3.1 Spatial distribution, seasonal variation, and potential sources of pollution
The concentrations range for Ʃ5PBDEs were 25.3–785 ng/L (Ʃ5PBDEs 329 ± 48.3 ng/L) in spring water samples and 30.1–110 ng/L (Ʃ5PBDEs 62.1 ± 1.50 ng /L) in summer water samples across the sites (Table 2). The PBDEs concentrations across the points of collection from the two matrices were significantly different (p < 0.05). This can be attributed to non-uniformity of the activities at the sampling sites. Points NH1 and NH2 are closer to the creek, which is a point of discharge to the Estuary, NH3 is characterized by its leisure activities, and road activities at point NH5 under the bridge. This variation probably contributed to differences in the concentrations of PBDE. The PBDEs concentrations in the spring water samples were higher than the summer samples. This could be attributed to atmospheric wet deposition and also the heavy runoff of foul-smelling stormwater on the sampling day (Luo et al., 2014; Zhan et al., 2019). With spring being a raining (wet) season in South Africa and windy, both wet and dry depositions are possible, especially in the coastal environment. Higher rainfall always support more of wet deposition than dry ones (Castro-Jiménez et al., 2011; Cetin et al., 2016; Mai et al., 2005). The highest contamination was observed in the spring water sample at NH1 with BDE- 17, 47, and 100 detected at 247, 190, and 178 ng/L, respectively (Table S4); suggesting ubiquitous usage of the commercial penta-BDE at the area (La Guardia et al., 2006). This dominance was also reported elsewhere with BDE-17, 47 and 100 at concentrations 2.0, 5.8, and 0.4 ng/L (Olisah et al., 2020a). This heavy pollution is attributed to a heavy fresh discharge observed at the creek (NH1) on sampling day. The water sample concentration of BDE- 17 was below the detection limit in NH4 in spring, NH3, NH4, and NH5 in summer season but relatively higher in NH5 in spring (137 ng /L) (Table S4). This variance could be as a result absence of microbial degradation as BDE-17 is a one of the major products of microbial degradation of high molecular weight PBDEs in the environment (Trinh et al., 2019). Point NH5 is a rocky steep under the bridge and occupied by some homeless individuals and characterized by vehicular emission and careless garbage dump by the road users (Anh et al., 2018; Ohoro et al., 2021). The anthropogenic waste could be why there was a higher concentration at this spot (Zhou et al., 2021) than at NH3 and NH4, which are closer to the potential most polluted area of this sampling site.
The Ʃ6PBDEs in spring sediment samples was 1.91–6.57 ng/g (Ʃ6PBDEs 4.19 ± 0.35 ng/g dw), and 1.98–235 ng/g (Ʃ6PBDEs 65.4 ± 15.9 ng/g dw) in summer sediment samples (Table 2). The sediment concentration of PBDEs was relatively higher in summer than in spring, higher temperature in spring notwithstanding; contrary to previous studies, which reported no detection of PBDE concentrations of sediments (Nouira et al., 2013), and higher concentration in summer season than spring (Hansson et al., 2006; Khairy and Lohmann, 2017). Similar report was documented on high summer concentration (Hansson et al., 2006). This could be attributed to atmospheric wet deposition (Tlili et al., 2012) and high turbidity observed in summer, preventing photodegradation (Fang et al., 2008; Pan et al., 2016). Estuarine sediment acts as a vital sink of PBDEs originated by several anthropogenic activities (Díaz-Jaramillo et al., 2016), though lesser concentrations in sediments compared to water was observed. Lower concentration of sediment than water is likely as a result of dilution of overlying water as also reported elsewhere (Chen et al., 2009). BDE- 17 and 66 showed the relatively highest concentrations in all sampling points, suggesting PBDE contaminants from an industry (Deng et al., 2007; Wu et al., 2015), except in NH1 which receives discharges from runoff. Nahoon Estuary is in East London, which is economically developed, densely populated, and characterized by its seaport. Consequently, Nahoon Eastuary could be receiving discharges from industrial waste which might have high PBDE concentration. Pollution of Nahoon Estuary with PBDE could also be attributed to improper plastic waste disposal from tourists, as plastics are major contributor of PBDE to the environment. No sediment sample was collected at NH5 in spring because of the lack of accessibility of the sampling point on the day of sampling. The point with the highest sediment concentration is NH3. This is where recreational activities and swimming take place. The high concentration of PBDEs could be attributed to anthropogenic pollution as this place is sometimes littered with wastes from leisure activities. There is possibility of NH3 receiving other forms of waste other than from recreational activities and runoff from the creek.
3.2 The contamination level of PBDEs in this current study compared with other countries
The concentration of PBDEs in the water and sediment samples is summarized in (Table S4, supporting information). The concentration ranges from BDL-247 ng/L in the spring season and BDL-70.2 ng/L in summer for water. PBDEs in sediment ranges from 0.16–3.42 ng/g dw in spring and 0.25–112 ng/g dw in summer. It is worthy of note that this high concentration which seems unusual for a River was observed at the point of discharge of runoff freshly discharged from a creek on sampling day. PBDES in the Estuary could probably come from flame retardants that contains plastic products and polyurethane foams (Oros et al., 2005). Comparing the concentration of water samples in this finding with previous studies in South Africa, the concentrations from this study were higher than reports from Jukskei River, Cape town (below detection limit) (Olukunle et al., 2012), Sundays River Estuary (2.5–39.1 ng/L) and Swartkops River (2.5–169 ng/L) in Port Elizabeth (Olisah et al., 2020a). The high concentration from Swartkops was not out of place as runoffs from Motherwell and Markman canal were noticeably discharging into Swartkops river Estuary (Olisah et al., 2020a). Higher concentrations from South Africa was also reported from Diep River (320–485 ng/L) in Cape town, which also received effluent discharges from wastewater treatment plant (Daso et al., 2013a). Although, BDE-209 was investigated in Diep River but were below detection limit in most cases (Daso et al., 2013a). Furthermore, the values from this study were higher than 18 ng/L (mean) in the Netherlands (De Boer et al., 2003), and 7.87 ng/L in South China (Yang et al., 2015). It was observed that the sediment concentrations in this study were lower than bdl-212 ng/g in the U.S.A, which possibly could be from leaching and emission from a nearby refuse dump (Oros et al., 2005), but higher than 0.5-3 ng/g in the U.S.A (Song et al., 2004). BDE-47 and 100 which are the most bioaccumulative congeners from the commercial pentaBDE mixture among others (Oros et al., 2005), were the dominant congeners in all the above mentioned sites. Compared to Federal Environmental Quality Guideline (FEQG), water and sediment values were below the standards except the pentaBDE which has higher values than the FEQG standards both in spring and summer seasons for water (4.25–178 and 7.36–11.5 ng/L) and sediment samples (0.21–0.41 and 0.26–25.7 ng/g dw) respectively.
Table 2
Mean concentrations of PBDEs in surface water and sediments of Nahoon River estuary in ng/L and ng/g dw, respectively
| Spring | | | | | Summer | | | |
Surface water | | | | | | | | | |
Congener | Mean (n = 5) | Max | Min | DF (100%) | | Mean (n = 5) | Max | Min | DF (100%) |
BDE 17 | 140 ± 91.2 | 247 | BDL | 80 | | 23.5 ± 31.5 | 70.2 | BDL | 40 |
BDE 47 | 68.9 ± 76.7 | 190 | 4.27 | 100 | | 7.92 ± 2.80 | 12.4 | 5.43 | 100 |
BDE 100 | 44.0 ± 64.4 | 178 | 4.25 | 100 | | 8.95 ± 2.96 | 11.5 | 7.36 | 100 |
BDE 153 | 5.88 ± 75.7 | 6.39 | 4.97 | 100 | | 6.59 ± 1.77 | 8.00 | 5.82 | 100 |
BDE 183 | 5.79 ± 0.98 | 5.56 | 5.41 | 100 | | 7.02 ± 1.01 | 8.80 | 5.13 | 100 |
ƩPBDE | 329 ± 48.3 | | | | | 62.1 ± 1.50 | | | |
Sediment | | | | | | | | | |
BDE 17 | 1.42 ± 1.14 | 2.77 | 0.44 | 100 | | 17.4 ± 12.2 | 32.0 | 0.14 | 100 |
BDE 47 | 0.27 ± 0.03 | 0.29 | 0.24 | 100 | | 3.14 ± 3.25 | 8.75 | 0.28 | 100 |
BDE 66 | 1.47 ± 1.36 | 3.42 | 0.27 | 100 | | 8.88 ± 17.8 | 31.4 | 0.29 | 100 |
BDE 100 | 0.20 ± 0.08 | 0.41 | 0.21 | 100 | | 7.25 ± 10.4 | 25.69 | 0.26 | 100 |
BDE 153 | 0.19 ± 0.08 | 0.27 | 0.08 | 100 | | 6.00 ± 10.7 | 25.1 | 0.63 | 100 |
BDE 183 | 0.56 ± 0.07 | 0.64 | 0.47 | 100 | | 22.7 ± 49.9 | 112 | 0.25 | 100 |
ƩPBDE | 4.19 ± 0.35 | | | | | 65.4 ± 15.9 | | | |
BDL: below detection limit; D- frequency of detection; N = number of samples |
3.3 Impact of physicochemical parameters on concentrations of PBDEs in Nahoon Estuary
The temperature range across the five sampling points in the spring and summer season was 20.7–21.3 oC and 24.5–26.6 oC, respectively. There was no significant difference for the physicochemical properties of samples collected (Table 3) from the different sampling points (p > 0.05). Higher concentrations were observed in water in the spring season than in summer. High temperatures and strong sunshine in summer help the transfer of PBDEs via wet/dry deposition, and consequently, promoting the degradation of higher brominated diphenyl ethers to lower brominated diphenyl ethers (Shao et al., 2018). Although, there is paucity of experimental data accessible on properties and temperature dependence of PBDEs. PBDEs are endothermal, so the solubility increased with increased temperature (Kuramochi et al., 2007). Although, sediment also recorded higher levels of pollutants in summer, this could be due to other factors like higher turbidity observed in summer season. The pH affects the chemical processes of the water body and can help measure the degree of the effluent trail in the water body (Chapman, 1996). However, PBDEs' chemical features are not affected by pH (Fontana et al., 2009). The pH range across the five sampling points in the spring and summer season was 8.27–8.65 and 8.3–8.94, respectively. The range of pH for both are same, implying that the influence pH on the concentrations of PBDE detected in this site is negligible. The salinity values were 28.8–34.4 PSU and 33.5–33.8 PSU for spring and summer seasons, respectively. Salinity showed no effect on the sorption of BDE-47 on plastics as reported (Xu et al., 2019), but can influence PBDEs' distribution (Anim et al., 2017). Increase in salinity decreases solubility of many chemicals, and causes adsorption of organic contaminant to the suspended particles and then deposited on to the sediment (Y. Wu et al., 2017). It was observed that increase in salinity decreased the concentration of PBDE in surface water of the study site and vice versa. Conductivity is the extent of water's capability to conduct an electric current. Rough estimate of conductivity specifies the water's mineral content and could be significantly higher in polluted water or any that receives a large quantity of urban runoff (Chapman, 1996). It is an indicator for salinity of water (Rusydi, 2018). The electrical conductivity was about 44.4–46.5 mS/cm and 51.0-55.5 mS/cm for both spring and summer. Higher conductivity brings about warmer water (Olisah et al., 2019), and consequently lower concentration due to degradation. From this study, the concentration of PBDEs in water was higher in spring than in summer because spring season had lower conductivity value than summer. The oxidation-reduction property (ORP) of water is a characteristic of state of natural water. Increase in DO increases ORP (Chapman, 1996). Value of ORP for this present study ranges from 23.3–70.8 MvORP and 22.7–55.1 MvORP in summer and spring correspondingly. Increase in temperature and salinity brings about decrease in DO (Chapman, 1996). The DO of this study ranges from 5-5.59 mg/L and 5.88–8.55 mg/L in summer and spring in that order. Areas of high concentration level causes decrease in dissolved DO (Liu et al., 2015). Higher concentration of PBDEs in water samples with lower DO and vice versa was observed for spring and summer seasons, respectively. Turbidity slows the degradation of PBDEs such as BDE-209 (Viganò et al., 2011). In this study, it ranged from 3.97-73 and 10.6–26.4 NTU in summer and spring, respectively. Higher molecular congeners of POPs are known to adsorb to particulate matters and subsequently settle down in the sediment (Moon et al., 2012; Wang et al., 2016; Zhou et al., 2019), and turbidity could have prevented debromination of PBDEs by obstructing the penetration of light (Rügner et al., 2013; Viganò et al., 2011) Moreover, natural organic matter is known to inhibit degradation of dibromophenyl ether (Zhu et al., 2018). Organic matter speeds up the gas/particle partitioning. The organic matter in this study ranged from 0.30–0.60% and 0.21–0.27% in summer and spring. This could also explain the reason for higher concentration in spring, as organic matter was lower. High concentration of suspended solids suggests potential elevation of hydrophobic endocrine disruptors concentration, which is as a result of compounds having high log Kow values linked with the non-settleable solids (Langford et al., 2007). However, lower concentration was observed in summer in this study, probably because of high temperature. The range of TSS was 4.0–15.0 mg/L. TSS is inversely related to particulate organic carbon content (Chapman, 1996). Resistivity assesses the lateral spread of salinity (Chapman, 1996), and was measured to be 21.0-22.7 and 19.0–20.0 ohm-cm for spring and summer seasons, respectively. The summary of the physicochemical properties of the water collected from the study area is presented in Table 3.
Table 3
Physicochemical properties of surface water and sediment samples
| Spring | | Summer | |
Parameters | Mean ± STD | Range | Mean ± STD | Range |
Temp.[°C] | 21.0 ± 0.28 | 20.7–21.3 | 25.9 ± 0.79 | 24.5–26.6 |
pH | 8.48 ± 0.17 | 8.27–8.66 | 8.65 ± 0.22 | 8.33–8.94 |
EC [mS/cm] | 45.7 ± 1.02 | 44.4–46.5 | 51.5 ± 61.0 | 51.0-51.5 |
TDS [g/L] | 22.9 ± 0.51 | 22.2–23.3 | 25.6 ± 80.1 | 25.5–25.7 |
Sal.[psu] | 29.7 ± 0.74 | 28.8–34.4 | 33.6 ± 0.12 | 33.5–33.8 |
Turb.FNU | 17.8 ± 5.97 | 10.6–26.4 | 31.4 ± 28.8 | 3.97-73.0 |
mVorp | 32.2 ± 13.1 | 22.7–55.1 | 55.4 ± 19.3 | 23.2–70.8 |
RES(Ohm-cm) | 21.9 ± 0.60 | 21.0-22.7 | 19.6 ± 0.43 | 19.0–20.0 |
DO (mg/L) | 6.84 ± 1.11 | 5.88–8.55 | 5.31 ± 0.26 | 5.00-5.59 |
TSS (mg/L) | 8.33 ± 3.25 | 4.00-12.7 | 9.13 ± 4.21 | 4.00–15.0 |
% MC | 63.3 ± 1.05 | 62.5–64.8 | 30.0 ±3.69 | 25.0–35.0 |
% OC | 0.25 ± 0.02 | 0.21–0.27 | 0.29 ± 0.07 | 0.17–0.35 |
%OM | 0.42 ± 0.04 | 0.37–0.47 | 0.50 ± 0.12 | 0.30–0.60 |
Temp- temperature; TDS- total dissolved solid; EC- electrical conductivity; Sal- salinity; mVorp- oxidation-reduction potential; Turb- turbidity; DO- dissolved oxygen; TSS, total suspended solid; MC- moisture content; OC- organic content; OM- organic matter |
3.4 Correlation of PBDEs in water and sediment with physicochemical properties
The Pearson correlation analysis between PBDEs concentration in water and sediment with the physicochemical parameters was performed (Tables S2 and S3). Correlation values for BDE-17 versus 47 (r = 0.91, p < 0.01), BDE- 100 (r = 0.79, p < 0.01), BDE- 183 (r = 0.78, p < 0.01), were observed in water samples. All the congeners correlated strongly among themselves except for BDE-153, which showed no correlation with BDE- 17, 47, and 183. The positive correlation effect suggested that the congeners all came from the same source, except BDE- 17. The temperature and pH did not show any correlation with the congeners. Correlation values for EC versus BDE-17 (r = -0.87, p < 0.01), BDE- 47 (-0.77, p < 0.01), BDE- 100 (-0.77, p < 0.01), and BDE-183 (-0.86, p < 0.01) were observed. This implies that the congeners decrease with an increase in EC. There was no correlation between EC, TSS, and DO with BDE- 153. The correlation of EC with all the physicochemical parameters was observed, only pH correlated with EC and resistivity. Negative correlation was observed between salinity and all congeners except BDE-153 with a very poor correlation (r = 0.128), suggesting “salting out” effect (Y. Wu et al., 2017). In sediment samples, BDE- 47, 100, 153, and 183 showed a very strong correlation with all except BDE- 17. There was no correlation between the congeners with the OM and OC, all the congeners and physicochemical parameters correlated with moisture content. The observed positive correlation may propose a potential impact of physicochemical parameters on the PBDEs concentrations.
3.5 Contamination pattern and source apportionment of pollution in Nahoon Estuary using a dendrogram
Dendrogram demonstrating the ranked cluster analysis (Hellar-Kihampa et al., 2013) of PBDEs of water and sediment samples from 5 sampling points at the Nahoon River Estuary is illustrated (Fig. 3). Locations in the same clusters show similar contamination. The study site of PBDEs concentrations was classified with hierarchical cluster analysis by employing the rescaled distance cluster combined with the average linkage method as reported elsewhere (Olisah et al., 2021). The mean water samples (NHW1, NHW2, NHW3, NHW4, NHW5) and sediment samples (NHS1, NHS2, NHS3, NHS4, NHS5) across the sites were represented. The cluster analysis showed that the area of study is clustered into four major groups based on their mean concentrations in both water and sediment. The first group is NHS3. This is the site with the highest concentration of PBDEs. BDE-183 has the highest concentration of all the congeners in this site. This is possibly an indication of the presence of commercial octa-BDE from local anthropogenic source (La Guardia et al., 2006). The second cluster comprises NHS5 with the second-highest concentration of PBDEs, having BDE-17 as the highest concentration from this point. The third cluster consists of NHS2, NHS1, and NHS4. These are the sites with the third-highest concentrations of PBDEs. The fourth cluster consists of NHW1, NHW4, NHW2, NHW5, and NHW3, which are class of cluster with low concentrations.
3.6 Compositional patterns of PBDEs in the surface water and sediments
The summary of the percentage distribution of the Ʃ6PBDE is given in Fig. 2. In water samples, the dominant congener is BDE- 17 (43%), which came majorly from NH1 > NH2 > NH3 > NH4, followed by BDE- 47 (27%), and BDE- 100 (26%) correspondingly, all suggesting that NH1 and NH2 are the most polluted points which are the closest point to the creek where the runoff from uknown source is being discharged to the Estuary. The dominant congener in the sediment is BDE- 183 (33%), majorly at point NH3, followed by BDE- 17 (27%), emanating from NH5 and NH3, BDE- 66 (15%), coming from NH3 and NH1, and BDE- 100 (11%), coming from NH3, NH5, NH1. All the congeners are detected at NH4 in low concentration. The highest concentrations of the congeners in sediments were from point NH3, with BDE-183 having the highest concentration (112 ng/g). BDE-183 is an indicator of octa-BDE; therefore, the relatively high concentration is an indication of possible extra contribution from octa-BDE products as similarly reported (Chen et al., 2009). Furthermore, lower brominated congeners could be because of debromination or higher congeners or extensive use of products of penta-BDE mixtures as stated earlier.
3.7 Ecotoxicological risk assessment
The result from the ecotoxicological risk is given (Table 4), which indicates that HQ for water samples shows no risk in the concentrations of PBDEs, while pentaBDE in sediment samples suggests possible low non- cancer risk (0.2) To further evaluate the probable eco-toxicological risk of PBDEs in water and sediment samples in Nahoon River Estuary, the Federal Environment Quality Guidelines (FEQG) standards for PBDEs of Canada (Environment Canada, 2013) was adopted as was also reported elsewhere (Ge et al., 2014). The mean concentrations from the two seasons each (Table 5) were compared with BDE-17, 66, and 183 were not included in the homologues in the evaluation of the ecotoxicological risk as they were not given in this guideline. It was observed that hexaBDEs and tetraBDE in both water and sediments pose no risk. However, pentaBDE in both water and sediment samples for the two seasons were above the standard values for FEQG. Although, the concentrations of pentaBDE from this study is higher than the standard values for FEQG; it does not pose threat to water, though low potential non-cancer risk for sediment is envisaged. Therefore, this calls for special concern so as to ensure safety of aquatic lives, tourists, and athletes
Table 4
Hazard quotient (HQ) for ecotoxicological risk
Water | | | |
Congener | Mean (ng/L) | EDI (ng/L) | HQ |
BDE 47 | 38.4 | 1.28 | 0.0 |
BDE 66 | 36.6 | 1.22 | 0.0 |
BDE 100 | 26.5 | 0.88 | 0.0 |
BDE 153 | 6.23 | 0.21 | 0.0 |
Sediment | | | |
Homologue | Mean(ng/g dw) | PNEC (ng/g)* | HQ |
PentaBDE | 5.48 | 31 | 0.2 |
OctaBDE | 14.7 | 9100 | 0.0 |
*PNEC values for water (ng/L) and sediment (ng/g) extracted from literature (Canada Environment Protection, 2006); EDI = Estimated daily intake; HQ = Hazard quotient |
Table 5
Comparison of the PBDEs concentration of the present study with FEQG for both water (ng/L) and sediment (ng/g dw)
| | | This study | |
Homologue | Congener | FEQG** | Spring | Summer |
Water | | | | |
TetraBDE | BDE-47 | 24 | 4.27–190 | 5.43–12.4 |
PentaBDE | BDE-100 | 0.2 | 4.25–178 | 7.36–11.5 |
HexaBDE | BDE-153 | 120 | 4.97–6.39 | 5.82-8.00 |
HeptaBDE | BDE-183 | 17 | 5.41–3.56 | 5.13–8.80 |
Sediment | | | | |
TetraBDE | BDE-47 | 39 | 0.24–0.29 | 0.28–8.75 |
PentaBDE | BDE-100 | 0.4 | 0.21–0.41 | 0.26–25.7 |
HexaBDE | BDE-153 | 440 | 0.08–0.27 | 0.63–25.1 |
**FEQG values extracted from the literature (Environment Canada, 2013) |