Ibukun
Ola
*a,
Carsten
Drebenstedt
a,
Robert M.
Burgess
b,
Lane
Tidwell
c,
Kim
Anderson
c,
Nils
Hoth
a and
Christoph
Külls
d
aInstitute of Mining and Special Civil Engineering, Technical University Mining Academy, Gustav-Zeuner Street 1A, Freiberg, 09599, Germany. E-mail: Ibukun.Ola@doktorand.tu-freiberg.de
bU.S. Environmental Protection Agency, Office of Research and Development, Center for Environmental Measurement and Modeling, Atlantic Coastal Environmental Sciences Division, 27 Tarzwell Drive, Narragansett, Rhode Island 02882, USA
cFood Safety & Environmental Stewardship Lab, Environmental & Molecular Toxicology, Oregon State University, USA
dLabor für Hydrologie und Internationale Wasserwirtschaft, Technische Hochschule Lübeck, Lübeck, 23562, Schleswig-Holstein, Germany
First published on 7th October 2024
In equilibrium-based passive sampling applications, the accuracy of estimating freely dissolved concentration (Cfree) of hydrophobic organic compounds (HOCs) relies on the passive sampler–water partition coefficient (KPS–W) values applied. The vast majority of KPS–W are generated under standard conditions: 20 °C in deionized or freshwater. Few empirically derived values are available for non-standard conditions. In this study, polyethylene (PE)–water partitioning coefficients (KPE–W) were experimentally determined for 15 polycyclic aromatic hydrocarbons (PAHs, comprising 9 parent and 6 alkylated compounds) under three different temperature (10, 20, 30 °C) and salinity (0, 18 and 36‰) regimes, the KPE–W values were found to correlate strongly with a variety of molecular parameters (e.g., octanol–water partition coefficients (KOW), molecular weight (MW) and molecular volume (MVOL)). The effects of temperature and salinity on the magnitude of KPE–W were found to be substantial. For temperature, the values range between −0.005 and −0.023 log units per °C; these values indicate that every 10 °C rise in temperature would potentially decrease the KPE–W by a factor of between 0.4 to 1.6. For salinity, the values range from 0.0028 to 0.0057 log units per unit ‰, indicating that an 18‰ increase in salinity would likely increase the KPE–W by a factor of between 0.28 and 0.82. Moreover, temperature and salinity were shown to be independent of each other and non-interacting. Temperature effects were chemical-specific and moderately dependent on hydrophobicity (expressed as the KOW), whereas salinity effects were independent of hydrophobicity. We also assessed the combined impact of temperature and salinity, which showed increasing effects with the hydrophobicity of the PAHs studied. Based on the results, KPE–W values adjusted for site-specific temperature and salinity can be calculated. The impact of applying such site-specific values was demonstrated using a PE-based field monitoring dataset for PAHs from coastal waters of Grand Isle (LA, USA) collected during the 2010 Deepwater Horizon oil spill. When KPE–W values were adjusted to 10 °C and 30 °C, the final freely dissolved concentrations (Cfree) decreased or increased depending on the adjustment. Use of the results of this investigation allow for adjusting existing PE-based datasets to site-specific conditions resulting in more accurate Cfree values for estimating exposure and adverse ecological effects.
Environmental significanceThis study examines how temperature and salinity affect the estimation of freely dissolved concentrations (Cfree) of hydrophobic organic compounds (HOCs) using polyethylene (PE)-based passive samplers. By determining partition coefficient (KPE–W) values for polycyclic aromatic hydrocarbons (PAHs) under varying temperature and salinity conditions, we report significant temperature effects on KPE–W, which are chemical-specific and moderately dependent on hydrophobicity. Salinity effects, on the other hand, are independent of hydrophobicity. These results highlight the need for site-specific adjustments to improve the accuracy of Cfree estimations, crucial for assessing HOC exposure and ecological impacts in aquatic environments. Applying these adjustments to field monitoring datasets from areas affected by the 2010 Deepwater Horizon oil spill demonstrates the practical implications of our findings, aiding informed decision-making in environmental management and remediation efforts. |
The ability of nonpolar passive sampling devices (PSDs) to effectively measure the Cfree of NOCs has been adequately demonstrated.4,5 Nonpolar PSDs mostly find use in measuring the Cfree of NOCs of environmental concern including PAHs, PCBs, hexachlorobenzene (HCB), and polybrominated diphenyl ethers (PBDEs)6–9 and other HOCs of emerging concern including triclosan,10,11 alkylphenols11 and organophosphate pesticides.12 Several types of nonpolar PSDs have been developed. The pioneer nonpolar PSD was biphasic (e.g., semipermeable membrane device (SPMD)) and filled with the synthetic lipid triolein. This type of sampler was used on a considerable scale in the early applications of passive sampling. Single phase polymeric materials (e.g., polyethylene (PE), polyoxymethylene (POM), polydimethylsiloxane (PDMS), silicon rubber (SR)) have been used more frequently recently. The initial group (i.e., the biphasic) are gradually being phased out by the latter (i.e., single phase polymers). This is in part, because, the single phase polymers allow simpler modelling of polymer–water kinetics and are less susceptible to damage in that they have no associated risk of lipid/triolein leakage during exposure and/or extraction.13,14
Single phase polymers when exposed to the aquatic environment act as a sorption phase by accumulating target compounds until system equilibrium is reached or polymer exposure terminated. The Cfree of the target compounds can be determined using the model (eqn (1)) from Huckins et al.1 and Smedes & Booij:15
(1) |
(2) |
As seen in eqn (1) and 2, knowledge of KPS–W is crucial to the precise estimation of Cfree. For this reason, many investigations have been carried out to determine compound-specific KPS–W for several polymers including PE,6,14,20–25 POM,6,25–28 SR,21,29,30 and PDMS.25,31–36 The vast majority of KPS–W for all the types of passive samplers were experimentally determined or modelled under standard conditions (20 °C, deionized water).
Based on thermodynamic theory it is recognised that the partitioning of NOCs in a two-phase environmental system such as water and a solid phase is influenced by environmental parameters including temperature and salinity. At low temperatures and high salinity, the aqueous solubility of non-polar compounds decreases thereby increasing their hydrophobicity and preferential sorption to the solid phase such as a passive sampling polymer. This means, the use of KPS–W derived under standard conditions to estimate Cfree of compounds from laboratory experiments or field-deployments carried-out under non-standard conditions would likely yield inaccurate results.
Numerous passive sampling based studies focused on assessing Cfree of NOCs have been performed in non-standard environments including deep ocean waters37,38 and cold waterbodies.20,28,39,40 In these studies, the effects of changes in temperature and salinity on KPS–W were mostly corrected using the Van' t Hoff equation and the Setschenow constant, respectively. This correction approach is valid and useful for adjusting the individual effect of temperature and salinity; however, the method may not be appropriate for correcting for combined effects or assessing possible interacting effects of both temperature and salinity on KPS–W. Lohmann41 provided a comprehensive review of these correction methods, which forms a valuable basis for understanding how temperature and salinity individually affect KPS–W.
Alternative means using different single phase polymeric materials have been presented through laboratory studies. This new method based on empirical studies, depending on the experimental design, allows for the quantification and correction for both individual and combined effects of temperature and salinity on KPS–W. Furthermore, it also allows for the investigation of possible interacting effects between both parameters.
Currently, there are two issues with this alternative empirical approach. First, the results reported from several laboratory studies (using different polymers) are inconsistent. For example,16,30,32,42 using polymers including SR, PE and PDMS found substantial temperature effects on KPS–W values for low molecular weight (LMW) PAHs and PCBs. Interestingly, against theoretical principles, enhanced partitioning with increasing temperature was observed for methyl-triclosan, n-nonylphenol and some high molecular weight (HMW) PAHs and PCBs for PE.11 Conversely, no substantial temperature effects were observed in the sorption of some PAHs to PDMS, POM28 and PE,20 and the partitioning of triclosan and selected n- and t-octylphenols to PE.11 Similarly, substantial salinity effects have been reported on the partitioning of PAHs and PCBs to SR30 and PAHs sorption to PDMS28 and PE16 have been reported. In contrast, minor salinity effects on the partitioning of LMW PAHs, and sorption of methyl-triclosan and n-nonylphenol to PE11,22 have been observed. Overall, the mixed results are surprising given the effects of changes in temperature and salinity on KPS–W are supposedly driven by a compound's aqueous solubility and not by the differences in polymer properties.30 Variations in experimental design such as temperature ranges, salinity levels, equilibration times, and the presence of organic matter can significantly impact partitioning outcomes. Small differences in these experimental variables across studies can contribute to the observed inconsistencies.
A second concern with many of these laboratory studies except that of Jonker et al.30 is that they have largely focused on quantifying the individual effects of temperature and salinity leaving out the assessment of combined and possible interacting effects. Results from Jonker et al. show the effects of temperature and salinity on SR–water partition coefficients (KSR–W) of PAHs and PCBs are independent and non-interacting but their combined effects increase with chemical hydrophobicity.
Considering the current non-consensus in the literature on temperature and salinity effects on KPS–W, further studies focused on the quantification of not only individual effects, but also combined and possible interacting effects are needed for more commonly used nonpolar passive sampling polymers. Also, as noted earlier, the vast majority of KPS–W were determined under standard conditions (i.e., 20 °C in freshwater or deionized water). Consequently, an area of passive sampling application that needs further research is expansion of the experimental and modelling efforts for deriving these partition coefficients at temperatures and salinities beyond these narrow conditions. Access to KPS–Ws at higher salinities along a wider range of temperatures would expand the usefulness of passive sampling (e.g., in polar and tropical locations). To this end, the following exercises were carried out in this study: (1) using PE as the passive sampling polymer, we experimentally determined the PE–water partitioning coefficient (KPE–W) for 15 PAHs (10 parent, 5 alkylated) under three different temperature (10, 20, 30 °C) and salinity (0, 18 and 36‰) regimes while varying experimental temperatures and salinities on KPE–W, (2) assessed the joint effects of temperature and salinity on KPE–W values on the target compounds, and (3) using the relationships derived between temperature and salinity and KPE–W a field PE dataset collected during an oil spill was adjusted for site-specific conditions. Results of this investigation should allow for more accurate determinations of Cfree for estimating exposure and adverse ecological effects for a range of temperature and salinity conditions.
Salts used in this study included sodium chloride (NaCl), sodium sulfate (Na2SO4), sodium tetraborate (Na2B4O7), calcium chloride (CaCl2·2H2O), strontium chloride (SrCl2·6H2O), sodium carbonate (NaHCO3), potassium chloride (KCl), potassium bromide (KBr), magnesium chloride (MgCl2·6H2O), and sodium azide (NaN3). All salts were of extra pure quality obtained from Merck KGaA (Darmstadt, Germany), Carl Roth Gmbh & Co. KG (Karlsruhe, Germany), and Sigma-Aldrich (Steinheim, Germany). Tables S1 and S2 in the ESI† contains additional information on the salt composition and the target compounds.
Polyethylene (PE) (70 μm thickness) was obtained from Brentwood Plastics (St. Louis, MO, USA) kindly supplied by K. Booij (PaSOC, The Netherlands). The PE was resized into several small square-shaped strips (0.05 g per strip) and the strips were cleaned by soaking twice in cyclohexane by shaking at 150 rpm. Each precleaning cycle lasted 24 hours.
The KPE–W experiment was carried out using the desorption approach. This approach involved a first step that loaded the precleaned PE strips with fixed amount of target compounds (Table S2†) prior to the PE–water equilibration step. The loading process was carried out following the procedures detailed in the study by Booij et al.17 Briefly, PE strips were incubated in a target compound-spiked methanol/water (80/20) (V/V) mixture, the water content was increased in 10% steps (over 13 days mixed at 150 rpm) until a 50/50 methanol/water content was reached. Clean laboratory tissue paper was used to remove traces of methanol from the PE strips. Along with the methanol swelling the polymer to enhance HOC partitioning, the increasing aqueous fraction encourages the HOCs into the polymer rather than staying in the methanol.
Amber bottles (250 mL) were prepared by dishwashing twice with solvent and distilled water and oven dried for a 6 h period. Thereafter, 220 mL of aqueous solution was poured into each bottle followed by the addition of a piece of the loaded PE strips. The aqueous solution consisted of 50 mg L−1 sodium azide (to inhibit microbial growth) and sufficient salt contents for the treatments of 18‰ and 36‰ salinity levels. The filled amber bottles were swiftly closed by glass stoppers and transferred to corresponding rotating orbital shakers placed in temperature-controlled rooms. In total, there were three shakers, one each for the three different temperature regimes. Each treatment (i.e., combination of temperature and salinity level) was replicated three times. The overall shaking period for the partitioning experiment lasted 11 week.
For the analysis in this study, only data from Grand Isle, Louisiana (LA) was investigated. For the specific data related to Grand Isle, Louisiana (LA), it should be noted that samplers were lost from Grand Isle in July 2010. The duration of sampling deployments at Grand Isle varied ranging from 3 to 41 days (Table S3†). The PAHs monitored at Grand Isle consisted mainly of 33 parent and alkylated PAHs (Table S4†). Throughout the sampling events at Grand Isle, the average temperature exhibited a range from 24.85 to 32.85 °C, with the salinity of the water consistently measured at 35 (‰). Detailed passive sampling conditioning, construction, cleanup, extraction and subsequent chemical analyses at Grand Isle are described in Tidwell et al.44 Briefly, approximately one meter long PSDs made from low-density PE (LDPE) tubing were fortified with deuterated PAHs (PRCs) for water sampling rate calculations. PRCs spanned a range similar to the target PAHs, with the most similar used for quantification. PSDs were transported in sealed polytetrafluoroethylene (PTFE) bags and stored at 4 °C until extraction within two weeks. All solvents were Optima grade or better, and standards had purities of ≥97%. PSDs were extracted as a composite sample for increased sensitivity, using n-hexane dialysis, and stored in amber glass vials at −20 °C until analysis.
logKPE–W = 0.0264 MW − 0.3705 (r2 = 0.96, n = 15) | (3) |
PAH | 10 °C | 20 °C | 30 °C | ||||||
---|---|---|---|---|---|---|---|---|---|
0‰ | 18‰ | 36‰ | 0‰ | 18‰ | 36‰ | 0‰ | 18‰ | 36‰ | |
2-Methyl naphthalene | 3.40 ± 0.02 | 3.49 ± 0.07 | 3.56 ± 0.04 | 3.39 ± 0.09 | 3.44 ± 0.01 | 3.46 ± 0.01 | 3.28 ± 0.02 | 3.36 ± 0.04 | 3.46 ± 0.02 |
Acenaphthene | 3.65 ± 0.01 | 3.75 ± 0.07 | 3.81 ± 0.02 | 3.63 ± 0.09 | 3.67 ± 0.02 | 3.69 ± 0.02 | 3.53 ± 0.05 | 3.59 ± 0.01 | 3.68 ± 0.00 |
2,6-Dimethyl naphthalene | 4.00 ± 0.01 | 4.12 ± 0.07 | 4.19 ± 0.04 | 3.99 ± 0.09 | 4.05 ± 0.01 | 4.08 ± 0.02 | 3.89 ± 0.05 | 3.96 ± 0.03 | 4.05 ± 0.02 |
Fluorene | 3.81 ± 0.00 | 3.89 ± 0.07 | 3.95 ± 0.02 | 3.76 ± 0.09 | 3.8 ± 0.03 | 3.83 ± 0.03 | 3.65 ± 0.04 | 3.71 ± 0.03 | 3.8 ± 0.00 |
Phenanthrene | 4.26 ± 0.02 | 4.36 ± 0.08 | 4.42 ± 0.02 | 4.21 ± 0.09 | 4.24 ± 0.01 | 4.28 ± 0.03 | 4.07 ± 0.05 | 4.12 ± 0.02 | 4.22 ± 0.03 |
1-Methylfluorene | 4.4 ± 0.00 | 4.49 ± 0.07 | 4.55 ± 0.01 | 4.34 ± 0.09 | 4.38 ± 0.01 | 4.43 ± 0.03 | 4.22 ± 0.04 | 4.27 ± 0.02 | 4.36 ± 0.00 |
Fluoranthene | 4.95 ± 0.01 | 5.03 ± 0.09 | 5.08 ± 0.02 | 4.84 ± 0.08 | 4.86 ± 0.00 | 4.92 ± 0.05 | 4.7 ± 0.03 | 4.74 ± 0.04 | 4.81 ± 0.01 |
Pyrene | 5.09 ± 0.01 | 5.16 ± 0.08 | 5.21 ± 0.02 | 4.97 ± 0.08 | 5.00 ± 0.00 | 5.05 ± 0.05 | 4.84 ± 0.03 | 4.86 ± 0.05 | 4.93 ± 0.01 |
2-Ethylanthracene | 5.52 ± 0.04 | 5.6 ± 0.07 | 5.65 ± 0.02 | 5.41 ± 0.09 | 5.42 ± 0.01 | 5.51 ± 0.04 | 5.32 ± 0.06 | 5.33 ± 0.04 | 5.46 ± 0.08 |
1-Methylpyrene | 5.6 ± 0.02 | 5.75 ± 0.07 | 5.8 ± 0.02 | 5.51 ± 0.12 | 5.52 ± 0.01 | 5.58 ± 0.03 | 5.32 ± 0.07 | 5.36 ± 0.01 | 5.48 ± 0.02 |
Benzo(a)anthracene | 5.77 ± 0.01 | 5.85 ± 0.06 | 5.9 ± 0.03 | 5.64 ± 0.09 | 5.66 ± 0.00 | 5.71 ± 0.03 | 5.46 ± 0.07 | 5.5 ± 0.01 | 5.6 ± 0.02 |
Benzo[e]pyrene | 6.31 ± 0.02 | 6.49 ± 0.12 | 6.52 ± 0.04 | 6.29 ± 0.06 | 6.36 ± 0.04 | 6.15 ± 0.09 | 6.1 ± 0.10 | 6.12 ± 0.01 | 6.22 ± 0.02 |
Benzo(a)pyrene | 6.78 ± 0.16 | 6.80 ± 0.15 | 6.83 ± 0.08 | 6.52 ± 0.06 | 6.56 ± 0.09 | 6.61 ± 0.07 | 6.34 ± 0.11 | 6.38 ± 0.05 | 6.46 ± 0.03 |
7,12-Dimethylbenz[a]anthracene | 6.19 ± 0.09 | 6.31 ± 0.15 | 6.46 ± 0.03 | 5.69 ± 0.27 | 5.68 ± 0.11 | 5.76 ± 0.03 | 5.43 ± 0.05 | 5.29 ± 0.13 | 5.42 ± 0.24 |
Benzo[ghi]perylene | 6.15 ± 0.22 | 7.17 ± 0.27 | 7.21 ± 0.13 | 7.05 ± 0.07 | 7.05 ± 0.03 | 6.28 ± 0.36 | 6.83 ± 0.12 | 6.9 ± 0.07 | 6.93 ± 0.13 |
As seen in Fig. 1, logKPE–W values increase with increasing values of the individual molecular parameters, except for 7,12-dimethylbenz[a]anthracene which showed an unusual interaction with the test polymer. Causes of the anomalous behaviour of this chemical are unclear but was noticed in all experimental treatments (Fig. S1†) and in the additional systems set-up for confirming partitioning equilibrium. The unusual behavior of 7,12-dimethylbenz[a]anthracene with the test polymer may be due to unique steric hindrance created by the methyl groups at the 7 and 12 positions, altering its conformation and interaction with the polymer in ways not seen with other methylated PAHs. Additionally, these specific positions uniquely alter the electron density, affecting interaction with the polymer differently. Unique non-covalent interactions, such as van der Waals forces or π–π stacking, may also occur between the polymer and the 7,12-dimethyl substituents, which are absent in other methylated PAHs.
For the PAHs in this study, addition of a methyl group to the ring structure consistently adds 0.4–0.5 log unit to the KPE–W values (Fig. S2†) but the expected ∼1.2 log unit increase for 7,12-dimethyl-benz(a)anthracene versus benz(a)anthracene is not observed, and, actually, becomes negative at higher temperatures (i.e., KPE–W values for 7,12- dimethyl-benz(a)anthracene are lower than those of benz(a)anthracene). This behaviour is inconsistent with theory, and it is also not supported by any of the other measurements (e.g., 2-ethylanthracene which is 1.2 log unit higher than phenanthrene has a similar KPE–W as anthracene (Figure S2†)). This observed inconsistency in the 7,12-dimethyl-benz(a)anthracene KPE–W values further supports the earlier mentioned unexpected behaviour of the compound with the test polymer.
Linear correlations between logKPE–W values and the molecular parameters (Fig. 1) indicates the reliability of the PAH KPE–W values determined in this investigation. To further validate the reliability of the results determined under standard conditions, the KPE–W values from this study and those reported in previous studies are listed in Table 1 for comparison. It is important to mention, for a fair comparison, only KPE–W values determined at standard conditions were considered. This means KPE–W values for PAHs determined from saline water exposure20,39,47 or laboratory experiments carried out at lower20,42 or higher temperatures16,42,48 were excluded. Also, the suggested best-fit KPE–W values for PAHs from the extensive literature review by Lohmann41 were excluded because the values were largely derived from pooled KPE–W data that included experimental conditions that were not standard.
As seen in Table 1, the logKPE–W values determined here are within the range of those reported in the literature. The logKPE–W values compare best with results from Jonker25 and Hale et al.49 varying by only ± 0.01 to ± 0.04 log units. Similar minor differences are observed when comparing with data from Smedes et al.21 (±0.01 to ± 0.47 log units), Fernandez et al.50 (±0.14 to ± 0.27 log units), Bao et al.24 (±0.09 to ± 0.62 log units), Reitsma et al.20 (±0.11 to ± 0.68 log units), and Belles et al.14 (±0.03 to ± 0.72 log units). Whereas the majority of our logKPE–W values (particularly the more hydrophobic PAHs) are higher than those from Perron et al.6 (0.03–1.24 log units) and Choi et al.22 (0.08–0.82 log units). In summary, it is evident the logKPE–W values determined under standard conditions in this study compare very well with those reported in the literature.
As expected, the logKPE–W values decrease with increasing temperature, this is consistent with theoretical principles and corroborates with observations from previous studies. As earlier discussed in the Introduction, Adams et al. and Booij et al. observed similar effects on the partitioning of low molecular weight (LMW) PAHs to PE polymer.16,42 Also, Jonker et al. reported comparable effects on the sorption of several LMW PAHs and PCBs to silicone rubber.30 The slopes of the plots (Fig. 2) differ an indication that temperature effects are chemical dependent.
Using the slope of the logKPE–W – temperature correlation plots, a numerical quantification of the change in logKPE–W per °C for each individual chemical was determined and is presented in Table S6.† The values range between −0.005 and −0.023 log units per °C (across the three salinities); these values indicate that every 10 °C rise in temperature would potentially decrease the KPE–Ws by a factor of between 0.4 to 1.6. The temperature effects (as quantified by the logKPE–W – temperature correlation plots) do not vary substantially across the different salinities (Table S6†), suggesting temperature influences on KPE–W are independent of the salinity of the experimental systems. Plotting each PAH's temperature effects (i.e., change in logKPE–W per °C derived at different salinities for each individual chemical (Table S6†)) against its respective logKOW, a moderately linear correlation with an r2 ranging from 0.54 to 0.69 is observed. The changes in logKPE–W per °C values becomes more negative with increasing PAH hydrophobicity (Fig. 3a).
To further understand the effect of temperature on KPE–W of the PAHs, we considered relationships with temperature expressed in van't Hoff form:
(4) |
For selected PAHs, the InKPE–W – temperature relationship demonstrated a linear correlation (Fig. 4). The positive slope of the individual chemicals and the negative ΔG values (i.e., ranging from −18.82 to −39.46, (Table S6†)) indicate an exothermic sorption process.51 Values for ΔHPE–W ranged from −9.5 to 34.7 kJ mol−1 (Table S6†) and showed a consistent trend with comparable values for PAHs with the same number of aromatic rings. The entropy term is typically greater than zero (Table S6†) for the individual chemicals. The ΔHPE–W values derived here are similar to those reported by Adams et al. (−20 to −30 kJ mol−1) and Booij et al. (−20 to −50 kJ mol−1) for PE.16,42 Muijs & Jonker reported PDMS–water partitioning enthalpy values between −15.7 and −34.7 kJ mol−1 for PAHs.32 Similarly Jonker et al. using silicone rubber (SR) observed SR–water partitioning enthalpy values of between −16.9 and −58.0 kJ mol−1 for PAHs.30 Polymers used in the latter two studies (i.e., PDMS and SR) though different from PE yielded comparable results, this suggests the sorption behaviour of PAHs to these polymers (i.e., PE, PDMS and SR) is likely similar thermodynamically.
The changes in logKPE–W per unit salinity (‰) was quantified using the slope of plots in Fig. 5 and the results are presented in Table S8.† The values range from 0.002 to 0.0057 log units indicating that an 18‰ increase in salinity would likely increase KPE–W by a factor of between 0.28 and 0.82. Additionally, the data in Table S7† show salinity effects are similar across the three temperatures (observable but small), suggesting salinity effects on KPE–W is independent of temperature of the aqueous systems. A plot of the salinity effect as measured by the change in logKPE–W per unit salinity (‰) for individual PAHs determined at different temperature against their respective logKOW show appreciable scatter with no clear relationship between the two variables (Fig. 3b).
logKPE–W(T,S) = logKPE–W(20,0) + β × (T − 20) + α × (S) | (5) |
Results presented in Table S9† show the overall effect of temperature and salinity increasing with hydrophobicity and are largest for the more hydrophobic chemicals. For example, at freezing temperatures (i.e., 0 °C) and 36‰, a corrected logKPE–W value for benzo(a)pyrene would exceed its corresponding values determined at standard conditions by 0.63 log units (a factor of 5.4) while for a less hydrophobic chemical, like fluorene, the difference is smaller at 0.2 log units (a factor of 1.7). A visual representation of the combined effect of temperature and salinity on the logKPE–W of benzo(a)pyrene is presented in Fig. S3.† The plot shows that relative to logKPE–W values determined under standard conditions (benzo(a)pyrene: 6.52 ± 0.06), low temperatures combined with high salinities result in increased logKPE–W values ranging between 0.4 to 0.76 log units. However, high temperatures combined with the low salinities also reduces the logKPE–W by about 0.12 to 0.22 log units.
For one sampling event (April 2011) at the Grand Isle station, Fig. 6 evaluates the influence of adjustments in KPE–W due to variations in temperature (10 °C, 24.85 °C (actual field temperature), and 30 °C) and salinity (a constant salinity of 35 ppt is maintained to align with field conditions reported by Tidwell et al.44) on the estimated sum PAH of Cfree. As temperature increases from actual conditions to a hypothetical 30 °C, there is a consistent rise in sum PAH of Cfree. This indicates that the adjustments to KPE–W for higher temperatures lead to higher estimated PAH concentrations, highlighting the temperature–concentration relationship inherent in the adjusted partitioning behavior. Conversely, sum PAH of Cfree decreases relative to the actual conditions when adjusted for 10 °C (Fig. 6). PAHs with higher logKow values (>5.5) tend to exhibit a reduced sensitivity to the adjustments. Fig. 7 presents the sum PAH of Cfree for each of the eight sampling events applying the adjusted KPE–W values. Fig. 7b, indicates the relative change in sum PAH of Cfree compared to the actual field conditions. Overall, increasing the temperature to 30 °C resulted in an average 5.73 ± 2.52% increase in the Cfree while reducing the temperature to 10 °C affected a mean 29.9 ± 5.90% decrease in sum PAH of Cfree. It is important to note that the temperature correction does not directly affect the actual Cfree values but does influence the deviation in estimating Cfree. The direct inference from Fig. 7 is that the utilization of adjusted KPE–W values correlates with substantial increases or decreases in sum PAH of Cfree as temperatures adjusted up or down relative to actual conditions. This trend is consistently observed across the eight distinct sampling events. Even in cases such as June-1 and September sampling events, where field temperatures exceeded 30 °C, the use of adjusted KPE–W values led to an increase in Cfree.
To assess the impact of KPE–W adjustments on estimates of toxicity to aquatic life, an analysis was conducted across the eight distinct sampling events. Specifically, the sum PAH toxic units (TU) were estimated for each event (Fig. 8). The TU for an individual PAH is calculated by dividing its Cfree value (μg L−1) by the corresponding narcosis secondary chronic value (SCV) based on Di Toro et al.3 and Burgess et al.52 To obtain the sum PAH TU for a given event, the individual PAH TU values were summed. The estimated TU values for these events ranged from 0.001 to 0.045. A sum PAH TU exceeding 1 is typically indicative of potential sublethal toxicity to aquatic life.52 However, these findings indicate the TU values remain well below this threshold, implying a very low likelihood of toxicity resulting from the presence of PAHs from the Deepwater Horizon spill at these stations at the time of the passive sampler deployments.
Fig. 8 Estimated toxic units for total PAHs under various sampling events with different treatment conditions. |
Adjustments to the KPE–W values were found to have a minimal impact on the TU calculations. A comparison of TU values before and after the adjustments showed changes within a small range (0.001 to 0.003 units), indicating that while the adjustments refine the accuracy of the partitioning coefficients, they do not significantly alter the overall toxicity estimates. The TU calculations included 31 PAH compounds (Table S4†), selected for their prevalence and toxicological relevance in the context of the Deepwater Horizon spill. While it is acknowledged that petroleum spills contain thousands of compounds contributing to narcotic toxicity through additive effects, the selected PAHs serve as representative indicators. Therefore, despite the potential presence of additional unmeasured compounds, the low TU values observed for the analyzed PAHs indicate a relatively low risk of sublethal toxicity under the conditions and timeframe of this study.
This exercise demonstrates the power of having KPE–Ws that allow these temperature adjustments to be accurately performed. The continuing effects of climate change increasing oceanic water temperatures along with our on-going reliance on fossil fuels, and consequently, the occasional petroleum spill, provide a ‘real world’ application for this type of exercise. For example, modelling projected effects onsum PAH of Cfree under different future seawater temperatures and various spill volume magnitudes would be very useful for assessing petroleum exploration, transport and usage risks especially in sensitive habitats.
Partition coefficients for PAHs were reliably determined at varying temperatures and salinities, the resulting data allowed for the direct quantification of individual and combined effects of both parameters on KPE–W values. Individual influences of both parameters on PAH KPE–W values were substantial: a factor of 0.4 to 1.6 decrease for a 10 °C increase in temperature and a factor between 0.28 to 0.82 increase per every 18‰. Observed temperature effects were chemical-specific, moderately dependent on hydrophobicity and independent of salinity, whereas salinity effects were independent of temperature and hydrophobicity. Furthermore, when combining both temperature and salinity effects, an increasing trend with respect to chemical hydrophobicity for KPE–W was observed. As shown in the current study, correcting PE-based monitoring data for site-specific environmental conditions (temperature and salinity) using the Deepwater Horizon oil spill dataset substantially influenced the final Cfrees. Notably, this correction led to a decrease in sum PAH of Cfree of about 30% when adjusted to 10 °C and an increase in Cfree of about 6% when adjusted to 30 °C.
This study benefits the application of passive sampling technology in a number of ways including: (1) a new set of reliable experimentally determined KPE–W for PAHs and (2) data on the direct quantification of temperature and salinity effects on PAH partitioning to PE demonstrates the greatest impacts particularly at low temperature and elevated salinities (i.e., 10 °C, 18‰ and 36‰). Normally, these trends and behavior are difficult to tease out due to non-equilibration issues with experimental systems. Finally, tools for determining the effects of temperature and salinity on PAH partitioning into PE are available herein and shown in Tables S5 and S7† while combined effects may be corrected for using the chemical specific equations given in Table S8.† Use of these chemical specific correction equations maybe extended to PAHs not specifically covered in this study if they are within the logKOW range used here (i.e., 3.88 to 7.24).
Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4em00133h |
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