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Frontiers of Earth Science

ISSN 2095-0195

ISSN 2095-0209(Online)

CN 11-5982/P

邮发代号 80-963

2019 Impact Factor: 1.62

Frontiers of Earth Science  2019, Vol. 13 Issue (1): 33-42   https://doi.org/10.1007/s11707-018-0701-4
  本期目录
The distribution and sources of polycyclic aromatic hydrocarbons in shallow groundwater from an alluvial-diluvial fan of the Hutuo River in North China
Jincui WANG1,2(), Yongsheng ZHAO1, Jichao SUN2, Ying ZHANG2, Chunyan LIU2
1. College of Environment and Resources, Jilin University, Changchun 130026, China
2. Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China
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Abstract

This paper has investigated the concentration and distribution of polycyclic aromatic hydrocarbons in shallow groundwater from an alluvial-diluvial fan of the Hutuo River in North China. Results show that the concentration levels of 16 priority polycyclic aromatic hydrocarbons range from 0 to 92.06 ng/L, do not conform to drinking water quality standards in China (GB 5749-2006). However, the concentration figures of priority polycyclic aromatic hydrocarbons are much lower than that of other studies conducted elsewhere in China. In addition, highly-concentrated polycyclic aromatic hydrocarbons (50–92 ng/L) are fragmentarily distributed. The composition of polycyclic aromatic hydrocarbons from this study indicates that low molecular polycyclic aromatic hydrocarbons are predominant in groundwater samples, medium molecular compounds occur at low concentrations, and high molecular hydrocarbons are not detected. The polycyclic aromatic hydrocarbon composition in groundwater samples is basically the same as that of gaseous samples in the atmosphere in this study. Therefore, the atmospheric input is assumed to be an important source of polycyclic aromatic hydrocarbons, no less than wastewater discharge, adhesion on suspended solids, and surface water leakage. Ratios of specific polycyclic aromatic hydrocarbons demonstrate that they mainly originate from wood or coal combustion as well as natural gas and partially from petroleum according to the result of principal component analysis. On the whole, conclusions are drawn that the contamination sources of these polycyclic aromatic hydrocarbons are likely petrogenic and pyrolytic inputs. Future investigations by sampling topsoil, vadose soil, and the atmosphere can further verify aforementioned conclusions.

Key wordspolycyclic aromatic hydrocarbons    unconsolidated sedimentary aquifers    groundwater protection    hydrochemistry    North China
收稿日期: 2017-01-04      出版日期: 2019-01-25
Corresponding Author(s): Jincui WANG   
 引用本文:   
. [J]. Frontiers of Earth Science, 2019, 13(1): 33-42.
Jincui WANG, Yongsheng ZHAO, Jichao SUN, Ying ZHANG, Chunyan LIU. The distribution and sources of polycyclic aromatic hydrocarbons in shallow groundwater from an alluvial-diluvial fan of the Hutuo River in North China. Front. Earth Sci., 2019, 13(1): 33-42.
 链接本文:  
https://academic.hep.com.cn/fesci/CN/10.1007/s11707-018-0701-4
https://academic.hep.com.cn/fesci/CN/Y2019/V13/I1/33
Compounds Abbreviations The number of rings Solubility/(mg·L−1) Log Kow a)
Polycyclic aromatic hydrocarbons PAHs
Naphthalene Nap 2 31.7 3.37
Acenaphthylene Acy 2 1.93 4.00
Acenaphthene Ace 2 3.42 3.92
Fluorene Flu 2 1.9 4.18
Phenanthrene Phe 3 1.29 4.57
Anthracene Ant 3 0.076 4.54
Fluoranthene Fla 3 0.26 5.22
Pyrene Pyr 4 0.14 5.18
Benzo(a) anthracene BaA 4 0.01 5.91
Chrysene Chr 4 0.002 5.86
Benzo(b) fluoranthene BbF 4 0.001 5.80
Benzo(k) fluoranthene BkF 4 0.0007 6.00
Benzo(a) pyrene BaP 5 0.0038 6.04
Indeno(1,2,3-cd) pyrene InP 5 0.062 6.50
Dibenzo(a,h) anthracene DiA 5 0.0005 6.75
Benzo(g,h,i) perylene BgP 6 0.00026 6.50
Tab.1  
Fig.1  
pH T/°C DO/(mg·L−1) Eh/mv EC/(ms·cm−1)
Range 7.08–7.90 14.5–17.2 0.03–13.76 48.7–208 749.9–1110.9
Mean 7.51 15.5 3.46 116.0 775.5
Tab.2  
Sample number Nap Acy Ace Flu Phe Ant Fla Pyr BaA Chr BbF BkF BaP InP DiA BgP SPAHs
G01 ndb) nd nd nd nd nd nd nd 0.19 0.25 nd nd nd nd nd nd 0.44
G02 2.15 0.86 1.05 2.50 4.94 0.46 2.80 1.74 nd nd nd nd nd nd nd nd 16.52
G03 0.02 0.05 0.06 0.01 0.10 0.15 0.01 0.01 nd nd nd nd nd nd nd nd 0.42
G04 0.01 nd nd nd nd nd nd nd nd nd nd nd nd nd nd nd 0.01
G05 0.02 0.07 nd nd nd nd nd nd nd nd nd nd nd nd nd nd 0.09
G06 0.01 nd nd nd nd nd nd nd nd nd nd nd nd nd nd nd 0.01
G07 0.65 0.14 0.07 0.16 0.89 0.05 0.10 0.15 0.06 0.32 nd nd nd nd nd nd 2.57
G08 1.86 1.35 0.46 0.80 6.38 0.43 1.36 1.03 0.16 0.20 0.19 0.11 nd nd nd nd 14.33
G09 0.01 0.02 nd nd 0.01 0.01 nd nd nd nd nd nd nd nd nd nd 0.06
G10 0.01 nd nd nd nd nd nd nd nd nd nd nd nd nd nd nd 0.01
G11 0.02 nd nd nd nd nd nd nd nd nd nd nd nd nd nd nd 0.02
G12 1.27 0.11 0.04 0.09 0.40 nd nd nd nd nd nd nd nd nd nd nd 1.93
G13 2.27 0.98 0.27 1.02 2.66 0.09 0.36 0.26 nd 0.04 nd nd nd nd nd nd 7.94
G14 2.03 3.09 1.28 3.03 7.51 0.55 0.93 0.60 0.06 0.10 nd nd nd nd nd nd 19.20
G15 0.09 nd nd nd 0.02 0.01 0.02 0.01 nd nd nd nd nd nd nd nd 0.15
G16 23.04 3.70 2.06 4.33 6.30 0.29 0.81 0.54 0.37 0.16 nd nd nd nd nd nd 41.62
G17 0.02 nd nd nd nd nd nd nd nd nd nd nd nd nd nd nd 0.02
G18 0.02 0.02 nd nd nd nd nd nd nd nd nd nd nd nd nd nd 0.04
G19 nd nd nd nd nd nd nd nd nd nd nd nd nd nd nd nd nd
G20 0.36 0.08 nd 0.02 0.09 0.02 0.02 0.03 nd nd nd nd nd nd nd nd 0.60
G21 1.14 0.64 0.17 0.63 3.86 0.07 0.80 0.44 nd nd nd nd nd nd nd nd 7.76
G22 0.01 0.02 nd nd nd nd nd nd nd nd nd nd nd nd nd nd 0.03
G23 5.95 2.46 0.82 35.28 4.92 0.09 0.92 0.50 0.44 0.12 nd nd nd nd nd nd 51.55
G24 0.01 0.03 nd nd nd nd nd nd nd nd nd nd nd nd nd nd 0.05
G25 0.99 1.98 1.07 4.04 13.73 0.41 1.33 0.77 0.60 0.16 nd nd nd nd nd nd 25.11
G26 0.40 0.04 0.08 0.04 0.06 nd nd nd nd nd nd nd nd nd nd nd 0.62
G27 0.01 0.02 nd nd nd nd nd nd nd nd nd nd nd nd nd nd 0.03
G28 0.93 1.06 0.73 1.78 3.46 0.15 1.36 0.92 1.17 0.18 nd nd nd nd nd nd 11.75
G29 5.69 1.52 1.04 2.38 4.06 0.24 0.56 0.36 0.22 0.05 nd nd nd nd nd nd 16.14
G30 0.12 0.02 nd nd 0.04 0.02 0.02 0.02 nd nd nd nd nd nd nd nd 0.23
G31 0.13 0.02 nd 0.02 0.02 0.01 nd nd nd nd nd nd nd nd nd nd 0.20
G32 0.63 0.43 nd 0.04 0.09 nd nd nd nd nd nd nd nd nd nd nd 1.19
G33 1.07 0.43 0.28 1.29 4.65 0.17 0.76 0.52 0.43 0.14 nd nd nd nd nd nd 9.75
G34 nd 0.13 nd nd 0.01 0.02 nd nd nd nd nd nd nd nd nd nd 0.17
G35 0.02 0.07 nd nd nd nd nd nd nd nd nd nd nd nd nd nd 0.08
G36 nd nd nd nd nd nd nd nd nd nd nd nd nd nd nd nd nd
G37 1.01 0.95 0.58 5.02 0.02 0.06 3.04 1.82 2.17 0.60 nd nd nd nd nd nd 15.28
G38 30.98 8.33 5.54 14.43 26.85 1.16 2.36 1.34 0.74 0.33 nd nd nd nd nd nd 92.15
G39 17.90 3.21 1.31 3.74 7.25 0.37 0.91 0.61 0.43 0.15 nd nd nd nd nd nd 35.92
Tab.3  
PAHs Residual levels/(ng·L−1) Standards/(mg·L−1)
Range Mean SD China US EPA
Nap nd–30.98 2.59 6.58
Acy nd–8.33 0.82 1.59
Ace nd–5.54 0.43 0.98 - 70
Flu nd–35.28 2.07 6.04 - 50
Phe nd–26.85 2.52 5.06
Ant nd–1.16 0.12 0.23 - 300
Fla nd–3.04 0.47 0.80 - 20
Pyr nd–1.82 0.30 0.49 - 20
BaA nd–2.17 0.18 0.41 - 1.2×10−3
Chr nd–0.60 0.07 0.13 - 0.12
BbF nd–0.19 0.00 0.03 - 1.2×10−3
BkF nd–0.11 0.00 0.02 - 1.2×10−2
BaP nd nd nd 0.01 1.2×10−4
InP nd nd nd - 1.2×10−3
DiA nd nd nd - 1.2×10−4
BgP nd nd nd
SPAHsc) nd–92.06 9.58 18.42 2 -
Tab.4  
Fig.2  
PAHs Factor loadings
F1 F2
Nap 0.89 d) 0.14
Acy 0.95 0.28
Ace 0.94 0.29
Flu 0.49 0.28
Phe 0.92 0.27
Ant 0.89 0.30
Fla 0.43 0.83
Pyr 0.41 0.84
BaA 0.10 0.93
Chr 0.22 0.86
% Variance 48.59 34.06
Tab.5  
Fig.3  
Fig.4  
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