Abstract:The complexation of CH 3 Hg with major ions present in sea and estuary waters (Cl À , SO 4 2À and CO 3 2À ) was studied potentiometrically in an NaClO 4 medium in the ionic strength range 0.1± 3.0 mol dm À3 at 25°C. The potentiometric data, treated with non-linear least squares computer programs, led us to establish the formation of the species CH 3 HgCl in equilibrium with chloride, CH 3 Hg(SO 4 ) À species with sulfate and no complex with carbonate. The stoichiometric stability constants obtained at the diff… Show more
“…This indicates that spatial distribution of the MeHg K d cannot be explained by a passive diffusion model. Alternatively, the particle solubility of MeHg would be increased in response to increasing Cl concentrations, if MeHg speciation were dominated by Cl complexation [33,34]. Indeed, the modeling result presented in Figure 5 is consistent with this hypothesis, suggesting that most of the microseston is not composed of phytoplankton and bacteria.…”
To understand the bioconcentration of methylmercury (MeHg) at the base of the riverine food chain, we determined levels of dissolved organic carbon, microseston, Hg, and MeHg in surface water in relation to the microzooplankton MeHg from Yeongsan River. The spatial distribution of unfiltered Hg (0.29-3.1 ng/L) and dissolved Hg (0.15-0.74 ng/L) closely followed the microseston distribution. The spatial distribution of unfiltered MeHg (0.0078-0.077 ng/L) and dissolved MeHg (0.0069-0.018 ng/L) increased with increasing distance from the river mouth and appeared to arise from the shallow wetlands surrounding the upper riverbanks and then to be transported downstream. The logarithm of the MeHg bioconcentration factor for microzooplankton ranged from 5.3 to 6.0 (5.7 ± 0.18), and for microseston ranged from 4.0 to 5.4 (4.9 ± 0.35). Linear correlation statistics comparing microzooplankton MeHg and river water characteristics revealed that microzooplankton MeHg concentration was most significantly correlated with unfiltered MeHg (r = 0.83) and particulate MeHg (r = 0.80) levels. This result suggests that MeHg in unfiltered river water, which is relatively easy to determine, can be used as a surrogate for MeHg in microzooplankton that may influence MeHg levels in higher-trophic-level organisms.
“…This indicates that spatial distribution of the MeHg K d cannot be explained by a passive diffusion model. Alternatively, the particle solubility of MeHg would be increased in response to increasing Cl concentrations, if MeHg speciation were dominated by Cl complexation [33,34]. Indeed, the modeling result presented in Figure 5 is consistent with this hypothesis, suggesting that most of the microseston is not composed of phytoplankton and bacteria.…”
To understand the bioconcentration of methylmercury (MeHg) at the base of the riverine food chain, we determined levels of dissolved organic carbon, microseston, Hg, and MeHg in surface water in relation to the microzooplankton MeHg from Yeongsan River. The spatial distribution of unfiltered Hg (0.29-3.1 ng/L) and dissolved Hg (0.15-0.74 ng/L) closely followed the microseston distribution. The spatial distribution of unfiltered MeHg (0.0078-0.077 ng/L) and dissolved MeHg (0.0069-0.018 ng/L) increased with increasing distance from the river mouth and appeared to arise from the shallow wetlands surrounding the upper riverbanks and then to be transported downstream. The logarithm of the MeHg bioconcentration factor for microzooplankton ranged from 5.3 to 6.0 (5.7 ± 0.18), and for microseston ranged from 4.0 to 5.4 (4.9 ± 0.35). Linear correlation statistics comparing microzooplankton MeHg and river water characteristics revealed that microzooplankton MeHg concentration was most significantly correlated with unfiltered MeHg (r = 0.83) and particulate MeHg (r = 0.80) levels. This result suggests that MeHg in unfiltered river water, which is relatively easy to determine, can be used as a surrogate for MeHg in microzooplankton that may influence MeHg levels in higher-trophic-level organisms.
“…Table 2 lists the anionic initiators along their respective pK s and pK a values and the corresponding morphology of the polymer observed by SEM. The pK s and pK a values shown in Table 2 were obtained from reports published in the literature [20][21][22][23][24]. For certain anions whose pK s values were unavailable, estimations were made for their values.…”
“…High NaCl content provides (i) Na cations, which effectively compete with mercury species for the anionic binding sites of kaolin, and (ii) Cl À anions, which promote the formation of very stable and negatively charged chloro-complexes of mercury, especially HgCl 4 2À , 9 and MeHgCl. 26 Both facts facilitate desorption of mercury species from the suspended particles. In our experiments, increasing the concentration of NaCl leads to significantly lower removals in all the situations checked.…”
The main tendencies in the adsorption of dissolved inorganic mercury (Hg 2 ) and methylmercury (MeHg ) on suspended kaolin particles have been investigated in synthetic aqueous solutions. The influence of NaCl, fulvic acid (FA) and suspended particulate matter (SPM) in the system has been studied at a constant pH of 7.2. The experiments were arranged according to a full factorial design with three factors (NaCl, FA SPM) at low (À) and high () levels. A central point (
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