Journal Pre-proof Spatial distribution, environmental risk and sources of heavy metals and polycyclic aromatic hydrocarbons (PAHs) in surface sediments-Northwest of Persian Gulf Meisam Rastegari Mehr, Behnam Keshavarzi, Farid Moore, Sahar Fooladivanda, Armin Sorooshian, Harald Biester PII:
S0278-4343(19)30419-4
DOI:
https://doi.org/10.1016/j.csr.2019.104036
Reference:
CSR 104036
To appear in:
Continental Shelf Research
Received Date: 22 February 2019 Revised Date:
30 November 2019
Accepted Date: 8 December 2019
Please cite this article as: Mehr, M.R., Keshavarzi, B., Moore, F., Fooladivanda, S., Sorooshian, A., Biester, H., Spatial distribution, environmental risk and sources of heavy metals and polycyclic aromatic hydrocarbons (PAHs) in surface sediments-Northwest of Persian Gulf, Continental Shelf Research, https://doi.org/10.1016/j.csr.2019.104036. This is a PDF file of an article that has undergone enhancements after acceptance, such as the addition of a cover page and metadata, and formatting for readability, but it is not yet the definitive version of record. This version will undergo additional copyediting, typesetting and review before it is published in its final form, but we are providing this version to give early visibility of the article. Please note that, during the production process, errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. © 2019 Published by Elsevier Ltd.
Spatial distribution, environmental risk and sources of heavy metals and polycyclic aromatic hydrocarbons (PAHs) in surface sediments-Northwest of Persian Gulf
1 2 3 4 5 6 7 8 9 10 11 12 13
Meisam Rastegari Mehra, Behnam Keshavarzib*, Farid Mooreb, Sahar Fooladivandab, Armin Sorooshianc, d, Harald Biestere a
Department of Applied Geology, Faculty of Earth Science, Kharazmi University, Tehran 15614, Iran Department of Earth Sciences, College of Sciences, Shiraz University, Shiraz 71454, Iran c Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ 85721, USA d Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ 85721, USA b
e
Institut für Geökologie, AG Umweltgeochemie, Technische Universität Braunschweig, 38106 Braunschweig, Germany
14 15
*Corresponding author;
16 17
Tel/fax: +98 71 32284572 E-mail address:
[email protected]
18 19
Abstract
20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38
In the current study, environmental risk, potential sources and spatial distribution of heavy metals and polycyclic aromatic hydrocarbons (PAHs) were investigated in the sediments of Musa Estuary, the largest Estuary in the Persian Gulf. A total of 68 surface sediment samples were collected and analyzed for heavy metals and PAH concentration using inductively coupled plasma mass spectrometry (ICP-MS) and High-Performance Liquid Chromatography (HPLC). Enrichment factor (EF) and ecological risk (E) calculation revealed the highest contamination and risk for Hg, mostly due to the activity of a petrochemical complex in the area. Also, most samples showed a mean probable effect level (PEL) quotient of 0.51 to 1.50, and a probable 49% toxicity. Pearson’s correlation coefficient and principal component analysis (PCA) indicated the same (anthropogenic) origin for Cu, Hg, Pb and Zn. Five-six ring PAHs are dominant in sediments, and most studied compounds showed higher concentrations than their effect range low (ERL) and effect range median (ERM). Moreover, the highest toxic equivalent (TEQ) and ecological risk were observed in the main treatment lagoon. PAH diagnostic ratios and PCA revealed both petrogenic and pyrogenic sources for these compounds, and calculated mass inventory (I) values indicated a relatively high potential of the sediments (0.2-12.28 tons) for contaminating the marine environment. The results indicated that the wastewater treatment has good efficiency in reducing contaminant levels, as Mann-Whitney U test results showed a significant difference in Ni, Cr, Hg and ∑PAH concentration between treatment lagoons and estuarine sediments.
39 40
Keywords: Sediment; Ecological risk; Treatment lagoon; Heavy metals; PAHs; Persian Gulf 1
41
1. Introduction
42
Most large cities around the world are located in coastal zones (Kim et al., 2016), where rapid
43
economic development, industrialization and urbanization, population growth and agricultural
44
practices have resulted in serious problems for the environment (Paramasivam et al., 2015). Due
45
to geomorphological and hydrodynamic features of estuarine systems, economic growth is
46
deeply rooted in these systems and they have numerous advantages for human settlement. A
47
large amount of pollutants including heavy metals and persistent organic pollutants are
48
discharged into the aquatic ecosystems through various pathways (Yin et al., 2011). In terms of
49
food resources and ecosystem services, coastal zones also have significant advantages for
50
humans. On the other hand, human activities pose severe negative impacts on the coastal and
51
estuarine ecosystems and the viability of the resources. Thus, management and pollution control
52
for conservation of aquatic organisms and marine environment is a necessity (Pejman et al.,
53
2015). It is a well-known fact that sediments are important reservoirs for many persistent and
54
toxic chemicals, and a route through which contaminants enter aquaculture and wildlife food
55
chains (Long et al., 1995; Praveena et al., 2007; Moore et al., 2015). Depositional zones can be
56
loaded with pollutants derived from anthropogenic sources and reflect the severity of
57
anthropogenic activities (Dudhagara et al., 2016). More recently, there has been increasing
58
interest in the study of heavy metals and PAHs within the scientific community owing to their
59
toxic effects (Zhang et al., 2016; Delshab et al., 2017).
60
In recent decades, a huge amount of contaminants originated mostly from rapid industrial and
61
agricultural development, and shipping traffic has entered the Persian Gulf and threatened its
62
aquatic ecosystem (Monikh et al., 2013; Pourkerman et al., 2017; Keshavarzi et al., 2018). The
63
current study investigates two important categories of contaminants (heavy metals and PAHs) in
64
surface sediments of Musa Estuary, as the most important industrial zone in Iran, famous for its
65
petrochemical complexes and the Imam Khomeini Port. The main objectives of this study are (1)
66
examining selected heavy metals and PAHs in the sediments of the Musa Estuary, with a focus
67
on characterizing their spatial distribution and concentrations; (2) investigating the role of
68
previous activity of the chlor-alkali unit on Hg contamination; (3) identifying potential sources
69
of these contaminants, and assessing the efficiency of the current treatment system to remove the
2
70
pollutants; and (4) evaluating the degree of contamination and the resulting ecological risk
71
caused by the heavy metals and PAHs.
72 73 74
2. Materials and Methods
75
2.1. Site description
76
The Persian Gulf, with an average depth and surface area of 35 m and 240,000 km2, respectively,
77
forms the coastline of several countries including Iran, Saudi Arabia, the United Arab Emirates,
78
Oman, Qatar, Bahrain, Iraq and Kuwait. This shallow sea, similar to Baltic and North Sea, has a
79
warm and saline water (Agah et al., 2009). The Persian Gulf’s hydrological system is such that
80
surface water moves toward the coasts, sinks, and subsequently flows out the Gulf by
81
counterflow at lower levels with the highest salinities, in both bottom and surface coastal water
82
(Sugden, 1963).
83
Musa Estuary is the largest Estuary in Iran, located northwest of the Persian Gulf in Mahshahr
84
County (30° 15′–30 ° 32′, 49°–49° 20′) (Fig 1). Irregular bed elevations observing in the main
85
branches of the Estuary, resulted from bed erosions and tidal current complexities. Therefore, no
86
regular stream is present in this multi branch Estuary. It has an arid climate with an annual
87
average temperature of 25.5 °C and annual average precipitation of 213.4 mm (Keshavarzi et al.,
88
2018). Agricultural lands and industrial sectors including LPG plants, petrochemical complexes
89
and oil transfer docks are built along the coast of the Estuary (Mortazavi and Sharifian, 2011;
90
Lahijanzadeh et al., 2019). Also, the two main urban population centers in this area include
91
Mahshahr and Bandar-e-Eman Cities. Mahshahr is an important industrial hub in Iran because of
92
its petrochemical complexes, Imam Khomeini Port, and metal and petroleum industries. Most of
93
the petrochemical complexes in the area transfer their wastewater to the Fajr Wastewater
94
Treatment Plant, in which wastewater is treated, held in treatment lagoons located in the
95
petrochemical zone (north of the Estuary), and then discharged into the Musa Estuary. Also,
96
some petrochemical units have their own wastewater treatment facilities or discharge their
97
untreated wastewater directly into the Musa Estuary.
3
98 99
2.2. Sampling and sample analysis
100
In this study, a sampling strategy was developed based on the information regarding the main
101
contaminating industries, shipping routes and the main fisheries and docks (obtained from
102
Khuzestan Environmental Protection Office). A total of 36 surface sediment samples (S1-S36)
103
were collected using a stainless steel van Veen grab sampler in February 2015 in the Musa
104
Estuary and its tributaries (24 samples; S1-S24), the northwest shore of the Persian Gulf (7
105
samples; S25-S31) and treatment lagoons of the petrochemical zone (5 samples; S32-S36). A
106
hand-hold GPS was used to record sampling locations (Table 1 and Fig 1). Six subsamples were
107
taken and mixed thoroughly to obtain a bulk/representative sample for each sampling site. The
108
composite samples were transported to the laboratory (placed into polyethylene bags). A fraction
109
of each sediment sample was air dried, homogenized in a porcelain mortar and passed through a
110
63 µm sieve to achieve a fine-grained sediment sample. Concentration of seven heavy metals
111
(Al, Cr, Cu, Hg, Ni, Pb and Zn) was measured following aqua regia digestion using inductively
112
coupled plasma mass spectrometry (ICP-MS) in Acme Analytical Laboratories, Ltd. Quality
113
assurance and control (QA/QC) included duplicate analyses, procedural blank, and use of
114
standard reference materials (STD DS10 and STD OREAS45EA). The relative standard
115
deviation (RSD) was less than 4% for each element, and the recovery percentages ranged from
116
96-103%, and the blank was below the detection limit.
117
The pH, electrical conductivity (EC) and cation exchange capacity (CEC) of sediment samples
118
were determined based on methods summarized by Ryan et al. (2007). In all sediment samples
119
the organic matter (OM) content was analyzed using the LOI procedure (Schulte and Hopkins,
120
1996). In order to determine sediments texture, each sediment was sieved through a 2 mm mesh
121
sieve (Keshavarzi et al., 2015), and particle size distribution (sand, silt, and clay content) was
122
determined using the hydrometer method (Gee and Bauder, 1986).
123
To determine 16 PAH concentrations, 32 surface sediment samples (H1-H32) were collected at
124
the same locations as for heavy metals sampling (each sample comprising six subsamples) from
125
Musa Estuary and its tributaries (21 samples; H1-H21), northwest shore of the Persian Gulf (7
126
samples; H22-H28) and treatment lagoons of the petrochemical zone (4 samples; H29-H32)
127
(Table 1 and Fig 1). The samples were kept in a solvent-cleaned glass jar and stored in a cool 4
128
box at 4 °C and transported to the laboratory of Isfahan University of Technology to be prepared
129
and analyzed. In the laboratory, EPA 3550 B and EPA 3630 C methods were used for extraction
130
and clean-up procedures, respectively. The 16 PAH compounds were measured using a RIGOL
131
L-3000 High-Performance Liquid Chromatography (HPLC) system, with a Hewlett-Packard
132
1046 A fluorescence detector and a RIGOL L-3500 UVvis detector. For the extraction of
133
analytes, 100 mL dichloromethane (CH2Cl2) was added to 2 g of each homogenized sample, and
134
mixed for 8 h. Then, a rotary vacuum evaporator was used to concentrate the extracts to 1 mL,
135
and 20 µL of this extract was injected for PAHs analysis. The mobile phase consisted of
136
acetonitrile/water in gradient mode at a flow rate of 1.0 mL min−1 and the temperature set at 35
137
°C. Duplicates, method blanks and standard reference materials (Sigma-Aldrich Co. LLC EPA
138
525 PAH Mix A and EPA 525 PAH Mix B) were used to assess quality assurance and quality
139
control, and RSD and the average recovery for the spikes were <9% and ranged between 89-
140
98%, respectively. The detection limits varied between 0.01 and 1 µg/kg for individual PAHs
141
(Table 5).
142 143
2.3. Data analysis
144
2.3.1. Enrichment Factor (EF)
145
Enrichment factor (EF) is widely used to discriminate between natural and anthropogenic
146
sources and to reflect the status of environmental contamination. It is calculated as follows (Hu et
147
al., 2013; Pang et al., 2015):
148 149
EF = (X/Al) sample / (X/Al) Background
(1)
150 151
where X refers to the concentration of a heavy metal of interest. In this study, Al was used to
152
normalize the metal concentrations, and mean elements’ concentration in the Earth’s crust was
153
considered as background sample, to calculate the enrichment factor. EF<1 indicates no
154
enrichment, 1-3 minor enrichment, 3-5 moderate enrichment, 5-10 moderate to severe
5
155
enrichment, 10-25 severe enrichment, 25-50 very severe enrichment, and >50 extremely severe
156
enrichment (Chabukdhara and Nema, 2012).
157 158
2.3.2. Potential ecological risk index (PER)
159
The potential ecological risk index (PER) assesses the contamination degree of heavy metals in
160
sediments, and is calculated as follows (Bastami et al., 2015):
161 162
PER = ∑ E
(2)
163
E = TC
(3)
164
C = Ca/Cb
(4)
165 166
where C is the single element pollution factor, Ca is the concentration of the element in samples,
167
and Cb is the background reference value of the element (mean elements’ concentration in the
168
Earth’s crust was used in this study). PER is a comprehensive potential ecological index, E is the
169
ecological risk of individual metals or potential risk factor, T is toxic response factor which for
170
the analyzed elements is taken as Zn = 1 < Cr = 2 < Cu = Ni = Pb = 5 < AS = 10 < Cd = 30 < Hg
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= 40. The potential risk factors are classified as: low (E < 40); moderate (40 ≤ E < 80);
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considerable (80 ≤ E < 160); high (160 ≤ E < 320); and very high (E ≥ 320). Consequently the
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potential ecological risk categories are as follows: low (PER < 150); moderate (150 ≤ PER <
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300); considerable (300 ≤ PER < 600); or very high (PER ≥ 600) (Hakanson, 1980; Rastegari
175
Mehr et al., 2016).
176 177
2.3.3. Mean PEL quotient
178
Heavy metals always occur in sediments as complex mixtures, and they form combined toxicant
179
groups in sediments. In order to evaluate the possible biological effects of the coupled toxicity of
180
the studied metals the mean probable effect level (PEL) quotient method was used (Zhang and
181
Gao, 2015): 6
182 ∑
Mean PEL quotient =
183
(5)
184 185
where Cx is the sediment concentration of metal ‘‘x’’, PELx is the PEL for metal ‘‘x’’, and ‘‘n’’
186
is the number of the studied metals.
187 188
2.3.4. Toxic equivalents (TEQs) of PAHs
189
To quantify the toxicity of PAH compounds relative to benzo[a]pyrene (i.e., an assumed
190
reference chemical), toxic equivalency factors (TEFs) were calculated. Toxic equivalents (TEQs)
191
of PAHs in each sampling station were calculated using the following equation (Nisbet and
192
LaGoy, 1992):
193
TEQ = ∑ Cn TEFn
194
(6)
195 196
where Cn is the concentration of PAHs, and TEFn is the toxic equivalency factor for PAHs
197
(Table 5).
198 199
2.3.5. Ecological risk of PAHs
200
M-ERM-Q was used to assess the ecological risk of multiple toxic chemicals exceeding their
201
effects range median (ERM) guidelines. The quantity is calculated according to the following
202
equation (Li et al., 2015):
203
204
M-RM-Q =
∑(
)
205 7
(7)
206
where Ci is the concentration of compound i in a sediment sample, ERMi is the ERM for
207
compound i, and n is the number of compounds.
208 209
2.3.6. Mass Inventory
210
The mass inventories of PAHs in the sampled sediments, as a potential source of pollution to
211
oceanic environment, were calculated using the following equation (Li et al., 2015):
212
I = CAdρ
213
(8)
214 215
where I is the inventory (in ton), C is concentration of total PAHs (µg/kg) in sediment, A is the
216
water area of sampling region (km2), d is sediment thickness (7 cm in this study), and ρ is the
217
sediment density (1.5 g/cm3).
218 219
2.4. Statistical analysis and geographic information system
220
Statistical analysis of the data was carried out using SPSS 19.0 for Windows. Multivariate
221
statistical techniques such as correlation coefficients and principal component analysis (PCA)
222
were performed for the dataset to reveal relationships between parameters and for source
223
identification. Also, the Mann-Whitney U test, which is often considered the non-parametric
224
alternative to the independent t-test, was used to compare heavy metal and PAH concentrations
225
between the treatment lagoon and estuarine sediments. Also, ArcGIS (version 10) was applied to
226
plot the location of sampling stations, and to determine the area of treatment lagoons and
227
sampled region of the Estuary for calculation of mass inventories. For these purposes, satellite
228
images obtained from SASPlanet (V.12.8.8) with appropriate magnification were georeferenced
229
and used as base maps.
230 231
3. Results and discussion
8
232
3.1. Physicochemical parameters and total metals concentration
233
Table 2 provides the descriptive statistics of heavy metal concentrations and physicochemical
234
parameters in sediment samples, as well as their PEL and mean values in Earth’s crust. Based on
235
the United States Department of Agriculture (USDA) ternary diagram, sediment texture could be
236
classified as silty clay, clayey silt, clayey loam and silty sand showing the dominance of fine
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texture, particularly in the Estuary. The sediments collected from the interior of the Estuary have
238
a reduced sand size fraction compared to the northwestern coast of the Persian Gulf. This coarse
239
texture in S25-S31 samples is probably the result of local elevated hydrodynamics that interfere
240
with fine particle deposition.
241
The sediment pH ranges from 7.91 to 8.57 in treatment lagoons and 8.23 to 9.08 in the Estuary
242
with mean values being 8.28 and 8.49, respectively. These high values reveal the alkaline nature
243
of the sediments, and are comparable with the values measured in Tapti River Estuary in India
244
(~8.29) (Shah et al., 2013). Seemingly, two main factors that affect pH values in the present
245
study include the presence of a large amount of carbonate shells and discharge of several high
246
pH petrochemical wastewaters (8 to 11) into the Estuary, reported by Moore and Keshavarzi,
247
(2016). The mean sediment CEC value in the Estuary (34.99 meq/100g) is comparable with that
248
of treatment lagoons (32.11 meq/100g). Sediment EC values are variable, ranging from 5.32 to
249
34.72 and 2.97 to 32.62 mS/cm with an average of 16.99 and 13.36 mS/cm in the Estuary and
250
treatment lagoons, respectively. Also, mean organic matter content values of sediments in the
251
lagoons and the Estuary are 11.23 % and 10.52 %, respectively.
252
Considering elemental concentrations, a decreasing trend is observed from the northern part of
253
the Estuary to the outer Estuary (and northwestern coast of the Persian Gulf) and from the east of
254
the petrochemical zone to the southwest. Two key source variables for this trend include
255
petrochemical companies and urban activities, as well as the finer grain size of sediments in the
256
North of the study area causing more pollutants adsorption. Aluminum is the most abundant
257
metal in all sediment samples, and the mean concentration of Hg and Ni in both treatment
258
lagoons and Estuary exceeds their characteristic concentrations in the Earth’s crust. The highest
259
Hg concentration (17952 µg/kg) is measured in sample S21 (east of the petrochemical zone).
260
Also, mean Zn concentration in lagoon sediments exceeds its concentration in Earth’s crust. In
261
comparison with probable effect level, Hg and Ni are the only elements with higher mean 9
262
concentrations in surface sediment samples in the study area. Moreover, the mean Zn
263
concentration in treatment lagoons typically is enhanced relative to other samples. The difference
264
could also be seen for Cu and Pb, although to a lesser extent. This situation, clearly, shows the
265
role of treatment lagoons in reducing metal concentrations (particularly Zn) in wastewater. In
266
fact, the present wastewater treatment system is relatively efficient in removing heavy metals.
267
However, if the produced enriched sediments is not disposed properly, a greater problem will
268
emerge.
269 270
3.2. Contamination level and risks of heavy metals
271
The enrichment factor (EF) of metals at each station was calculated to quantify the influence of
272
anthropogenic sources. Values of EF decreases in the following order: Hg > Ni > Zn > Cu > Pb >
273
Cr (Fig 2). The mean EF of Ni (27.60) and Hg (167.57) exceeds 25, indicating very severe and
274
extremely severe enriched levels, respectively. Cu and Zn are classified as moderately to
275
severely enrich with mean EF values of 5.32 and 7.78, respectively. Also, Pb (3.58) and Cr
276
(2.40) exhibit moderate and minor enrichments, respectively. It must be noted that, despite high
277
EF of Ni, it should not be considered as a highly anthropogenically influenced element in the
278
area. Negligible variations in Ni concentration (and EF) in different sampling stations and its low
279
skewness (which may show the normal distribution) confirms the high natural concentration of
280
Ni in the study area, consistent with past work (Moore and Keshavarzi, 2016). Moreover, in
281
contrast to higher EF values of Pb and Zn in treatment lagoons, the highest EFs for Hg are
282
observed in the eastern and southeastern parts of the petrochemical zone, probably due to the
283
activity of a chlor-alkali unit with a mercury-cell process in this location.
284
Chemical conditions of the sedimentary environment, pollutant inputs and physical
285
characteristics are important factors that affect heavy metal contamination in sediments (Sun et
286
al., 2015). In this study, higher heavy metal concentrations in samples collected from the eastern
287
part of the petrochemical zone, clearly illustrate the influence of anthropogenic metal input. The
288
role of the metal input is already reported in other parts of the Persian Gulf (Almasoud et al.,
289
2015; Alharbi et al., 2017; Bibak et al., 2018; Janadeleh et al., 2018). On the other hand,
290
generally, lower metal concentrations are measured in areas with intensive tidal washing (Mistch
291
et al., 2009). As mentioned earlier, the interior of the Estuary has a reduced hydrodynamics 10
292
where, greater contents of fine particles, as well as low washing mechanism of heavy metals, has
293
led to further accumulation of contaminants in the sediments. This is confirmed by the much
294
lower concentration of heavy metals in the northwestern coast of the Persian Gulf (samples S25-
295
S31) with coarse sediment texture.
296
The potential ecological risk index (PER) of heavy metals and ecological risk index (E) of
297
individual metals were calculated using the concentrations of studied elements (Cr, Cu, Hg, Ni,
298
Pb and Zn) in sediment samples. Figure 3 shows the calculated E values for each metal and PER
299
of the six studied elements in the surface sediments. Values of E for all investigated metals,
300
except Hg, in all sampling stations exhibit a low potential risk (below 40). Among the studied
301
metals, Hg shows the highest E value due to severe contamination, particularly east of the
302
Estuary (samples S19, S20, S21and S22), and its high toxic-response factor. Mercury
303
contamination also reaches 32.9 and 38.8 mg/kg in tissues of Cynoglossurs arel and Belangerii
304
of this area (Keshavarzi et al. 2018). Considering calculated PER values, low, moderate,
305
considerable and very high potential ecological risk are revealed for 10 (27.7 %), 8 (22.22 %), 13
306
(36.11 %) and 5 (13.88 %) of sediment samples, respectively. However, a decreasing trend in
307
ecological risk is observed from the inner Estuary to the outer Estuary and northwestern coast of
308
the Persian Gulf. It should be also noted that, because the wastewater of Bandar Imam
309
Petrochemical Company, as the main source of high Hg contamination, is discharged directly
310
and without treatment to the Estuary, PER is higher in the North of the Estuary than in sediments
311
of treatment lagoons.
312
To assess possible combined biological effects of heavy metals in sediments of the study area,
313
the mean PEL quotient of each sampling station was calculated (Fig 4). Based on previous
314
studies (Long et al., 2000; Zhang and Gao, 2015), mean PEL quotients of <0.1, 0.11–0.5, 0.51–
315
1.5 and >1.50, show 9%, 21%, 49% and 76% probable toxicity, respectively. The mean PEL
316
quotient of a large part of the Estuary ranges from 0.51 to 1.50, and consequently the probability
317
of such areas being toxic is 49%. Also, the highest probability for toxicity is measured for
318
sediments in the eastern part of the petrochemical zone with mean PEL quotient exceeding 1.5.
319 320
3.3. Metal Interrelationships and Source Identification
11
321
Pearson’s correlation coefficient analysis was performed to identify the relationship among
322
heavy metals, and between metals and physicochemical parameters in sediment samples (Table
323
3). The data normality was evaluated using Shapiro-Wilk normality test, and non-normal
324
parameters were normalized before the analysis. Pearson’s correlation analysis between the
325
concentrations of Cr, Ni and Al shows that these metals has a strong positive correlation (r =
326
0.89 to 0.97, p < 0.01). With regard to very slight variations in Ni, Cr and Al concentration in the
327
study area, their high correlation coefficients could be due to the same, natural, source. Also, the
328
relatively strong correlation between Al concentration and clay percent, and consequently its
329
correlation with CEC, stems from the role of Al in clay mineral structure (Brady and Buckman,
330
1960). Significant correlations are also observed between Cu, Pb and Zn with relatively severe
331
concentration variations in different sampling stations. Despite the similarity of Hg with Cu, Pb
332
and Zn in terms of concentration variations, there is no correlation between Hg and these metals,
333
mainly because of their different sources and distribution. The medium correlation between OM,
334
and Cu and Hg could arise from the affinity of these elements for organic matter, which is also
335
reported in previous studies (Yang et al., 2015; Keshavarzi et al., 2015; Amjadian et al., 2016).
336
The effect of sediments OM, silt and clay content on CEC is clearly obvious considering the
337
strong correlation between CEC and these parameters.
338
Principle component analysis (PCA) using factor extraction with an eigenvalue >1 after varimax
339
rotation was also applied to identify elements’ sources. Three principal components explaining
340
more than 78 % variance of the data were extracted (Table 4). The first factor is significantly
341
loaded with three metals (sand percentage, Al, Cr and Ni in descending order of loading values)
342
explaining 34.96 % of the total variance. As also evident from EF and correlation coefficients,
343
these metals are believed to be mostly accounted for by geogenic sources and to a minor extent
344
by anthropogenic sources. However, despite the fact that Ni is significantly enriched, it displays
345
a low variation coefficient, symmetric box plot and low range. Based on Paul et al., (2003) high
346
natural concentration of Ni in south Iran is the result of the proximity to the Zagros Mountain
347
belt, where, limestone, shale, sandstone and conglomerate are the main outcrops, while Ni is
348
enriched in some bauxite deposits. Association of these three metals with sand percentage in the
349
sediment samples confirms their geogenic source. The second component explained 22.87 % of
350
the total variance and loadings heavily on Pb, Zn and clay, and moderately on Cu, OM and silt.
351
The metals of this component seem to be affected by human activities, mainly wastewater of 12
352
petrochemical companies, Bandar-e-Emam port, pipe manufacturing units and commercial
353
dockyards. Placement of the metals with OM, clay and silt indicates their adsorption by mineral
354
and organic colloids. Also, the third component is loaded primarily by Hg, Cu and OM, and
355
moderately by clay accounting for 20.79 % of the total variance. Cu and Hg (particularly Hg),
356
are enriched in sediments of the study area and probably have anthropogenic sources, and their
357
correlation with clay and (particularly) organic matter reveals that these colloids have an
358
important role in accumulation of Hg and Cu in sediments. Overall, considering PCA, EF and
359
variation coefficients Hg, Cu, Zn and Pb are mostly affected by human activities.
360 361
3.4. Polycyclic aromatic hydrocarbons (PAHs) concentration and composition
362
Table 5 shows the descriptive statistics of PAH concentrations in sediments of the treatment
363
lagoons, and the Estuary. Total PAH concentrations (∑PAH), low-molecular-weight PAH (2–3
364
rings), and high-molecular-weight PAH (4–6 rings) range from 13 to 53449 µg/kg (averaging
365
11834.9 µg/kg), 1.95 to 29100 µg/kg (averaging 6500.11 µg/kg), and 11.05 to 24349 µg/kg
366
(averaging 5334.79 µg/kg) in lagoons, and 9.48 to 1514.3 µg/kg (averaging 148.76 µg/kg), 1.65
367
to 967 µg/kg (averaging 75.33 µg/kg) and 7.73 to 547.3 µg/kg (averaging 73.42 µg/kg) in the
368
Estuary, respectively. Sediment quality guidelines (the effect range low (ERL) and effect range
369
median (ERM) were used to assess the ecological risk of individual PAHs. Results show that
370
median concentrations of all PAHs are lower than both ERL and ERM, while in lagoon
371
sediments the mean concentrations of Acenaphthene (Ace), Fluorene (Fl), Fluoranthene (Flu),
372
Benzo[a]anthracene (BaA), and Chrysene (Chr) are higher than their ERL, and mean
373
concentrations of Phenanthrene (Phe) and Anthracene (Ant) exceed their ERM. Also,
374
Naphthalene (Np), Ace, Fl and Phe concentrations in sediments of the eastern part of the
375
petrochemical zone, affected by untreated wastewater, exceeded their ERL.
376
PAHs classification based on the number of aromatic rings in sediment samples is presented in
377
Figure 5. The results show that in the study area, the concentrations of 2-3 rings, 4 rings and 5-6
378
rings PAHs account for 4.44 to 31.92 %, 9.30 to 30.37 % and 50.94 to 78.89 % of total
379
concentration respectively. Therefore, 5-6 rings PAHs (BeP, BbF, BkF, BaP, DiBA, BgPer and
380
IndPy) are the dominant compounds in both lagoons and estuarine sediments.
13
381
To characterize the carcinogenic properties of PAH mixtures, TEQs were calculated (Fig 6). The
382
results indicate that total TEQ for sediment samples of treatment lagoons and the Estuary range
383
from 1.31 to 1981.51 µg/kg and 1.30 to 23.54 µg/kg, respectively. The highest TEQ values are
384
observed in the main treatment lagoon and eastern part of the petrochemical zone. Also, total
385
concentration of carcinogenic (BaA, Chr, BeP, BaP, BbF, BkF, IndPy, DiBA) PAHs in treatment
386
lagoons and the Estuary range from 12.30 to 19787 µg/kg, and 2.57 to 213.1 µg/kg, respectively.
387
To analyze the ecological risk of PAHs in sediment samples, the mean ERM quotient was
388
calculated. Based on ecological risk, the sampling sites are classified as low (<0.1), medium–low
389
(0.11-0.5), medium–high (0.51-1.50), and high-priority (>1.50), and are determined to coincide
390
with <11%, 25–30%, 46–53%, and >75% incidences of acute toxicity (Li et al. 2015). The
391
results show that except for the two main treatment lagoons, all sampling stations have m-ERM-
392
Q values below 0.1, indicating low priority, and the probability of being toxic was less than 11%.
393
The highest mean ERM quotient value (2.68) is observed in the main treatment lagoon to which
394
wastewater of different petrochemical companies are discharged. This indicates the importance
395
of these lagoons and, consequently, standard disposal of their bottom sediments. In fact, the
396
bottom sediments of the treatment lagoons in which PAHs are concentrated should be considered
397
as a potential source for contamination of the environment, and therefore, it needs to be disposed
398
safely after each periodic dredging of bottom sediments.
399 400
3.5. Identification of PAHs sources
401
The diagnostic ratios including Low Molecular Weight to High Molecular Weight
402
(LMW/HMW), Phe/Ant, Flu/Pyr, and Flu/Flu+Pyr were used to characterize the PAH potential
403
sources in sediments. The LMW/HMW ratio indicates that PAHs in 75% of the samples have
404
originated from pyrogenic sources (LMW/HMW< 1) (Readman et al., 2002). Also, the range of
405
Phe/Ant, Flu/Pyr, and Flu/Flu+Pyr are 2-55, 0.03-2.25, and 0.03-0.69, respectively. Based on
406
Qiao et al., (2006), Flu/Pyr values < 1 are indicative of petrogenic sources and values > 1 are
407
indicative of combustion origins; Flu/(Flu + Pyr) ratios below 0.5 and greater than 0.5 are typical
408
of petrogenic and pyrogenic origins respectively; and Phe/Ant values > 15 and < 10 are
14
409
indicators of petrogenic and pyrogenic sources, respectively. Therefore, apart from pyrogenic
410
input as a major source, there are also some petrogenic sources for PAHs in sediments.
411
Principal component analysis (PCA) was also conducted to reduce the number of variables (PAH
412
compounds) and to analyze relationships. Due to non-normal distribution of the data (based on
413
Shapiro-Wilk normality test) the data was log-transformed prior to performing PCA. Two
414
principal components (PCs) with accumulative variance of more than 85 % were extracted for
415
the sediment samples after Varimax rotation (Table 6). All PAH compounds have a positive
416
coordinate in PC1. This component, which explains 64.87 % of total variance, has strong
417
correlations with all compounds except DiBA, BgPer and IndPy. Regarding the strong
418
correlation of PAH compounds in PC1 with the total PAH concentration, it could be concluded
419
that the first component is a quantitative correlation component and corresponds to the total
420
PAHs concentration. PC2, contributing 20.24 % of the total variance, is dominated by 5-6 rings
421
PAHs (DiBA, BgPer and IndPy) related to pyrogenic sources, e.g., petroleum combustion and
422
refined petroleum products (Li et al. 2015). The highest concentrations of these three PAH
423
compounds are found in sediments close to Bandar Imam and Razi petrochemical complexes and
424
also in the main treatment lagoon. There are several fired flairs in the petrochemical zone,
425
emitting gaseous and particulate contaminants which may affect surrounding environments as
426
fallout. It seems that this atmospheric source, is the main pyrogenic origin of PAHs in this
427
region.
428 429
3.6. Mass inventory of total PAHs
430
Contaminated sediments in the study area could act as a source for the oceans. To assess this
431
potential, mass inventories of total PAHs were calculated. In this study, the mass inventories of
432
treatment lagoons and estuarine areas were calculated separately. Geographical information
433
system (GIS) was used to determine the water surface area of each sampling region and
434
accordingly, the area of lagoons and Estuary were 2.4 and 786 km2, respectively. Also, the
435
median and mean concentrations of the PAHs as lower and upper limits, respectively, were used
436
to deduce the conservative estimate of the concentrations. The calculated inventories range from
437
0.2 to 2.98 tons and 1.96 to 12.28 tons in the treatment lagoons and estuarine area, respectively.
438
Regarding the lower area of the lagoons compared with estuarine regions in this study, its
439
calculated mass inventories could be considered high, and urgent attention to lagoons’ sediments 15
440
is required. However, the mass inventory assessment may have some limitations and
441
uncertainties. For example, a homologous spread of PAHs in sediments, and a flat seabed with
442
no topographic variability was assumed in the calculations. This uncertainty for the Estuary may
443
be even more significant for the treatment lagoons. Nevertheless, the results obtained from this
444
approach can provide an initial view for the potential of a polluted area (as a secondary source)
445
to contaminate the marine environment. This approach could become more valuable if, for
446
instance, the mass inventory is also calculated for other coastal areas in the Persian Gulf. It
447
should be noted that, using mean concentrations of contaminants can reduce uncertainty to some
448
extent.
449 450
3.7. Mann-Whitney U test
451
The Mann-Whitney U test is used to compare differences between two independent groups when
452
the dependent variable is either ordinal or continuous, but not normally distributed. In the present
453
study, this test was performed to compare heavy metals and ∑PAH concentrations in sediment
454
samples collected at lagoons and estuarine areas due to their non-normal distributions (Table 7).
455
Results show that the concentrations of Cu, Pb, Zn and Al (p > 0.05) are not statistically different
456
between treatment lagoons and the Estuary. On the other hand, there are significant differences
457
in Ni, Cr, Hg and ∑PAH concentrations between the two sediment groups (p < 0.05).
458 459
3.8. Comparison with other Estuaries around the world
460
Heavy metal and PAH concentrations of sediment samples from Musa Estuary were compared
461
with data reported for some other locations around the world, particularly from other parts of the
462
Persian Gulf (Table 8). The concentrations of Pb, Cu, and Zn in the Musa Estuary are lower than
463
those at Jobos Bay (the main anthropogenic sources include fire event and Tire-tread materials),
464
Nemrut Bay (enriched mainly by smelting and refining, steel-producing industries and additives
465
in gasoline) and Djiboty (mainly effected by sewage discharges and the electrical power station),
466
but higher than the Red Sea (with oil shipping, marine paints and terrigenous sediments derived
467
from basement rocks as the main sources). Compared with data obtained from other locations in
468
Persian Gulf, Cu concentrations are higher in the Musa Estuary except for the Hormoz Strait
469
where commercial waste and domestic discharges are the main anthropogenic sources.
470
Moreover, Zn concentrations in the study area are much higher than those at other locations in
16
471
the Persian Gulf. Concentrations of Ni and Cr in this study are relatively higher when compared
472
with those at other coasts (except Nemrut Bay for Cr, which is mainly originated from steel-
473
producing industries).
474
Considering the mean concentration of Hg, sediments of the Musa Estuary are much more
475
contaminated than Assaluyeh and Qatar Coasts, but higher mean concentration is observed in
476
Nemrut Bay, where the main sources of Hg are smelting and mining activities. However,
477
maximum Hg concentration in sediments of the eastern part of the petrochemical zone in Musa
478
Estuary is severely higher (up to 17952 µg/kg). Mining activities caused higher Hg
479
concentrations in some other areas such as Idrija- Slovenia (up to 610 mg/kg), West Jawa-
480
Indonesia (up to 22.68 mg/kg), Karaburun- Turkey (Up to 100 mg/kg) and Steamboat Creek-
481
USA (Up to 21.43 mg/kg) (Gemici and Oyman, 2003; Stamencovic et al., 2004; Hidayati et al.,
482
2009; Bavec et al., 2014). Furthermore, the Musa Estuary is more contaminated with PAHs than
483
other parts of the Persian Gulf including Assaluyeh Coast and Khark Island. Like the Musa
484
Estuary, in these two areas, oil spill, and combustion of fossil fuels and natural gas in oil refinery
485
and petrochemical complexes have been reported as the main sources of PAH contamination, but
486
it seems that due to the coarse texture of sediments, less PAHs are concentrated in Assaluyeh
487
Coast and Khark Island. The Musa Estuary has also higher PAHs concentrations than the Gulf of
488
Aden (where the PAHs are mainly originated from urban activities), and lower than Jobos Bay
489
(with tire recycling center and thermoelectric plant that generates oil-based energy), Yellow Sea
490
(with municipal sewage and untreated industrial wastewater), Lenga Estuary (with combustion of
491
fossil fuels as the main source) and Daya Bay (with emissions and effluents from power plants
492
and nuclear power stations).
493
Many factors including industries, commercial ship traffic, urban effluents, ignorance about the
494
environmental principles and improper environmental management all play a role in the high
495
contamination in the study area. Some of these sources are mentioned also for other areas. For
496
instance, alkyl lead additives for gasoline are an important Pb source in Nemrut Bay, and also
497
petrochemical companies producing gasoline in the Musa Estuary may use this compound. Also,
498
the same urban and industrial sources for studied metals and PAHs were mentioned. Moreover,
499
water flow direction (from south towards the Iranian coasts) and the finer sediments texture (due
500
to hydrological conditions) could also have a role in the higher sediment contamination by the
17
501
Iranian coast of the Persian Gulf as compared to Arabian coasts (Reynolds, 1993; Agah et al.,
502
2009; Delshab et al., 2017).
503 504
4. Conclusions
505
In the present study, the pollution status, potential sources and ecological risk of selected heavy
506
metals and PAHs in the surface sediments of the Musa Estuary were investigated. The results
507
reveal the efficiency of treatment lagoons in preventing discharge of contaminants (particularly
508
PAHs) into the Estuary. However, direct discharge of untreated wastewater from petrochemical
509
units into the Estuary has resulted in high contamination of bottom sediments. These sources
510
together with local fallout from atmospheric sources, qualify Musa Estuary as one of the most
511
contaminated areas in the Persian Gulf. Regarding the high PAHs contamination of the lagoons’
512
sediments, standard disposal is a priority. Dredging of bottom sediments in the Bandar Imam
513
Port, which is periodically performed, will change the physicochemical conditions and move the
514
contaminants, particularly Hg and PAHs, from sediments to the soluble phase in the water. This
515
could make the chemicals bioavailable to aquatic organisms, especially fish, and consequently
516
pose a potential threat to consumers. This is a matter of great concern due to high pollutant loads
517
in Musa Estuary as compared to other coastal areas in the Persian Gulf. Considering the
518
importance of the Persian Gulf for sailing (since shipping traffic is an important source of
519
contamination) and fishing, it will be interesting to determine the share of each of the eight
520
Persian Gulf’s states for contamination risk by calculating mass inventories. By identifying the
521
types and major sources of contaminants, it will be possible to take preventive measures to
522
reduce pollution to this important aquatic environment.
523 524
Acknowledgements
525 526 527
This research was financially supported by Bandar Imam Petrochemical Company. The authors wish to express their gratitude to the Research Committee and Medical Geology Center of Shiraz University for logistic and technical assistance.
18
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24
Table 1 UTM coordinates and texture of sediment sampling sites (Zone N38) HMs
PAHs
X
Y
Texture Clayey Loam Clayey Loam
S1
H1
295815
3357481
S2
-
301496
3356482
S3
H2
302928
3364916
Clayey Silt
S4
H3
311506
3364123
Clayey Silt
S5
-
317566
3363811
Clayey Loam
S6
H4
321955
3363651
Clayey Silt
S7
H5
323672
3366247
Clayey Silt
S8
H6
323357
3361766
Clayey Loam
S9
H7
324275
3370738
Clayey Silt
S10
-
328630
3370758
Silty Clay
S11
H8
313810
3376347
Silty Clay
S12
H9
314337
3373922
Silty Clay
S13
H10
314383
3371393
Silty Clay
S14
H11
311056
3370805
Silty Clay
S15
H12
308593
3373897
Silty Clay
S16
H13
313012
3368120
Clayey Silt
S17
H14
317026
3366416
Clayey Silt
S18
H15
327071
3373286
Silty Clay
Location Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary Musa Estuary
HMs
PAHs
X
Y
Texture
Location
S19
H16
317930
3371933
Silty Clay
Musa Estuary
S20
H17
318349
3370626
Silty Clay
Musa Estuary
S21
H18
319286
3369230
Silty Clay
Musa Estuary
S22
H19
318936
3367936
Silty Clay
Musa Estuary
S23
H20
321162
3374522
Clayey Silt
Musa Estuary
S24
H21
322093
3369855
Clayey Silt
Musa Estuary
S25
H22
415592
3330808
Clayey Silt
Persian Gulf
S26
H23
381276
3331237
Clayey Silt
Persian Gulf
S27
H24
281120
3321048
Silty Sand
Persian Gulf
S28
H25
276127
3307373
Clayey Loam
Persian Gulf
S29
H26
358244
3327376
Clayey Loam
Persian Gulf
S30
H27
297315
3322298
Silty Sand
Persian Gulf
S31
H28
331465
3335081
Silty Sand
Persian Gulf
S32
H29
317407
3370643
Silty Clay
Treatment Lagoon
S33
H30
317325
3372512
Silty Clay
Treatment Lagoon
S34
-
316398
3373590
Silty Clay
Treatment Lagoon
S35
H31
316015
3375330
Silty Clay
Treatment Lagoon
S36
H32
316114
3371665
Silty Clay
Treatment Lagoon
25
Table 2 Descriptive statistics of selected heavy metals and physicochemical parameters in surface sediment samples
Limit of Detection Musa Estuary and Persian Gulf Mean Lagoons Musa Estuary and Persian Gulf Median Lagoons Musa Estuary and Persian Gulf Std. Deviation Lagoons Musa Estuary and Persian Gulf Skewness Lagoons Minimum
Maximum
Variation coefficient
Musa Estuary and Persian Gulf Lagoons Musa Estuary and Persian Gulf Lagoons Musa Estuary and Persian Gulf Lagoons
Cu (mg/kg) 0.01
Pb (mg/kg) 0.01
Zn (mg/kg) 0.1
Ni (mg/kg) 0.1
Cr (mg/kg) 0.5
Al (%) 0.01
Hg (µg/kg) 5
CEC (meq/100g) -
OM (%) -
19.27
7.25
54.14
78.45
52.7
1.16
1629.68
34.99
20.6
8.53
181.98
68.66
46.52
1.11
104.4
18.41
6.43
48.5
79
52
1.09
17.73
8.38
73.8
69
47.2
3.84
3.45
16.49
9.11
7.9
2.60
227.14
0.72
5
2.07
-
EC (mS/cm) -
Sand (%) -
Clay (%) -
Silt (%) -
10.52
8.49
16.99
29.15
31.23
39.62
32.11
11.23
8.28
13.36
44.43
25.2
30.37
420
36.04
10.15
8.48
16.5
22.96
31.76
44
1.15
59
32.67
12.03
8.34
9.53
37.52
23.2
29.28
5.56
0.20
3820.1
3.69
3.27
0.16
7.17
22.36
11.19
12.79
8.6
6.12
0.09
116.95
2.94
2.66
0.28
11.91
13.77
11.40
7.11
1.91
-0.31
-0.19
0.06
3.42
-0.82
0.59
1.61
0.77
0.92
-0.35
-0.78
1.41
2.04
-0.02
0.38
-0.27
2
-0.77
-0.30
0.44
1.35
0.53
-0.4
0.79
12
5.04
34.6
56.7
39.4
0.75
99
23.61
5.7
8.23
5.32
0.8
3.2
4
15
6.11
36.4
59.2
40.3
1
25
27.63
7.67
7.91
2.97
30.8
9.2
22
29.76
25.19
111.4
95.8
64.1
1.57
17952
41.47
17.32
9.08
34.72
92.8
51.2
63.28
34.53
12.82
580.6
78.4
55
1.22
309
35.53
14.49
8.57
32.62
61.52
37.2
41.28
0.19
0.47
0.30
0.11
0.1
0.17
2.34
0.10
0.31
0.01
0.42
0.76
0.35
0.32
0.38
0.30
1.24
0.12
0.13
0.08
1.12
0.09
0.23
0.03
0.89
0.30
0.45
0.23
pH
Mean concentration in Earth crust*
26
15
66
20
155
8.2
55
-
-
-
-
-
-
-
PEL**
108.2
112.2
271
42.8
160.4
-
700
-
-
-
-
-
-
-
*
Kabata-Pendias and Mukherjee (2007)
**
Probable effect level
26
Table 3 Pearson’s correlation coefficients of metals and physicochemical parameters Ni Cr Al Cu Pb Zn Hg CEC OM pH EC sand clay silt
Ni
Cr
Al
Cu
Pb
Zn
Hg
CEC
OM
pH
EC
sand
clay
silt
1 0.97 0.92 0.44 0.22 0.18 0.28 0.12 0.37 -0.14 0.36 0.41 0.28 0.33
1 0.89 0.38 0.23 0.22 0.29 0.27 0.34 -0.12 0.34 -0.53 0.45 0.34
1 0.41 0.25 0.26 0.16 0.63 0.51 -0.25 0.44 -0.48 0.73 0.42
1 0.58 0.73 0.53 0.35 0.54 -0.52 0.33 -0.49 0.41 0.39
1 0.61 -0.02 -0.06 0.03 -0.24 0.02 -0.12 0.15 0.07
1 0.2 -0.02 0.32 -0.54 -0.01 -0.11 0.12 0.08
1 0.32 0.59 -0.09 0.43 -0.32 0.18 0.4
1 0.57 -0.29 0.53 -0.69 0.64 0.61
1 -0.54 0.53 -0.6 0.48 0.39
1 -0.32 0.35 -0.28 -0.36
1 -0.56 0.4 0.62
1 -0.91 -0.93
1 0.7
1
27
Table 4 Principal component analysis of the physicochemical parameters and heavy metals to reduce the dimensions and analyze relationships Component 1
2
3
Cu
0.35
0.48
0.67
Pb
0.10
0.73
0.14
Zn
-0.09
0.79
0.25
Ni
0.95
0.18
0.17
Cr
0.93
0.11
0.16
Al
0.89
0.24
0.09
Hg
-0.16
0.03
0.95
OM%
0.21
0.48
0.85
Sand
0.65
0.16
-0.14
Silt
0.33
0.42
0.17
Clay
0.28
0.59
0.49
28
Table 5 Descriptive statistics of PAHs in sediment samples (µg/kg)
Compound
Mean LOD
TEF
ERL
Median
Std. Deviation
Skewness
Minimum
Maximum
ERM Lagoon
Musa Estuary
Lagoon
Musa Estuary
Lagoon
Musa Estuary
Lagoon
Musa Estuary
Lagoon
Musa Estuary
Lagoon
Musa Estuary
Naphthalene (Np)
0.01
0.001
160
2100
23.04
28.53
1.4
4.8
43.28
88.09
2.17
4.87
ND
ND
100
460
Acenaphthene (Ace)
0.01
0.001
44
640
589.09
3.81
3.4
0.23
1184.54
10.47
2.20
3.33
ND
ND
2700
45
Fluorene (Fl)
0.01
0.001
19
540
499
4.7
2.7
0.23
1010
15.52
2.20
4.45
ND
ND
2300
78
Phenanthrene (Phe)
1.00
0.001
240
1500
4166
36
20
1.4
7827.24
97.77
2.11
3.15
0.5
0.2
18000
370
Anthracene (Ant)
0.10
0.01
853
1100
1222.96
2.21
2.8
0.2
2670.86
5.70
2.23
3.03
0.1
ND
6000
24
Fluoranthene (Flu)
1.00
0.001
600
5100
678.16
5.81
6.9
0.5
1167.58
11.65
1.92
2.37
0.3
0.3
2700
44
Pyrene (Pyr) Benzo[a]anthracene (BaA) Chrysene (Chr)
1.00
0.001
665
2600
443.82
29.62
8
5.6
603.17
62.03
0.67
2.86
3.8
2.7
1200
240
0.10
0.1
261
1600
2048.83
10.8
21
1.7
4445.79
22.47
2.23
2.97
ND
0.2
10000
99
1.00
0.01
384
2800
1548.14
8.25
16
1.2
3328.48
16.59
2.23
2.59
0.4
ND
7500
67
1.00
-
-
-
127.56
6.24
3.5
1.2
259.1
10.94
2.21
2.50
0.4
ND
590
47
0.1
320
1800
102.5
1.16
1.7
0.2
216.76
2.08
2.23
2.56
ND
ND
490
8.7
0.1
280
1620
228.31
3.83
2.7
0.6
487.52
7.35
2.23
2.52
ND
ND
1100
28
1
430
1600
114.68
0.56
0.2
0.2
254.53
1.33
2.24
4.90
ND
ND
570
7.1
1
63.4
260
17.57
2.93
1.9
2.1
36
2.10
2.23
1.53
ND
ND
82
8.5
0.01
430
1600
15.71
2.81
2.2
2.1
31.5
2.25
2.22
2.90
ND
ND
72
12
0.1
-
-
9.52
1.40
0.9
0.9
19.84
1.43
2.23
1.32
ND
ND
45
5.3
Benzo[e]pyrene (BeP) Benzo[b]fluoranthene (BbF) Benzo[k]fluoranthene (BkF) Benzo[a]pyrene (BaP) Dibenzo[ah]anthracene (DiBA) Benzo[ghi]perylene (BgPer) Indene[1,2,3-cd]pyrene (IndPy) ∑PAHs
0.10
-
-
-
-
11834.90
148.76
78.85
23.75
23385.83
326.60
2.18
3.35
13
9.48
53449
1514.3
LMW
-
-
-
-
6500.11
75.33
26.8
6.4
12716
201.77
2.17
3.84
1.95
1.65
29100
967
HMW
-
-
-
-
5334.79
73.42
59.05
17.30
10671.58
133.18
2.19
2.60
11
7.73
24349
547.3
1.00 0.10 0.50
0.10 0.01
LOD, Limit of Detection; ∑PAHs, total PAHs concentration; LMW, low molecular weight PAHs; HMW, high molecular weight PAHs; TEF, toxic equivalency factor for PAHs; ERL, effect range low; ERM, effect range medium.
29
Table 6 Principal component analysis of PAHs to reduce the dimensions and analyze relationships
Np Ace Fl Phe Ant Flu Pyr BaA Chr BeP BbF BkF BaP DiBA BgPer IndPy
Component 1 2 0.686 0.374 0.926 0.098 0.912 0.095 0.930 0.189 0.951 0.120 0.955 0.206 0.886 0.298 0.917 0.248 0.927 0.284 0.891 0.360 0.883 0.206 0.842 0.301 0.767 -0.035 0.132 0.968 0.048 0.971 0.401 0.783
30
Table 7 Mann-Whitney U test results for heavy metals and PAHs Mann-Whitney U Wilcoxon W Sig.
Cu
Pb
Zn
Ni
Cr
Al
Hg
∑PAHs
69 84 0.723
40 536 0.091
38 534 0.074
34 49 0.047
31.5 46.5 0.032
69.5 84.5 0.723
11 26 0.001
14 420 0.013
31
Table 8 Range (and mean) heavy metals and PAHs concentration in sediments from different locations Location
Cu (mg/kg)
Pb (mg/kg)
Zn (mg/kg)
Ni (mg/kg)
Cr (mg/kg)
Hg (µg/kg)
Musa Estuary (Persian Gulf) Assaluyeh Coast (Persian Gulf) Jobos Bay (Puerto Rico) Nemrut Bay (Turkey)
12.01-29.76 (19.27) 1.9-304.8 (15.43)
5.04-25.19 (7.25) 1-14.5 (3.39)
34.60-111.40 (54.14) 5.1-123.6 (21.08)
56.70-95.80 (78.45) 5.4-80 (19.04)
39.40-64.10 (52.70) 5.7-52.4 (16.13)
99-17952 (1629.68) 32-365 (116.38)
1.6-53 (29)
1.5-22 (11)
10.8-129 (64)
-
-
9.6-43.7 (29.5) 1-72.2 (36.6) 25-32.5 (27.5)
22.3-89.4 (60.4) 0.7-44.8 (22.65) 20-25 (22.50)
75-271 (182.9) 0.3-288.1 (144.2) 45-52.5 (48.8)
18.1-63.4 (50.4) 0.8-39.7 (20.25)
1.2-8.2 (4.4)
0.4-3.9 (2.4)
-
0.04-0.72 (0.38)
1.12-4.94 (2.56)
-
Djibouti-city Hormoz strait (Persian Gulf) Qatar Coast (Persian Gulf) Red Sea (Egypt) Yellow Sea (China) Lenga Estuary (Chile) Daya Bay (China) Gulf of Aden (Yemen) Assaluyeh Coast (Persian Gulf) Khark Island (Persian Gulf)
∑16 PAHs (µg/kg) 9.48-1514.3 (148.76)
Reference This study
-
Delshab et al., 2017
40.4-1912 (593.12)
Aldarondo-Torres et al., 2010
35.7-98.8 (69.6) 1.9-63 (32.45)
1700-9600 (5750)
-
Esen et al., 2010
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Ahmed et al., 2017
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Bastami et al., 2015
11.5-40.8 (27.1)
1.1-6.7 (1.7)
-
De-Mora et al., 2004
5.26-12.36 (7.66)
0.7-20.8 (11.2) 1.40-4.83 (3.16)
-
-
-
Nour et al., 2006
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
32
52.3-1870.6 (472) 290-6118 (2025) 340-710 (480) 2.2-604 (82.36) 12.8-81.25 (28.6) 2.95-253.30 (71.87)
Jiao et al., 2012 Pozo et al., 2011 Sun et al., 2016 Mostafa et al., 2009 Keshavarzifard et al., 2017 Akhbarizadeh et al., 2016
Fig. 1 Map of the study area showing location of the sampling sites.
Fig. 2 Box plot showing enrichment factor of heavy metals
Fig. 3 Ecological risk of individual metals and potential ecological risk in sediment samples
Fig. 4 Bar graph of calculated mean PEL quotient for heavy metals
Fig. 5 Ternary diagram of PAH compositions in sediments
Fig. 6 Bar graph of PAHs’ toxic equivalents for sediment samples in the study area
Highlights • • • • •
Persian Gulf is threatened by contaminants from industrial and shipping activities. Sediments of Musa estuary are highly contaminated by PAHs and HMs (especially Hg). Contaminants originating from petrochemical zone pose high ecological risk to aquatic life. The Estuary has a high potential for contaminating the marine environment. Treatment lagoons have a great role in reducing metal and PAH concentrations.
Declaration of interests ☒ The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper. ☐The authors declare the following financial interests/personal relationships which may be considered as potential competing interests: