysis.

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Sample Extraction and Cleanup. After spiking with an aliquot of the

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internal standard, the surface soil and tree leaf samples were Soxhlet extracted with 250 mL

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of hexane/dichloromethane (1:1, v/v) for 20 h. The lipids in the leaf extracts and the

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sulfur-containing compounds in the soil extracts were removed using a concentrated

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sulfuric acid treatment and activated copper powder treatment, respectively. The

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concentrated extracts were subjected to a successive cleanup procedure, multi-layer silica

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gel column and subsequent basic alumina column. The clean extract was gradually

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transferred to a micro-vial, evaporated to near dryness with a nitrogen stream, and then

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re-dissolved in 40 µL of the recovery standard solution for instrumental analysis. The

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detailed information on the sample extraction and cleanup can be seen in the Supporting

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Information (SI).

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C6-δ-HCH

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21

22 W

E

16

S

15 14 12 13

7 9

17

10

8 5

1 3

2

19 4

6

11

Surface Soil Coniferous leaves

18 23

20 25

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Figure 1. Map of the study areas and sampling sites. ☆ represents the location of the CP production

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plant.

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Instrumental Analysis and Quantification. Measurements of the SCCPs and MCCPs

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were carried out on a Shimadzu GCMS-QP2010 plus system operating in ECNI mode with

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a splitless injection. The GC was equipped with a DB-5 capillary column (15 m × 0.25 mm

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i.d. × 0.25 µm film thickness, J&W Scientific, U.S.). The temperature program was set as

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follows: initially 100 °C for 2 min, ramped to 260 °C at 20 °C/min and held for 2 min, and

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then ramped to 310 °C at 30 °C/min and held for 12 min. Helium and methane (99.995%

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purity) were used as the carrier gas and reagent gas, respectively. The ion source, transfer

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line and injector temperatures were kept at 200 °C, 280 °C and 280 °C, respectively.

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Selected ion monitoring (SIM) mode was applied for the detection of the most abundant

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signal within the isotope clusters of the [M−Cl]− fragment ion for each CP congener group.

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A total of 48 CP congener groups with carbon chain lengths of 10−17 and chlorine atom

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numbers of 5−10 were monitored. Comparisons of the retention time, signal profile, and

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corrected isotope ratio between the samples and standards were conducted for the

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identification of possible interferences from the CPs themselves and other interfering

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compounds. For each sample, two individual injections were executed for the detection of

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the SCCPs and MCCPs, respectively.

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The signal response interferences between the SCCP and MCCP congener groups were

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deducted using the calculation methods described by Zeng et al.,25 with minor modification.

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The corrected chromatographic peak areas of the SCCP and MCCP congener groups were

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used for the quantifications according to the procedure described by Reth et al..26 A linear

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correlation was obtained between the total response factors of reference CP mixture

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standards and their calculated chlorine contents, which was allowed to compensate the

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effect of the chlorine content differences on the total response factors between the CPs in

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the environmental samples and the reference CP mixture standards. The detailed

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instrumental analytical method and quantification are shown in the SI.

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The total organic carbon (TOC) content in the surface soils was analyzed using the

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high-temperature combustion method with a total organic carbon analyzer (Vario TOC

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cube, Elementar, Germany). Each sample was pretreated with 1 mol/L HCl to remove the

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carbonate residues for the TOC measurements. The lipid content in the leaf samples was

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determined by a gravimetric method (extraction with petroleum ether).

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Quality Assurance and Quality Control. All of the glassware was rinsed in triplicate

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with n-hexane before use. The procedural and solvent blanks were included in each batch of

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5 samples. No CPs was detected in the procedural and solvent blanks. The procedural

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blanks spiked with a small quantity of SCCP and MCCP mixture standards were used to

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determine the method detection limits (MDL), which was calculated as three times the

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standard deviation at 6 time measurements. The MDL values for the total SCCPs (ΣSCCPs)

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were estimated to be 1.62 ng g–1 dry weight (dw) for surface soils and 8.09 ng g–1 dw for

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leaf samples; and the corresponding values for the total MCCPs (ΣMCCPs) were estimated

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to be 2.34 ng g–1 dw for surface soils and 11.70 ng g–1 dw for leaf samples. The recoveries

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of the internal standard

13

C6-δ-HCH in all of the samples were in the range of

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65.7%–118.6%. The reported data in this study were not blank and surrogate recovery

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corrected. As for the samples in triplicate, the relative standard deviations for the

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quantification of the total SCCPs and total MCCPs were both < 18%.

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Data Processing. Partial least squares discriminant analysis (PLS-DA) was applied with

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unit variance (UV) scaling to characterize the congener group distribution of the SCCPs

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and MCCPs. Concentrations that were below the MDL values were assigned a value of

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zero before conducting PLS-DA. All statistics and drawings were conducted using the

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following software: ArcGIS 10.3 (Esri Inc., USA), Origin 8.5 (OriginLab Inc., USA),

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SigmaPlot 12.0 (SigmaPlot Software Inc.), SIMCA-P11.5 (Umetrics, Sweden), Surfer 11

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(Golden Software Inc.) and SPSS PASW (SPSS Inc., Chicago, IL).

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RESULTS AND DISCUSSION

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Concentrations and Spatial Distribution of the SCCPs and MCCPs in

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Coniferous Leaves. Coniferous leaves can serve as a passive air sampler that integrates

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the gas and particulate phase associated pollutants over the years and provides averaged

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information about the contamination level.27 In this study, SCCPs and MCCPs were found

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at quantifiable concentrations in all of the coniferous leaf samples. The concentrations were

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in the ranges of 218.7–2196.6 ng g–1 dw for the ΣSCCPs, 337.8–4388.4 ng g–1 dw for the

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ΣMCCPs, and 745.8–6585.0 ng g–1 dw for the sum of the SCCPs and MCCPs (Table 1 and

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Table S3), respectively. The highest concentrations of the ΣSCCPs (2196.6 ng g–1 dw) and

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ΣMCCPs (4388.4 ng g–1 dw) were both detected in the cypress leaves sampled at site 2

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inner the CP production plant (Figure 1 and Table S3). Spruce needles from sampling site 3,

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located approximately 500 m away from the CP plant, also showed higher concentrations of

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ΣSCCPs (1742.2 ng g–1) and ΣMCCPs (3711.1 ng g–1). The ΣSCCP and ΣMCCP

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concentrations in the other coniferous leaf samples from the CP production plant

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surroundings were in the ranges of 218.7–1441.2 ng g–1 dw (average: 653.7 ng g–1 dw) and

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were much higher than those in spruce needles in the European Alps (total CPs level:

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26–450 ng g–1 dw)18 and those in most Masson pine needle samples from Shanghai

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(geometric means: 63.7 ng g–1 dw for ΣSCCPs, 677 ng g–1 dw for ΣMCCPs),20 while they

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are comparable to those in pine needles from Beijing (ΣSCCPs: 400–4010 ng g–1 dw).19

219 220

Table 1. The ΣSCCP and ΣMCCP concentrations (range and mean in parenthesis) in the

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collected surface soils and coniferous leaves

Samples

In-plant coniferous leaves

Ambient coniferous leaves

In-plant surface soils

Ambient surface soils

No

Total SCCPs

Total MCCPs

SCCPs + MCCPs

.

(ng/g dw)

(ng/g dw)

(ng/g dw)

1280.9–2196.6

1231.5-4388.4

2512.4–6585.0

(1738.7)

(2809.9)

(4548.7)

218.7–1742.2 (701.0)

337.8–3711.1 (1677.7)

745.8–5453.3 (2378.7)

1018.4–1824.4

2028.0–2074.8

3093.2–3870.4

(1421.4)

(2051.4)

(3481.8)

24.8–481.6 (141.9)

19.3–1460.6 (199.4)

63.8–1884.4 (341.4)

2

23

2

23

222 223

The extractable lipid contents in the collected coniferous leaves ranged from 4.1% to

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9.8% with an average of 7.4%. The lipid contents in the cypress leaves (average: 8.2%)

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were found to be significantly higher than those in pine needles (average: 7.0%).

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Nevertheless, there was no significant difference between the CP concentrations in these

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two types of leaves sampled from adjacent sites. This suggested that the accumulation

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levels of the CPs in the coniferous leaves from the environment surrounding the CP

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production plant should mainly depend on the pollution diffusion gradient and rely less on

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the lipid content in the coniferous leaves.

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The spatial distributions of the SCCPs and MCCPs in the coniferous leaves were also

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presented in Figure 2. Within a 1.5-km radius of the production plant, the concentrations of

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ΣSCCPs and ΣMCCPs in the coniferous leaves both showed a rapidly decreasing tendency

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from the center of the CP production plant to the surrounding environment. The pine

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needles sampled from sites 7 and 22, located near the small residential areas, showed an

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abruptly elevated concentration of ΣMCCPs (Figure 1 and Table S3), and thus, resulted in

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two unexpected pollution dispersion sources in the iso-concentration map (Figure 2b). One

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was located approximately 1.6 km northwest of the CP production plant and another was

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located approximately 5.4 km north of the CP production plant. The pollution dispersion

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from the CP production plant could not provide an adequate explanation for the abruptly

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elevated concentrations, and therefore, the most probable cause was the incidental pollution

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as a result of residential activity.

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244 245

Figure 2. Iso-concentration maps of CPs in the inner and surrounding environment of the

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tested CP production plant. a: ΣSCCPs in coniferous leaves, b: ΣMCCPs in coniferous leaves, c:

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the sum of SCCPs and MCCPs in coniferous leaves, d: ΣSCCPs in surface soils, e: ΣMCCPs in

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surface soils, and f: the sum of SCCPs and MCCPs in surface soils.

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In environmental science, Gaussian air pollution models are successfully employed to

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predict the short-range dispersion of both gaseous pollutants and particles from a point

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source with simplifying assumptions that landscape is approximately flat and unobstructed,

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and only dry deposition occurs.28–31 In this study, there were 3 low hills in the sampling

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area. Nevertheless, the altitude differences for all of the sampling sites were less than 20 m.

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Therefore, the dispersion process of the CPs from the production plant to the surrounding

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coniferous leaves should essentially agree with the simplifying assumptions of Gaussian air

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pollution models.

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The coniferous leaves generally accumulated CPs from the atmosphere for 0.5–3 years.

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During this period, the atmospheric stability and downwind speed often varies according to

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the weather. In sampling area, the static wind weather (wind speed < 0.5 m/s) accounts for

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about 140–180 days per year. The average wind speed is about 3.3 m/s, and the wind

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directions occurred at almost all the orientations (Figure S1). Therefore, the lateral diffusion

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and the wind speed can both exert the significant influence on the atmospheric dispersion of

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CPs from the CPs production plant in small scale. In addition, the emission rate of CPs

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(mainly via volatilization) also largely changed with the production activity intensity and

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weather temperature. When considering that the accumulation of CPs in coniferous leaves

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results from the long-term atmospheric deposition, the parameters reflecting dispersion,

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wind speed and emission rate can be assumed to constants. Therefore, the Gaussian air

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pollution model can be simplified to

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 1 y Ci = C 0 + A × exp  −   2  σ y 

   

2

   

(4)

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where Ci and Co are the actual and background concentrations of CPs in coniferous leaves,

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respectively; y is the lateral distance from the source, and σy is a lateral dispersion

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coefficient; A is a constant, reflecting the overall average results of vertical dispersion,

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lateral dispersion, wind speed and emission rate. The detailed derivation of eq. 1 is shown

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in Supporting Information.

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The derived Gaussian air pollution model (eq. 1) well fit the relationship between CP

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concentrations in the coniferous leaf samples and the distances of the sampling sites from

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the center of the production plant (Figure 3a, Table S5). The fitted data were all

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significantly (P < 0.01) correlated to the determined data for the ΣSCCPs (r = 0.709),

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ΣMCCPs (r = 0.595) and their sum (r = 0.681). These results indicate that the Gaussian air

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pollution model can predict the dispersion process of the CPs from the production plant to

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the surrounding coniferous leaves.

283 284

Figure 3. Concentrations of the CPs in coniferous leaves and surface soils as a function of the

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distances from the center of the tested CP production plant, together with the fitting curves of

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Gaussian (a) and Boltzmann (b), respectively.

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Concentrations and Spatial Distribution of the SCCPs and MCCPs in the

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Surface Soils. SCCPs and MCCPs were also detected out in all of the surface soil

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samples. The ΣSCCP and ΣMCCP concentrations were in the ranges of 24.8–1842.4 ng g–1

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dw and 19.3–2074.8 ng g–1 dw, respectively (Table 1). The highest ΣSCCP (1842.4 ng g–1)

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and ΣMCCP (2074.8 ng g–1) concentrations in soils were found at site 1 and site 2 inner the

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CP production plant, respectively (Figure 1 and Table S4). Surface soil from sampling site 3,

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located approximately 500 m away from the CP plant, also showed significantly high

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ΣSCCP (423.9 ng g–1) and ΣMCCP (1460.6 ng g–1) concentrations. The ΣSCCP and

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ΣMCCP concentrations in the other ambient surface soils ranged from 24.8 ng g–1 dw to

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481.6 ng g–1 dw with an average of 141.9 ng g–1 dw and from 19.3 ng g–1 dw to 1460.6 ng

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g–1 dw with an average of 199.4 ng g–1 dw, respectively. The pollution levels were much

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higher than those in background soils from Western Europe (ΣSCCPs: