3.1 PAHs analysis
PAHs compounds are an important group of POPs containing two or more condensed aromatic rings. PAHs tend to be associated with organic carbon in aquatic media due to their hydrophobicity and then deposited in sediments which are their major reservoirs in the marine environments (Abdollahi et al. 2013, Barakat et al. 2013). The Environmental Protection Agency (USEPA) involved 16 PAHs as precedence control pollutants (Criteria and Office 1993), and over half of these PAHs are potentially carcinogenic to humans, according to the International Agency for Research on Cancer (IARC) (Cancer 2010) and the US EPA.
The mean concentrations level of 16 PAHs (µg/kg) in sediment samples of different MPAs are presented in Table 2. The mean levels of naphthalene, fluorene, phenanthrene, pyrene, and benzo (a) pyrene in different stations were statistically significantly different (p-value < 0.05). Results showed that total concentrations of 16 PAHs varied from 4.65 to 20.86 µg/kg dry weight (dw) (Table 2). The highest concentrations of Σ16PAHs were detected in station M2 (20.86), followed by station H1 (17.80), while the lowest concentrations were found in station NB1 (4.65), followed by M1 (6.0). M2 and H1 located in the Mond and Heleh Estuary mouth, respectively. Adjacent agricultural and aquaculture fields can be one of the reasons for the increase of PAHs in these stations. Also, there are motorboat fishing activities that PAHs could be released due to the accidental petroleum spills of a boat, discharge of fuel, or motorboats residues. Added to this, the discharge from the Mond and Helleh rivers might also have a role in this increase. Additional research will be required to assess and compare the contribution of these factors in the Mond and Helleh MPAs. According to Montuori et al., different sources can contribute to the formation of PAHs in the marine environment, which includes industrial effluents, sewage, oil spills, runoff, and atmospheric fallout (Montuori et al. 2022).
The PAHs composition and distribution in the sediments influenced by sediment characteristics such as TOM content and grain size (Baran et al. 2017). Stations H1 and M2 (Table 1) displayed a predominance of fine sediments (silt/clay), with values higher than 90%, and lower content of larger particles (sand). The higher PAH concentration detected in these stations corresponded to the higher fine fraction content in the samples (silt/clay). Also, the highest TOM content (Table 1) was found in these stations suggesting that TOM plays an essential role as a driver of PAH accumulation in these points.
The PAHs concentrations in this study were lower than those reported in sediments from other MPAs worldwide. The PAH concentrations in sediments from Goiana estuary, Brazil, were < LOD-156.4 µg/kg (de Arruda-Santos et al. 2018); in Mosaic of MPAs of Sao Paulo State, Brazil were < LOD-180.6 µg/kg (Moreira et al. 2019); 0.7 to 140 µg/kg in Spain (Cortazar et al. 2008); and 2.94-199.08 µg/kg in St. John, US Virgin Islands (Whitall et al. 2015). In a study by Perra et al. (2011), the total PAH concentrations ranged from 0.71 to 1550 µg/kg in surface sediment from 15 Italian MPAs (Perra et al. 2011). In another study by Oliva et al. (2020), total concentration of the PAHs in MPAs within the Argentinean Continental Shelf was ranged from 19.47 to 183.17 µg/kg and low molecular weight PAHs (anthracene and naphthalene) were predominant (Oliva et al. 2020). In Yim et al. (2007) study, total concentration of PAHs were in the range of 8.80–18500 µg/kg, and industrialized and urbanized areas exhibited a high amount of PAHs (Yim et al. 2007). The previous PAHs monitoring studies mainly focused on the polluted coastal region, and industrialized and urbanized areas, and MPAs have received less attention. Due to the ecological importance of MPAs in protecting critical habitats and representative samples of maritime life and assisting in restoring the productivity of the oceans and avoiding more degradation, continuous monitoring of these areas is necessary.
Considering all samples, the composition patterns of 16 priorities PAH congeners are as follows: 5-ring > 2-ring > 4-ring > 3-ring (see Fig. 2). The 6-ring PAHs were not seen in any of the stations (except station H1 in a small amount). Comparing the concentration levels of PAHs in sediment samples based on the frequency of rings showed that the distribution patterns is different among the studied stations (Fig. 2). The 4- and 5-ring PAHs were most dominant in stations M1, M2, H1, H2, NL2, and NB1. In contrast, the 2- and 3-ring structures were highest in stations NL1 and NB2. In general, petrogenic PAHs (e.g., from fossil fuels) present dominance of compounds with lower molecular weight PAHs-LMW (2–3 rings), while pyrogenic PAHs (e.g., those produced by burning processes) are dominated by higher molecular weight PAHs-HMW (4–6 rings) (Oliva et al. 2020). To expand this analysis, a molecular-ratios approach was applied to address pyrogenic and petrogenic sources. The following ratios were used: Fluoranthene/(Pyrene + Fluoranthene), Anthracene/(Anthracene + Phenanthrene), and LMW/HMW. Fluoranthene/ (Pyrene + Fluoranthene) values < 0.40 suggest petroleum origin, whereas values > 0.4 are indicators of combustion. Furthermore, values between 0.40 and 0.50 show liquid fossil fuel combustion, while ratios higher than 0.50 are attributable to biomass combustion (Yunker et al. 2002). For Anthracene/(Anthracene + Phenanthrene) ratios, pyrogenic sources indicate values higher than 0.10, whereas petrogenic PAHs show values < 0.10. Lastly, LMW/HMW ratios < 1 indicate pyrogenic source whereas values > 1 present petrogenic source (Yuan et al. 2001, Yunker et al. 2002). Table 2 shows the ratio of An/(Phe + An) > 0.1 for all locations, Flu/ (Flu + Py) < 0.40 (except NL1), and LMW/HMW < 1, indicating that the primary PAH source was mainly from pyrogenic origin. Only NL1 and NB2 present values of LMW/HMW > 1, which showed a petrogenic source at these sampling sites. Considering the PAH molecular ratios and ring's pattern, a mixed source with a pyrogenic fingerprint dominance was detected for sediments of the Persian Gulf's MPAs.
Table 2
The mean concentrations levels of PAHs (µg/kg) in sediments of marine protected areas.
PAHs | M1 | H2 | NL1 | NB1 | NB2 | NL2 | M2 | H1 | p-value | LOD | LOQ |
Naphthalene | < LOD | 3.21 | < LOD | < LOD | 5.74 | 3.81 | 8.08 | 4.63 | 0.045 | 0.464 | 1.547 |
Acenaphthylene | 0.03 | 0.09 | < LOD | < LOD | 0.06 | 0.05 | 0.15 | 0.04 | 0.125 | 0.008 | 0.028 |
Acenaphthene | < LOD | < LOD | 1.40 | < LOD | < LOD | < LOD | < LOD | 1.10 | 0.545 | 0.321 | 1.070 |
Fluorene | < LOD | < LOD | 1.78 | < LOD | 0.84 | < LOD | < LOD | 1.02 | 0.048 | 0.044 | 0.15 |
Phenanthrene | 0.71 | 0.72 | 2.32 | 0.58 | 0.85 | 0.72 | 0.91 | 0.76 | 0.015 | 0.046 | 0.152 |
Anthracene | 0.59 | 0.75 | 0.74 | 0.54 | 0.92 | 1.04 | 1.20 | 1.10 | 0.063 | 0.074 | 0.247 |
Fluoranthene | 0.41 | 0.59 | 1.91 | 0.31 | 0.44 | 0.28 | 0.40 | 0.83 | 0.055 | 0.018 | 0.060 |
Pyrene | 1.49 | 5.03 | 2.60 | 1.49 | 1.77 | 1.28 | 1.42 | 1.96 | 0.008 | 0.025 | 0.082 |
Benz(a) Anthracene | 0.29 | 0.24 | 0.11 | 0.31 | 0.24 | 0.26 | 0.32 | 0.25 | 0.112 | 0.011 | 0.036 |
Chrysene | 0.19 | 0.11 | < LOD | 0.09 | 0.08 | 0.11 | 0.18 | 0.08 | 0.088 | 0.015 | 0.050 |
Benz(b)Fluoranthene | 0.27 | 0.26 | < LOD | 0.16 | 0.20 | 0.46 | 0.76 | 0.50 | 0.064 | 0.044 | 0.148 |
Benzo(k)Fluoranthene | 0.14 | < LOD | < LOD | < LOD | < LOD | 0.11 | 0.14 | 0.14 | 0.077 | 0.03 | 0.094 |
Benzo(a)Pyrene | 1.87 | 1.68 | 0.56 | 1.17 | 1.53 | 4.10 | 7.29 | 4.69 | 0.004 | 0.03 | 0.107 |
Indenol (1.2.3-cd)Pyrene | < LOD | < LOD | < LOD | < LOD | < LOD | < LOD | < LOD | 0.37 | 0.061 | 0.07 | 0.248 |
Dibenzo(a,h) Anthracene | < LOD | < LOD | < LOD | < LOD | < LOD | < LOD | < LOD | < LOD | 0.215 | 0.10 | 0.336 |
Benzo (g.h.I) Perylene | < LOD | < LOD | < LOD | < LOD | < LOD | < LOD | < LOD | 0.30 | 0.111 | 0.09 | 0.300 |
An/(An + Phe) | 0.45 | 0.51 | 0.24 | 0.48 | 0.52 | 0.59 | 0.57 | 0.59 | - | - | - |
Flu/ (Py + Flu) | 0.22 | 0.10 | 0.42 | 0.17 | 0.20 | 0.18 | 0.22 | 0.30 | - | - | - |
LMW/HMW | 0.29 | 0.60 | 1.20 | 0.32 | 1.97 | 0.85 | 0.98 | 0.95 | - | - | - |
All PAHs had lower concentrations than the Effects Range-Low (ERL) and Effects Range-Median (ERM) values suggested by Long et al. (Long et al. 1995). The concentration levels of individual PAHs in our study varied from < LOD to 8.08 µg/kg, and were much lower than both of the ERL and ERM values (Table S1).
3.2 TPH analysis
Results showed spatial distribution of TPHs compound in the sediments was not homogenous and varied from 5.21 to 17.90 µg/g dw (Table 3). The mean concentrations of TPHs in different stations was statistically significantly different (p-value < 0.05). The highest value of TPHs were found at station M2 (17.90 µg/g dw) and H1 (15.94 µg/g dw), located in the Mond and Helleh Estuary mouth, respectively. The lowest levels were detected at the station NL1 (5.21 µg/g dw). The different pattern indicates the contribution of the anthropogenic sources to the TPH loads in the MPAs' coastal water. These sources may include adjacent agricultural and aquaculture activities, motorboat fishing activities, occasional oil spills, and land-based runoffs from Mond and Helleh rivers. Also, the results showed that TOM and a fine fraction of sediments (silt + clay) were effective parameters in controlling the alteration of TPH in the station M2 and H1. Smaller particles of sediments (e.g., muddy sediment) are frequently indicate more organic content and accumulate more organic pollutants (17).
Massoud et al. (1996) proposed that TPH contents in sediment in the range of 10 to 15 µg/g and 15 to 50 µg/g should be considered unpolluted and slightly polluted, respectively (17). Moreover, TPH concentrations that are less than 15 µg/g dw were considered the natural background levels for bottom sediment by ROPME (de Mora et al. 2010). According to these classifications, the sediment samples in Bushehr Province’s MPAs categorized between unpolluted and slightly polluted areas. Thus, stations M2, H1, NL2, and NB2 can be considered as vulnerable stations.
Based on Arzaghi et al. (2018) study, ecological risk assessment was done (Arzaghi et al. 2018). The hazard quotient (HQ) ≥ 1 indicates high risk; (HQ) < 1 is medium risk; and (HQ) < 0.1 indicate low risk (Tian et al. 2020). HQ is obtained by dividing the measured environmental concentration of specific hydrocarbon by the toxicity reference value. The toxicity reference values for sediment was 5.54 mg/kg for C14 – C18 and 9.88 mg/kg for C19 – C36 (Mean and Log 2007). The values of HQ are less than 1 in all stations (Table 3).
Table 3
Mean concentrations of TPHs (µg/g) and hydrocarbon indexes in the sediment for individual hydrocarbon.
TPHs | M1 | H2 | NL1 | NB2 | NL2 | NB1 | M2 | H1 |
C10 | 0.001 | 0.121 | 0.000 | 0.232 | 0.178 | 0.000 | 0.138 | 0.212 |
C11 | 0.000 | 0.005 | 0.000 | 0.001 | 0.002 | 0.000 | 0.005 | 0.004 |
C12 | 0.002 | 0.268 | 0.003 | 0.439 | 0.445 | 0.000 | 0.524 | 0.418 |
C13 | 0.000 | 0.008 | 0.005 | 0.007 | 0.005 | 0.000 | 0.006 | 0.008 |
C14 | 0.105 | 0.371 | 0.116 | 0.467 | 0.518 | 0.060 | 0.550 | 0.449 |
C15 | 0.001 | 0.003 | 0.003 | 0.001 | 0.002 | 0.001 | 0.003 | 0.003 |
C16 | 0.188 | 0.189 | 0.096 | 0.206 | 0.230 | 0.207 | 0.248 | 0.201 |
C17 | 0.002 | 0.003 | 0.003 | 0.005 | 0.003 | 0.005 | 0.003 | 0.003 |
C18 | 0.169 | 0.132 | 0.072 | 0.147 | 0.157 | 0.180 | 0.179 | 0.144 |
C19 | 0.001 | 0.002 | 0.001 | 0.002 | 0.002 | 0.002 | 0.002 | 0.002 |
C20 | 0.121 | 0.089 | 0.049 | 0.097 | 0.106 | 0.125 | 0.126 | 0.095 |
C21 | 0.005 | 0.004 | 0.002 | 0.004 | 0.004 | 0.005 | 0.005 | 0.005 |
C22 | 0.073 | 0.056 | 0.030 | 0.060 | 0.066 | 0.077 | 0.078 | 0.061 |
C23 | 0.007 | 0.005 | 0.003 | 0.005 | 0.006 | 0.003 | 0.008 | 0.006 |
C24 | 0.054 | 0.043 | 0.024 | 0.046 | 0.050 | 0.059 | 0.057 | 0.047 |
C25 | 0.011 | 0.010 | 0.006 | 0.011 | 0.012 | 0.012 | 0.014 | 0.012 |
C26 | 0.051 | 0.041 | 0.022 | 0.043 | 0.047 | 0.055 | 0.055 | 0.046 |
C27 | 0.022 | 0.015 | 0.009 | 0.016 | 0.016 | 0.019 | 0.020 | 0.022 |
C28 | 0.083 | 0.066 | 0.033 | 0.067 | 0.070 | 0.082 | 0.083 | 0.068 |
C29 | 0.070 | 0.027 | 0.019 | 0.030 | 0.028 | 0.034 | 0.048 | 0.075 |
C30 | 0.063 | 0.046 | 0.026 | 0.046 | 0.052 | 0.052 | 0.054 | 0.050 |
C31 | 0.061 | 0.014 | 0.016 | 0.020 | 0.020 | 0.019 | 0.036 | 0.063 |
C32 | 0.046 | 0.037 | 0.019 | 0.037 | 0.040 | 0.033 | 0.042 | 0.034 |
C33 | 0.034 | 0.010 | 0.007 | 0.010 | 0.011 | 0.010 | 0.021 | 0.031 |
C34 | 0.020 | 0.018 | 0.008 | 0.016 | 0.018 | 0.010 | 0.017 | 0.013 |
C35 | 0.009 | 0.009 | 0.003 | 0.009 | 0.008 | 0.006 | 0.011 | 0.010 |
C36 | 0.007 | 0.008 | 0.003 | 0.007 | 0.008 | 0.004 | 0.007 | 0.005 |
TPHs concentration | 11.51 | 17.9 | 10.27 | 15.19 | 15.94 | 12.56 | 5.21 | 15.89 |
The concentration of TPHs in the current study compared with the results of other regions with similar climate. The concentration of TPH in the studied area is significantly lower than the surface sediments of Imam Khomeini port (32.73–97.15 µg/g dw), a semi-closed ecosystem with limited connection to the PG (Jazani et al. 2013). Due to the extensive activity and high traffic of vessels carrying fuel and other export goods in this port, as well as the lack of its self-remediation capacity, the concentration of suspended solids and pollutants was high. The TPH concentrations in the Musa Bay (Northwest of PG) sediments varied from 16.48 to 97.15 µg/g dw with the mean value of 48.98 ± 30.36 µg/g dw (Jazani et al. 2013). The highest concentrations detected in stations adjacent to the coastline, which affected by severe petrochemical discharges and shipping activities. The concentration of TPH in sediments of the PG and Omani waters varied between 0.134 and 48,018 µg/g dw (Uddin et al. 2021). The TPH detected values ranged from 7.43 to 458.61 µg/g in the sediments of Kuwait’s coastline (Metwally et al. 1997).
The concentrations obtained in the current study are relatively higher than the concentration of TPHs of the northern parts of the Oman Sea, 0.10–4.10 µg/g dw (de Mora et al. 2010), Arvand River, 2.46–3.83 (Al-Saad 1995), coastline (ND to 1.71 µg/g dw) and mangroves (0.2 to 0.63 µg/g dw) sediments of the northern PG (Mohebbi-Nozar et al. 2015), and Tiab mangroves, Hormozgan province, Iran, 0.36 to 4.89 µg/g (Zahedi Dehuii et al. 2019). Globally, the TPH levels in the sediments of this study were significantly lower than those from other coastal areas like Algoa Bay in the Eastern Cape Province of South Africa (0.72 to 27.03 µg/g) (24); Newark Bay Estuary, New Jersey, USA (240 to 280 µg/g) (Huntley et al. 1995); and Barnegat Bay-Little Egg Harbor Estuary, New Jersey (47 to 1003 µg/g) (Vane et al. 2008). However, sediment from a few other places around the world discovered TPH concentrations that were comparable to those reported in the present study. Examples include those from Todos os Santos Bay, Brazil, 1.60 and 10.60 µg/g dw (de La Habana 2009).
3.3 PCBs analysis
18 PCB congeners, including eight mono-ortho PCBs 189, 167, 157, 156, 123, 118, 114, 105, four non-ortho PCBs 169, 126, 81, 77, and six indicator PCBs 180, 153, 138, 101, 52, 28 measured since they are the most toxic compounds and have a common mode of function. The mean concentrations of 18 PCBs (ng/g dw) in sediments of different MPAs presented in Table S2. The highest concentration of ΣPCBs is at NL2 (0.419 ng/g dw), followed by NB1 (0.413 ng/g dw), and the lowest concentration of PCBs is observed at H2 stations (0.345 ng/g dw). Among the 18 PCB congeners analyzed, the main components correspond to PCB-77, PCB-105, PCB-81, PCB-101, and PCB-114 (Fig. 3). The mean levels of PCB-28, PCB-52, PCB-123, PCB-118, PCB-157, and PCB-169 in different stations were statistically significantly different (p-value < 0.05). The mean concentration of ∑18PCB measured in the surface sediments of different MPAs (0.345–0.419 ng/g dw) was low compared to other marine environments such as Lake Chapala, Mexico (9–27 ng/g dw) (Ontiveros-Cuadras et al. 2019), San Diego Bay, southern California (23-1387 ng/g dw) (Neira et al. 2018), Pearl River Estuary, China (17.68-169.26 ng/g dw, (Zhao et al. 2016), Pearl River Delta, China (16.15-477.85 ng/g dw, (Wang et al. 2019), the coastal area of Bangladesh (32.17–199.4 ng/g dw) (Habibullah-Al-Mamun et al. 2019), Southern Yellow Sea (0.51–5.84 ng/g dw, (Zhang et al. 2007), Bengal Bay, India (0.019-6.5 ng/g dw, (Rajendran et al. 2005), Hugli estuary, India (0.18–2.33 ng/g dw, (Guzzella et al. 2005), coastal surface sediment, Hormozgan Province, Iran (0.88-461.97 ng/g dw, (Nozar et al. 2014), and Larak Island, Iran (2.95 to 7.95 ng/g dw) (Ranjbar Jafarabadi et al. 2019). Our results indicated that the sediments collected from the studied MPAs were much less polluted than Shadegan Wetland, Khoozestan Province, Iran, which is known as one of Iran’s industrial polluted zones. The total of 7 congeners concentrations of PCBs in sediment of 4 stations around Shadegan wetland protected area in the northwestern PG was from 3400–50200 ng/g dw, and the mean value was 18220 ng/g dw (Zahed et al. 2009).
However, the concentrations of PCBs were comparable to values reported in Tokyo Bay, Japan (0.04–0.64 ng/g dw, (Kobayashi et al. 2010), Laguna de Terminos, a protected area of the coast of Campeche, Mexico (0.016–0.36 ng/g dw) (57), Belgian coastal harbors (0.03–3.1 ng/g dw) (Monteyne et al. 2013), and Liaohe River protected area, China (0.08–0.36) (55). Arfaeinia et al. (2017) investigated levels of PCBs in the sediments of Asaluyeh harbor, the northern PG. The average concentration of ∑18PCB were 0.51, 0.14, and 0.031 ng/g dw for the industrial, semi-industrial and urban stations, respectively (Arfaeinia et al. 2017).
3.4 Trace metals analysis
Trace metals in sediments and seawater can be absorbed by aquatic organisms directly. Subsequent accumulation within their bodies may be magnified through the food chain, thus threatening the marine ecosystem and human health (Zhang et al. 2015). The average concentrations levels of trace metals and metalloids (arsenic and antimony) in sediments of different MPAs presented in Table 4. The concentration of metals ranged as follows: Arsenic (As): 4.79–9.69; Cobalt (Co): 2–12 µg/g; Chromium (Cr): 39–142 µg/g; Nickel (Ni): 18–90 µg/g; Vanadium (V): 15–58 µg/g; Magnesium (Mn): 184–425; Lead (Pb): 7-459 µg/g; Zinc (Zn): 6-424 µg/g; Copper (Cu): 4–20; Aluminum (Al): 0.75–4.12%; Iron (Fe): 0.35–1.62%. The concentration of Cadmium (Cd), Silver (Ag), Molybdenum (Mo), Mercury (Hg), and Antimony (Sb) was below the limit of detection. The mean levels of Co, As, Cr, Cu, Mn, Ni, V, Al, and Zn in different stations were statistically significantly different (p-value < 0.05). The Mn, Cr, Zn, and Pb were the primary trace metals in sediments of the studied MPAs. The highest concentration for most of the trace elements was found in sediments from station H1 followed by M1 and NL1, and the lowest concentration was at station NB2. Agriculture and aquaculture are the most important activity in H1 and M1 area. A similar finding attained by Guo et al. (2021), that the principal source of contamination of Cd, Zn, Pb, and Cr was agriculture. Long-term usage of phosphate fertilizer will result in the accumulation of Pb and Cr, which also occur at high levels in fertilizers (Guo et al. 2021).
Table 4
The mean concentrations levels of trace metals (µg/g) and Al, Fe (%) in sediments collected from marine protected areas.
Stations | Ag | As | Al | Fe | Mo | Cd | Co | Cr | Cu | Hg | Mn | Ni | V | Pb | Zn |
NB2 | <LOD | 8.25 | 0.75 | 0.35 | <LOD | <LOD | 2 | 45 | 4 | <LOD | 184 | 18 | 15 | 9 | 7 |
H1 | <LOD | 6.02 | 4.12 | 1.62 | <LOD | <LOD | 12 | 103 | 20 | <LOD | 352 | 90 | 58 | 9 | 37 |
H2 | <LOD | 9.69 | 0.76 | 0.44 | <LOD | <LOD | 3 | 39 | 5 | <LOD | 222 | 20 | 16 | 7 | 6 |
M2 | <LOD | 5.33 | 2.77 | 1.15 | <LOD | <LOD | 9 | 142 | 13 | <LOD | 400 | 61 | 42 | 8 | 26 |
M1 | <LOD | 4.79 | 3.36 | 1.31 | <LOD | <LOD | 10 | 83 | 17 | <LOD | 425 | 73 | 47 | 9 | 28 |
NL1 | <LOD | 6.21 | 3.08 | 1.28 | <LOD | <LOD | 9 | 120 | 16 | <LOD | 381 | 67 | 47 | 459 | 424 |
Mean | - | 6.71 | 2.47 | 1.02 | - | - | 7.50 | 88.67 | 12.5 | - | 327.33 | 54.83 | 37.5 | 83.5 | 88 |
ERLa | 1.0 | 8.2 | - | - | - | 1.2 | - | 81 | 34 | 0.15 | - | 20.9 | - | 46.7 | 150 |
ERMa | 3.7 | 70 | - | - | - | 9.6 | - | 370 | 270 | 0.71 | - | 51.6 | - | 218 | 410 |
Not pollutedb | - | < 3 | - | - | - | - | - | < 25 | < 25 | - | < 300 | < 11 | - | < 40 | < 90 |
Moderately pollutedb | - | 3–8 | - | - | - | < 6 | - | 25–75 | 25–50 | - | 300–500 | 12–56 | - | 40–60 | 90–200 |
Heavily pollutedb | - | > 8 | - | - | - | > 6 | - | > 75 | > 50 | - | > 500 | > 57 | - | > 60 | > 200 |
aERL and ERM for trace metals (µg/g) recorded in sediment according to Long et al. (Long et al. 1995) |
bUS Environmental Protection Agency (Agency 1987) |
The high concentration of trace metals in the stations located in the Helleh estuary (H1) and Mond River (M1) could be caused by the high percentage of small mud particles (silt + clay) in these stations (Table 1). Fine-grained sediments, with higher surface-to-volume ratios, have more potential to remove inorganic and organic pollutants from the water column. Generally, fine sediments with more organic content keep more pollutants than moderately coarse sand sediments (De Mora and Sheikholeslami 2002). Metwally et al. (1997) stated the highest concentration of nickel and vanadium in the coastal sediments of Kuwait was related to the stations whose sediments were muddy (Metwally et al. 1997).
According to the US Environmental Protection Agency (Table 4), the stations NL1, M1, M2, and H1 have recorded a high degree of Cr and Ni contamination and the other stations indicated moderate contamination. The Cr concentration was higher than the ERL but lower than the ERM values. The station NL1 showed a high level of Zn contamination, and Zn concentration was higher than both of the ERL and ERM values. The concentration of Mn in the sediments of NL1, M1, M2, and H1 with moderate contamination is significant. The stations NB2 and H2 showed a high level of As contamination, and the other stations indicated moderate contamination.
Trace metal concentrations in the current study compared with other regions in the PG, other parts of the world, and some standards of other countries (Table S3). The mean concentrations of Zn, Cr, Co, Ni, Mn, and V from our studied area were lower than sediments from Kuwait (Basaham and Al-Lihaibi 1993). The Fe concentration in the current study was lower than in the Strait of Hormuz, Kuwait, Bidkhun mangrove, and Black Sea, but more than in Nayband Bay, Bostaneh, Saudi Arabia, and Bahrain/Qatar (Table S3). The average Fe concentration was less than existing guidelines, as well (Guidelines for Metals in sediments, SEL and LEL).
The Co concentration in this study was less than its concentration in Kuwait and Mahshahr but higher than coastal sediments of the PG, Saudi Arabia, Bahrain/Qatar. The concentration of As was consistent with the result of an earlier study in the coastal sediments of the PG by de Mora et al. 2004. The As concentration was lower than Bidkhun mangrove, Guidelines for Metals in sediments (SEL), and Primary and Secondary China National Standard (Table S3). Unpolluted coastal sediments usually have As concentrations of 5–15 µg/g (Neff 1997). The Cr concentration was more than protected areas in Poland, Saudi Arabia, and Bahrain/Qatar and lower than the coastal sediments of the southern part of the PG and Kuwait. Cu concentration was more than its concentration in the region (Bushehr, Strait of Hormuz, Saudi Arabia, Bahrain/Qatar) but lower than the global standards mentioned in Table S3. Ni concentration was lower than SEL, Mahshahr (Iran), and Kuwait but higher than LEL, coastal sediments of southern PG, Saudi Arabia, Bahrain/Qatar, Nayband Bay, Strait of Hormuz, Bostaneh (Iran), and other regions far from the PG (Black Sea, Red Sea, protected areas, Poland). The average Ni concentration in the studied sediment (54.83 µg/g) was close to the adjacent region of Bidkhun mangrove (56 µg/g).
The mean concentration of V was more than the concentrations achieved in the other places of the PG, such as coastal sediments of southern PG, Saudi Arabia, and Bahrain/Qatar. Other studies have shown more concentration of V in Nayband Bay, Bidkhun mangrove, and Kuwait. According to some standards including, Primary China National Standard, Secondary China National Standard, Guidelines for Metals in sediments (LEL and SEL), and Canadian sediment quality guidelines (TEL), the mean Pb concentration in all studied stations (except NL1) was lower than the standard level (Table S3). The Pb concentration in this study was lower than its concentration in other marine regions (Bidkhun mangrove, Nayband Bay, Strait of Hormuz, Mahshahr, and sediments of southern PG) but higher than Bahrain/Qatar and Bostaneh (Iran). The mean Pb value in the sediments of station NL1 (see Table 4) exceeded all of the global standards and other marine regions. The reason for high concentration of lead in this station can be caused by the fossil fuels used for fishing and recreational motor vessels. Lead is also present in paint combinations, including the colors used for the hulls of ships and boats (CCREM 1987). Similar to Pb, the mean Zn concentration in all studied stations in Table 4 (except NL1) was lower than its levels in other marine regions and global standards (Table S3). Relatively high concentrations of Pb and Zn were observed in station NL1, supporting the hypothesis of a point source of pollution at this station, the effects of which reduce with distance from the source.