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Influence of sulfide, chloride and dissolved organic matter on mercury adsorption by activated carbon in aqueous system
Sustainable Environment Research volume 30, Article number: 22 (2020)
Using activated carbon (AC) as thin layer capping to reduce mercury (Hg) released from contaminated sediment is a feasible and durable remediation approach. However, several aqueous factors could greatly affect the Hg fate in the aquatic system. This study thus intends to clarify the influences on Hg adsorption by AC with the presence of sulfide, dissolved organic matter (DOM), and chloride. The lab-scale batch experiments were divided into two parts, including understanding (1) AC adsorption performance and (2) Hg distribution in different phases by operational definition method. Results showed that the Hg adsorption rate by AC was various with the presence of sulfide, chloride, and DOM (from fast to slow). Hg adsorption might be directly bonded to AC with Hg-Cl and Hg-DOM complexes and the rate was mainly controlled by intraparticle diffusion. In contrast, “Hg + sulfide” result was better described by pseudo-second order kinetics. The Hg removal efficiency was 92–95% with the presence of 0–400 mM chloride and approximately 65–75% in the “Hg + sulfide” condition. Among the removed Hg, 24–29% was formed into aqueous-phase particles and about 30% Hg was adsorbed on AC with 2–20 μM sulfide. Increasing DOM concentration resulted in more dissolved Hg. The proportion of dissolved Hg increased 31% by increasing DOM concentration from 0.25 to 20 mg C L− 1. Simultaneously, the proportion of adsorbed Hg by AC decreased by 47%. Overall, the presence of chloride increases the Hg adsorption by AC. In contrast, the presence of sulfide and DOM causes a negative effect on AC adsorption.
Mercury (Hg) has been known as one of the most toxic heavy metals to human beings and living organisms [1,2,3]. Despite the decreasing industrial use of Hg in the past recent years, human activities including fossil fuel combustions, gold-mining, and manufacturing industries have contributed to the increased Hg levels in the atmosphere and aquatic environments . The released Hg could ultimately transport to aquatic system and accumulate in sediment through wet or dry deposition. Thus, the formation and bioaccumulation of methylmercury (MeHg) formed from inorganic Hg under reducing conditions in sediment could put a serious threat to aquatic ecosystems [5, 6].
Several technical challenges still remain to remediate contaminated sediment, as the traditional approaches could not achieve risk reduction goals for human health and ecosystem protection and may even cause secondary pollution [7,8,9]. For example, dredging followed by ex-situ approaches has been typically used because of its long-term effectiveness and relatively short remediation time . Nevertheless, dredging could be very costly and results into remobilization of contaminants . In-situ thin-layer capping, which involves the use of chemically reactive materials that reduce the mobility, toxicity, and bioavailability of the contaminant, subsequently reducing ecological and human health risk, has been developed as a novel remediation of contaminated sediment [7, 12]. The use of activated adsorbents as capping materials has turned out to be a less expensive and high potential approach due to the ability to adsorb newly deposited contaminants. In previous studies of our research group, activated carbon (AC) was reported to successfully inhibit inorganic Hg and MeHg release into the overlying water in a lab-scale microcosm experiment [13, 14]. AC has been widely known as an effective adsorbent to remove Hg in recent years [15,16,17,18,19].
Several environmental factors, namely sulfide, chloride, and dissolved organic matter (DOM) could significantly affect the Hg fate in aquatic systems. The sulfide minerals in sediment are mainly the products of oxidizing organic matters by sulfate-reducing bacteria . Sulfide has high affinity for Hg and can form HgS particles; the forming of HgS(s) structure may inhibit Hg from being methylated and being transported [21,22,23]. Hg2+ concentrations are quite low as compared to sulfide concentration in aquatic ecosystems. Therefore, sulfides could control Hg speciation significantly and play an important role for stabilizing Hg in sediment .
Natural DOM in the stream water is typically at the range of 1 to 5 mg C L− 1, while in some high-organic soils or vegetated environments, DOM may have concentrations up to 20 or 50 mg C L− 1 . DOM is shown to hinder the aggregation of HgS particles by forming coordinate covalent bonds between functional groups on the organic molecules and atoms on the surface of the particles . Importantly, Hg interacted with DOM increased the methylating rate in comparison to Hg2+; moreover, the β-HgS nanoparticles formed by Hg mixed with sulfide and DOM have a higher availability than β-HgS microparticles for bacterial methylation . Recent studies have also shown that thiol functional groups are the major binding sites which mainly increases solubility, mobility and toxicity of Hg [27, 28].
The oxidation and reduction of Hg in the presence of chloride ion (Cl−) have also been studied mainly in oxic environments. The Hg-Cl complexes were regarded as non-adsorption Hg speciation in previous studies. Hg-Cl complexes were also reported to inhibit Hg reduction to gaseous Hg . Lee et al.  also reported that the increase of Cl− concentration inhibited Hg2+ reduction rate as the rate constant ranged from 0.14 to 1.7 h− 1 in the presence of Cl− as compared to 2.4 h− 1 in the absence of Cl−. Consequently, the health risk of organisms in the aquatic ecosystem is dependent on Hg chemical speciation and the phase of Hg rather than total Hg concentrations in the sediments.
Past studies showed that sulfide, DOM, and chloride ions could stabilize Hg in aquatic system. To further inference, sulfide, DOM, and chloride might inhibit Hg adsorption by AC and influence the Hg partitioning within various phases (i.e., aqueous, AC, and precipitation phases) that are still needed to be better comprehended. Therefore, in this study, batch experiments were conducted to gain further knowledge on the behavior of Hg adsorption by AC affected by sulfide, DOM, and chloride at various concentrations. The results obtained from this work could help clarifying the Hg adsorption mechanism by AC under the presence of essential elements in natural habitat, especially focusing on the impacts of sulfide, DOM, and chloride, and further help justifying whether thin layer capping can be applied to the aquatic system with the presence of these compounds at various concentrations.
Materials and methods
Lab-scale batch experiments were conducted to better understand the influences of sulfide, chloride, and DOM concentrations on Hg adsorption equilibrium and kinetics of AC in an aqueous system. The characterization of AC was also conducted to comprehend the effects of physicochemical properties of AC on Hg adsorption.
Physicochemical properties of AC
Commercial granular activated carbon (Wel Han Environmental Industrial Co., Taiwan) prepared from high-quality coconut shell was used. The AC was first washed with deionized water to remove fine particle and impurity, then dried at 60 °C in a drying oven for 24 h. After cooling in the drying oven, the AC was sieved by 10–18 mesh (1–2 mm) standard screens and stored for subsequent tests.
The specific surface area (SBET), total pore volume (Vtotal), and micropore surface area (Smicro) and micropore surface are (Vmicro) of AC were determined by N2 adsorption isotherm at 77 K (Micromeritics ASAP 2020). Brunauer–Emmett–Teller (BET) method was applied to evaluate SBET, Vtotal was calculated by total N2 volume adsorbed by AC at the relative pressure near one. The t-plot method was applied to evaluate the micropore volume and micropore surface area. Non-local density functional theory (NLDFT) model was applied to evaluate the pore size distribution of micropore. Barrett-Joyner-Halenda method was used to evaluate the pore size distribution of mesopore and macropore.
The morphology of AC samples was studied by scanning electron microscopy (SEM: JOEL JSM-7500F) with an accelerating voltage of 15 kV. AC was coated with a thin layer of gold to increase their electrical conductivity and stability, so that they can withstand the high vacuum conditions during analysis.
The elemental analyses were conducted to measure the contents of elements including nitrogen, carbon, hydrogen, sulfur (Vario EL cube, Elementar), and oxygen (Flash 2000, Thermo Fisher).
The zeta potential of AC under different pHs (1–9) was determined (Malvern Zetasizer Nano Z analyzer). AC was grounded into small powder for suspension in solution. Samples were prepared by adding 5 mg of AC in 9 mL Milli-Q water and adjusted to a given pH with NaOH and HNO3. The total solution volume was around 10 mL for analysis.
X-ray photoelectron spectroscopy (XPS; ULVAC PHI-5000) was conducted with Al Kα radiation of 15 kV to comprehend the functional groups on the surface of AC. The binding energies of peaks were referenced to C1s peak at 285 eV.
Batch experiments of Hg adsorption
The batch experiments include two parts: AC adsorption performance tests and Hg distribution tests. The AC adsorption performance experiments include AC dosage test and adsorption kinetic test. The AC dosage test was carried out by adding given amounts of AC into the spiked Hg solution in the absence of chloride, sulfide, and DOM. The adsorption kinetic test and Hg distribution test were carried out by using spiked Hg solution containing various concentrations of chloride, sulfide, and DOM individually under a fixed dosage of AC. The AC adsorption experiments in Hg-spiked solution mixed with chloride, sulfide, and DOM were designated as “Hg + Cl”, “Hg + sulfide”, and “Hg + DOM” respectively in this study. Each experiment was performed in triplicate. The main parameters are listed in Table S1 of Supplemental Materials.
Preliminary work of solution preparation
All solutions and reagents were prepared in degassed Milli-Q water, which was deoxygenated by purging with high-purity N2 at least 40 min (oxygen concentration < 2 mg L− 1). The Hg2+ solutions were prepared by diluting Hg (NO3)2 standard solution to 20–40 μg L− 1 then adding 5 mM sodium nitrate to maintain the ionic strength. Chloride stock solutions were prepared by dissolving sodium chloride in Milli-Q water. Sulfide stock solutions (pH = 11.5 ± 0.5) were prepared by dissolving crystals of Na2S·9H2O in Milli-Q water containing 10 mM H3BO3 then used immediately. The concentrations of chloride stock and sulfide stock were determined by UV-Vis spectrophotometer (Merck Spectroquant® Prove 300). DOM stock solutions were prepared by dissolving Suwanee River Humic Acid (SRHA) powder in Milli-Q water. The pH of the DOM stock was adjusted with 0.01 M NaOH to pH 6 then filtered through a 0.2 μm filter and stored in a refrigerator at 4 °C until measuring the total dissolved organic carbon (DOC) with a total organic carbon (TOC) analyzer.
AC adsorption performance
The experimental process followed the steps below:
Preparation of Hg solution
The Hg stock was diluted to 20 μg L-1 for AC dosage test. The “Hg + Cl” test was carried out by diluting Hg and chloride stock solution to 20 μg L-1 and 200 mM respectively in a 1 L beaker. The “Hg + DOM” test was carried out by diluting Hg and DOM stock solution to 20 μg L-1 and 2 mg C L-1 in a 1 L beaker, respectively. The “Hg + sulfide” test was carried out by diluting Hg and sulfide stock solution to 40 μg L-1 and 20 μM in each 500 mL beaker, respectively. Then, the sample solution was prepared by mixing equal volume of Hg and sulfide solution. Each Hg sample solution was adjusted to pH 7 ± 0.5 by using 0.01 M NaOH and 0.01 M HNO3 before adding AC.
The Hg sample solution was separated in a 50 mL volumetric flask and injected into a 50 mL glass vessel. The intended dosage of AC was added into glass vessels, which were then covered with a rubber stopper and aluminum cap. All of the glass vessels were then coated with aluminum foil to avoid light effect.
The samples were put into a water-bath incubating shaker and shaken at 125 rpm for 30–2880 min at 30 °C.
For the AC dosage and “Hg + Cl” test, 20 mL of the unfiltered initial Hg sample solution and 5 mL of the solution which was filtered with 0.2 μm filter after AC adsorption were preserved and digestion with 0.5% BrCl at least 1 day before the total Hg concentration (THg) analysis. For “Hg + sulfide” and “Hg + DOM” tests, 20 mL of the initial Hg sample solution and 5 mL of the solution which was filtered with 0.2 μm filter after AC adsorption were preserved with 0.5% BrCl and stored in a refrigerator at 4 °C until microwave digestion by HCl mixed with HNO3 (3:1 v/v). All the water samples were analyzed for the THg by the cold vapor atomic fluorescence spectrophotometer (CVAFS: Brooks Rand Model 3). The aqueous Hg removal efficiency by AC was calculated by Eq. (1) and the adsorption capacity of AC was calculated by Eq. (2).
where R (%) is the Hg removal efficiency, qe (μg g−1) is the adsorption capacity of AC, C0 (μg L−1) is the initial Hg concentration, Ct (μg L−1) is the residual Hg concentration at given time, V (L) is the volume of Hg sample solution, and WAC (mg) is the dosage of AC.
To determine the optimum AC dosage for the batch experiments, AC dosage tests were carried out by adding 20, 50, and 80 mg AC in 50 mL Hg solution (20 μg L− 1). The contact time of AC in “Hg + sulfide” test was controlled at 30, 60, 300, 600, and 1200 min. The contact time of AC in “Hg + Cl” and “Hg + DOM” tests were controlled at 30, 60, 300, 960, 1440, and 2880 min. The test parameters are listed in Table S2.
Hg distribution test
The purpose of this part of experiment is to realize the Hg distribution, including Hg in dissolved and solid phases under different concentration levels of sulfide/chloride/DOM. The test sample was divided into three parts by operational-defined method included “dissolved Hg”, “particulate Hg”, and “Hg in AC”. The parameters are listed in Table S3. The experimental process was basically the same as the step of AC adsorption performance. The process followed the steps below:
Preparation of Hg solution
The “Hg + Cl” and “Hg + DOM” tests were carried out using chloride/DOM solutions containing 20 μg L− 1 Hg in a 1 L beaker. The “Hg + S” test was carried out by mixing the equal volume (500 mL) of different concentrations of sulfide with Hg solution (40 μg L− 1) to have the solutions containing 20 μg L− 1 Hg. Each Hg solution was adjusted to pH 7.0 ± 0.5 by 0.01 M NaOH and 0.01 M HNO3 before adding AC.
The Hg solution was quantitated for 50 mL by volumetric flasks and injected into each glass vessel. The AC was then added into glass vessels and covered with a rubber stopper and aluminum cap. All of the glass vessels were then coated with aluminum foil to avoid light effect.
The samples were put into a water-bath incubating shaker and shaken at 125 rpm for 1440 min at 30 °C.
The residual Hg in the solution after AC adsorption was defined as “dissolved Hg”. For the “Hg + Cl” test, 5 mL of the solution which was filtered with 0.2 μm filter after AC adsorption was preserved and digestion with 0.5% BrCl at least 1 day before THg analysis. For the “Hg + S” and “Hg + DOM” tests, 5 mL of the solution which was filtered with 0.2 μm filter after AC adsorption was preserved with 0.5% BrCl and stored in a refrigerator at 4 °C until microwave digestion by HCl mixed with HNO3 (3:1 v/v). All the water samples were analyzed for THg by CVAFS.
The particles formed by Hg interacted with sulfide or DOM were defined as “particulate Hg”. The residual solution was filtered by 0.2 μm cellulose acetate membrane filter to intercept the particulate Hg. The membrane filter was preserved in a centrifuge tube and stored at − 20 °C. Then, freeze dryer system was used to remove moisture. The dried particulate Hg sample was microwave digested by HCl mixed with HNO3 (3:1 v/v). The samples were estimated for Hg by CVAFS.
Hg in AC
AC collected by manual screening after adsorption was defined as “Hg in AC”. After the residual solution was filtered by 0.2 μm cellulose acetate membrane filter and rinsing the glass vessel with Milli-Q water, the AC sample was collected by manual screening and stored at − 20 °C. Then, freeze dryer system was used to remove moisture. The AC sample was microwave digested by HCl mixed with HNO3 (3:1 v/v). The samples were estimated for Hg by CVAFS and the actual qe of AC was subsequently determined.
The THg in the aqueous sample was determined by CVAFS. The method detection limit of CVAFS used in this study is 0.26 ng L− 1. TOC in the water sample is oxidized to form CO2, which is then measured by a detection system (Aurora 1030w). The sulfide and chloride analyses were done by test kits and measured in the photometer (Merck Spectroquant® Prove 300). Detailed descriptions pertaining to the analyses of THg, TOC, sulfide, and chloride can be found in the Supplementary Materials.
Results and discussion
Physical and chemical properties of AC
Table 1 shows the physical and chemical properties of AC. The SBET and Smicro were 818 and 769 m2 g− 1, respectively, and the microporosity (i.e., Vmicro/Vtotal) was calculated to be 0.868, indicating that the AC used in this study is highly microporous (pore < 2 nm). This result is also supported by the pore size distribution based on NLDFT method (Fig. 1). SEM images of AC also showed that the AC used are particles with sizes around 1–1.5 mm with significant surface roughness that may increase the macropore and surface defects. As a result, without any surface modification process, the AC used retained a well-developed pore structure and distribution that could be beneficial for Hg adsorption. It is worth noting that the presence of micropores is essential for the Hg adsorption; the micropore surface area or volume, however, does not appear to be the only property that affects the Hg adsorption effectiveness . The presence of active sites, such as oxygenated functional groups in activated carbon, also governs the Hg adsorption.
AC was mainly composed of 78.9 wt% C, 4.52 wt% O, 1.41 wt% H, and 0.73 wt% N (Table 1). There was also a minor content of sulfur (0.47 wt%) in AC, however, it was not apparently existed as a functional group to adsorb Hg as shown in XPS because the peak intensity of S2p was weak (Fig. 2). XPS spectra of AC include (a) wide scan, (b) deconvoluted C1s, and (c) the deconvoluted O1s. The C1s spectra of AC in Fig. 2b could be deconvoluted into four peaks at the binding energies of 284.6, 286.0, 287.6, and 290.4 eV, corresponded to C-C, C-OH, C=O and COOH, respectively, according to Martinez et al. . The O1s spectra of AC in Fig. 2c was deconvoluted into six peaks at the binding energies of 530.2, 531.1, 531.8, 532.5, 533.4, 534.5, and 538.4 eV, corresponded to quinone, COOH, C=O, C-O, C-OH, and chemisorbed oxygen, respectively . The test AC contained numerous oxygen functional groups, which were well known as effective adsorption sites for Hg [33, 34]. Li et al.  also suggested that oxygen surface complexes, possibly lactone (COO−) and carbonyl (C=O) groups, are the potential sites for Hg capture.
Figure 3 shows the zeta potential of AC under different pH within 1–9. The zero point of charge of AC in Milli-Q water was shown to be around pH 1. Therefore, whether AC exists in natural environment or in the condition of this study (pH = 7), the surface charge of AC is always negative.
Hg adsorption performance by AC
The AC dosage test was to determine the appropriate dosage for the batch experiments with a given initial Hg concentration. The past study showed that the contact time of Hg adsorption by AC was approximately 16 h to reach equilibrium . To ensure reaching equilibrium, the contact time was set for 24 h in this part of batch experiments.
The initial Hg concentration was 18.4 μg L− 1 under different AC dosages. The results of dosage test are listed in Table 2. This result shows that the increase in Hg removal efficiency and the decrease in adsorption capacity became less significant at the dosage from 50 to 80 mg. Therefore, 50 mg AC was considered as the suitable dosage for the following experiments in this study.
The Hg adsorption kinetics are different in the presence of chloride, sulfide, and DOM in the aqueous phase. Table 3 shows the test condition and the adsorption results under various contact time of Hg adsorption in the presence of chloride, sulfide, or DOM. Figure 4 further shows the residual dissolved Hg in the solution under various contact time up to 48 h. These experimental results suggest that the behaviors of Hg adsorption are significantly different in “Hg + Cl”, “Hg + sulfide”, and “Hg + DOM” conditions. To reach equilibrium, the contact time was at least 16, 10, and 24 h in “Hg + Cl”, “Hg + sulfide”, and “Hg + DOM” conditions, respectively. In order to further understand the possible Hg adsorption mechanisms, the adsorption kinetic models should be discussed. The equations of pseudo-first-order, pseudo-second order, and intraparticle diffusion model are given in Eqs. (3)–(5) and the fitting results are shown in Table 4.
Data obtained in “Hg + Cl” condition had high R2 (0.9998 and 0.9828) by pseudo-first order and pseudo-second order model fitting (Table 4). However, the calculated qe2 is more approximate to the experimental qe. Data obtained in “Hg + sulfide” condition had a higher R2 (0.9998) by pseudo-second order model fitting than R2 (0.6886) by pseudo-first order model fitting. Data obtained in “Hg + DOM” condition had higher R2 (0.9843) by pseudo-first order model fitting than R2 (0.8503) by pseudo-second order model fitting. However, both the calculated qe1 and qe2 are similar to experimental qe in “Hg + DOM” condition. Therefore, the Hg adsorption by AC in “Hg + Cl” and “Hg + DOM” conditions may follow both pseudo-first order and pseudo-second order reaction mechanisms. The fitting result for “Hg + DOM” condition was similar to Singh et al. , which reported that the adsorption of Hg interacted with organic ligands by kaolinite obeyed multiple first order kinetics. In the multiple first order kinetics adsorption process, they suggested that one stage corresponds to the initial binding with the active sites of the solid surface . In this study, the reaction of Hg adsorption might be directly binding on AC with Hg-Cl and Hg-DOM complexes. However, the Hg adsorption reaction in “Hg + sulfide” condition was significantly different. The adsorption mechanism for “Hg + S” condition was more likely to fit pseudo-second order reaction based on the assumption that the rate-limiting step may be chemical adsorption or chemisorption involving valance forces through sharing or exchange of electrons . Since a high affinity of sulfide bind to Hg, precipitation of Hg occurred in the adsorption process. The pseudo-first order rate constants k1 for “Hg + Cl” and “Hg + DOM” were 0.0023 and 0.0009 min− 1 respectively. The pseudo-second order rate constants k2 for “Hg + Cl”, “Hg + S”, and “Hg + DOM” were 0.00057, 0.014 and 0.00022 g μg− 1 min− 1. The additional sulfide promoted the reaction rate of Hg adsorption by AC due to the precipitation of HgS. Conversely, DOM decreased the Hg adsorption rate dramatically. Hg, a soft Lewis acid, has a strong affinity for thiol functional groups in DOM. Song et al.  reported that Hg interacting with natural organic matter had high thermodynamic stability. Past research has suggested that the complexation of Hg by DOM thiol groups could hinder nanoparticle β-HgS growth [38, 39]. For inference, the same mechanism could occur in the Hg + DOM adsorption by AC. DOM worked as a barrier to inhibit the contact of Hg with AC; therefore, adsorption in “Hg + DOM” condition had the lowest rate constant.
The fitting results of intraparticle diffusion is also shown in Table 4. Data obtained in “Hg + Cl” and “Hg + DOM” condition had higher R2 (0.9980 and 0.9508). Therefore, the Hg adsorption by AC in “Hg + Cl” and “Hg + DOM” conditions are more likely depended on intraparticle diffusion. The intraparticle diffusion rate constants kp for “Hg + Cl” and “Hg + DOM” were 0.40 and 0.25 μg g− 1 min-0.5 respectively. The four basic steps of adsorption in a porous adsorbent included bulk solution transport, external transport, internal transport, and adsorption . The AC used in this study is a porous adsorbent with high volume of micropores. The rate-limiting step in “Hg + Cl” and “Hg + DOM” is likely toward to intraparticle diffusion. Therefore, the adsorption rates are low in the “Hg + Cl” and “Hg + DOM” conditions.
Preliminary adsorption capacity comparison
Tables 2 and 3 show the adsorption capacity (qe) of AC with and without additional chloride, sulfide, or DOM. The qe in the absence of these environmental factors (18.18 μg g− 1) was slightly higher than the qe in the “Hg + Cl” (14.32 μg g− 1) and “Hg + sulfide” (15.26 μg g− 1) conditions. AC in “Hg + DOM” condition had the lowest qe (10.4 μg g− 1). In past studies, chloride interacting with Hg to form a stable complex was considered as the reason for decreasing the qe of adsorbent [41, 42]. The additional sulfide seems to affect Hg adsorption on AC slightly. The DOM not only retarded Hg adsorption on AC but also decreased the qe significantly. The more detailed discussion on these effects on qe is presented in later section.
The calculation of qe is generally done by measuring the Hg concentration changes in aqueous phase before and after AC adsorption. There was a doubt appeared that whether Hg actually adsorbed on AC or not because the qe might be overestimated if Hg is reduced into Hg0 and escaped into the air. Therefore, the investigation of Hg recovery by mass balance is necessary to ensure the accuracy of calculated qe. In order to realize the influence of chloride on Hg adsorption, the recovery based on Hg mass balance before and after adsorption in the absence and presence of chloride had to be explored first (Fig. 5). The Hg recovery in the absence of chloride was 43%. The Hg recovery in the presence of chloride was 92%. Therefore, a various level of Hg could be escaped into the air in the absence of chloride. The reason for causing escape of Hg was due to the high pH value (pH = 7) of Hg solution. Chen et al.  reported that Hg0 reemission rates from the wet flue gas desulfurization slurry increased about 4 μg m− 3 as the pH values increased from 3 to 7; the Hg0 reemission rate decreased with increases chloride concentration. The acid condition could remain Hg2 + in the dissolved phase, as a result, Hg adsorption test was generally carried out under pH 3–5 [41, 44, 45]. However, the range of pH value is 6–8 in natural aquatic system. Therefore, it is reasonable to observe the apparent escape of Hg in this experimental condition (pH = 7). Nevertheless, adding chloride could enhance stabilizing Hg in the solution due to forming Hg-Cl complex. The phenomenon of Hg escaping into the air may thus possibly happen in this study as a result of the pH condition.
Hg distribution test results
The purpose of this part of the experiment is to realize the Hg distribution, including Hg in dissolved (< 0.2 μm) and solid phases (> 0.2 μm) under different concentration levels of sulfide/chloride/DOM. The test sample was divided into three parts including “dissolved Hg”, “particulate Hg”, and “Hg in AC”.
Hg + Cl″ condition
The “Hg + Cl” test was carried out by conducting Hg adsorption by AC under the chloride concentration of 1, 200, and 400 mM. Table 5 describes the experimental parameters and the results of Hg distribution. The proportion of “dissolved Hg” under chloride concentration 1, 200, and 400 mM was calculated to be 2.7, 7.9, and 4.8%, respectively. The Hg removal efficiency was similar under the chloride concentration of 1, 200, and 400 mM and more than 90% of Hg was removed. The proportion of “Hg in AC” under chloride concentration 1, 200, and 400 mM was calculated to be 92.2, 99.5, and 93.6%, respectively. The particulate Hg was undetected in “Hg + Cl” test. The Hg recovery (i.e., mass balance) in “Hg + Cl” tests was calculated to be approximately 100% (i.e., 95–107%) (Table 5 and Fig. 6). Overall, the behavior of Hg adsorption on AC was nearly the same under the chloride concentration 1–400 mM.
The comparison of calculated qe and THg removal efficiency between additional chloride concentration 0–400 mM is shown in Fig. 7. The THg removal efficiency was similar at the range of 92–95%. However, there was a significantly difference in calculated qe. The qe was 6.9, 13.8, 16.1, and 14.2 μg g− 1 under the chloride concentration 0, 1, 200, and 400 mM, respectively. The reason may be an escape of Hg into the air in the absence of chloride. Therefore, the THg removal includes two mechanisms, Hg adsorbed in AC and Hg escaped to the gas phase in the absence of chloride. Practically, the increase in chloride concentration increased qe due to the inhibition of Hg escape to the gas phase.
Past researches reported that the additional chloride decreased the Hg adsorption by AC or other relative adsorbents (Table S4). They suggested that Hg-Cl complex was a stable form and poorly adsorbed. Conversely, the presence of chloride could increase qe in this study, which contradicted to previous studies. The reason might be the initial Hg concentrations in these studies were significantly different. The initial Hg concentration of previous studies was at the range of 10–50 mg L− 1; however, the Hg concentration was approximately 20 μg L− 1 in this study. Therefore, the inhibition of Hg adsorption by chloride was not obvious in our results. The second possible reason could be an overestimate of qe in the previous studies. There was a doubt of Hg escaping into the air in the absence of chloride or in high pH condition . Nevertheless, the calculation method of qe was typically based on the difference in initial and residual Hg concentrations in previous studies. Additionally, the Hg recovery test was not conducted in these relative studies. Therefore, overestimated qe probably occurred in previous studies.
“Hg + sulfide” condition
The “Hg + sulfide” test was carried out by Hg adsorption on AC under sulfide concentrations of 2, 10, and 20 μM. Table 6 describes the experimental parameters and the results of Hg distribution. The proportion of “dissolved Hg” under sulfide concentration 2, 10, and 20 μM was 25.2, 35.1, and 25.0%, respectively; the proportion of “Hg in AC” was 28.7, 33.1, and 28.1%, respectively; and the proportion of “particulate Hg” was 28.7, 26.8, and 23.6%, respectively (Fig. 8).
Sulfide has a strong affinity for Hg tending to form Hg-S (Eq. (6)) . During an aging process, Hg-S aggregated into large particulate form of HgS [21, 26, 46]. Through 24 h contacting with sulfide, there was an amount of Hg forming into particles (> 0.2 μm) in this study. The initial Hg concentration was around 20 μg L− 1 (0.1 μM); however, sulfide concentrations (2, 10, and 20 μM) were at least 20 times higher than Hg concentration. Therefore, sulfide concentration was greatly in excess than the stoichiometric value based on Eqs. (6) and (7). Consequently, a certain proportion of particulate Hg would be formed. The Hg recovery was around 80% in “Hg + S” condition, which may be partly due to experimental error because the sample of 5 mL was firstly taken for measuring “dissolved Hg” that may cause particulate Hg loss.
Around 30% of Hg was adsorbed on AC under different sulfide concentrations. A portion of Hg was formed as HgSH + in “Hg + S” (Eq. (7)). The surface charge of AC was negative in this condition (Fig. 3). Therefore, the Hg species tended to be adsorbed on AC by Van der Wall’s force. Moreover, data from “Hg + S” test can be well fitted to the pseudo-second order model. There were two possible mechanisms to remove Hg. One of the mechanisms was chemical precipitation by Hg bonded to sulfide to form HgS(s). The other was adsorption of HgSH + by AC. Furthermore, a portion of Hg might exist in the form of HgS(aq) which was poorly adsorbed by AC. Therefore, the proportion of “dissolved Hg” in “Hg + S” (around 25%) was higher than in “Hg + Cl” (around 5%).
“Hg + DOM” condition
The “Hg + DOM” test was carried out by Hg adsorption on AC under various DOM concentration within 0.25–20 mg C L− 1. Table 7 describes the experimental parameters and the results of Hg distribution. The proportion of “dissolved Hg” under DOM concentration 0.25, 0.5, 2,10, and 20 mg-C L− 1 was 45.1, 57.8, 61.4, 68.4, and 75.7% respectively; the proportion of “Hg in AC” was 61.5, 49.3, 49.1, 26.9, and 14.7% respectively; and the proportion of “particulate Hg” was 3.1, 4.6, 3.2, 2.5, and 2.1% respectively.
Figure 9 further shows that increasing DOM concentration resulted in more dissolved phase of Hg in the solution. The proportion of “dissolved Hg” increased 30.6% from DOM concentration 0.25 to 20 mg C L− 1. This result was also reflected in “Hg in AC”. The proportion of “Hg in AC” decreased by 46.8% from DOM concentration 0.25 to 20 mg C L− 1. The reason for inhibition of Hg adsorption may be due to the affinity of DOM for Hg. The elemental compositions of SRHA are listed in Table S5. Graham et al.  reported that the reduced sulfur in SRHA is about 18.3 mol% of total sulfur. Therefore, the ratio of C to reduced sulfur is 542 (w/w). Xia et al.  reported that reduced S in SRHA analyzed by XANES was in the form of thiol/sulfide and thiophene. The thiol functional group on DOM was the major binding site with Hg [27, 28]. Among the ligands, sulfur-containing ligands bind Hg much more strongly than oxygen-containing ligands, which appear in AC . Therefore, the phenomenon of Hg escaping is not apparent and the recovery of Hg is approximately 100% (Fig. 9). In addition to thiol functional group, DOM also contained carboxyl (about 9 meq g− 1 C) and phenolic (about 4 meq g− 1 C) functional groups, which are effective binding sites for Hg [33, 34]. Hence, DOM is a large molecule tending to bind to Hg. This kind of molecule (DOM-Hg) then separated Hg from adsorption on AC. Since AC is usually nonpolar or slightly polar, DOM was considered as a stabilization agent for Hg instead of a carrier for Hg adsorption onto AC. Therefore, the DOM increased concentration may inhibit Hg adsorption dramatically.
In addition to DOM stabilizing Hg in dissolved phase, the formation of β-HgS particles from Hg2 + interacting with DOM was found in others [49, 50]. The particle size of β-HgS nanoparticles was around 3–5 nm reported by Manceau et al. . Therefore, β-HgS nanoparticles might be formed in this study. If the particle size of β-HgS was lower than 0.2 μm, it would be classified into “dissolved Hg” in this study. The formation of β-HgS nanoparticles was also a reason for increasing the proportion of “dissolved Hg”. However, β-HgS nanoparticles had the ability of aggregation. Therefore, even with the presence of DOM, β-HgS particles (> 0.2 μm) might still be formed during the adsorption process with a 24-h duration. For here, 2.1–4.6% of Hg particles were formed in “Hg + DOM”. This result showed that DOM could inhibit β-HgS aggregation significantly in this study.
The main aim of this study is to better understand the influences of chloride, sulfide, and DOM concentrations on the Hg adsorption equilibrium and kinetics of AC in an aqueous system. The important findings in this study are concluded as follows:
The rate of Hg adsorption on AC varied with the presence of sulfide, chloride, and DOM, from fast to slow. Hg adsorption might be directly bonded on AC with Hg-Cl and Hg-DOM complexes. The Hg adsorption kinetics by AC in “Hg + Cl” and “Hg + DOM” conditions are mainly controlled by intraparticle diffusion. Data from “Hg + S” test were better fitted to pseudo-second order model, resulting from Hg adsorption into AC and chemisorption of sulfide and Hg.
There were various levels of Hg escaping into the air in the absence of chloride in this study. Therefore, the investigation of Hg distribution is necessary to ensure the accuracy of calculated equilibrium capacity (qe) by mass balance, which could be overestimated by several earlier studies.
The THg removal efficiency (92–95%) was similar in the absence and the presence of chloride (1–400 mM). The increase in chloride concentration practically increased the qe due to inhibition of Hg escape in this study. This result was different with those of previous studies, which may due to the significant difference in initial Hg concentration and the overestimated qe in past studies.
The THg removal efficiency was around 65–75% in “Hg + sulfide” test. Among the removed Hg, there were 24–29% of Hg forming into particles and around 30% of Hg adsorbed on AC under sulfide concentration (2–20 μM). Hg of 25–35% might exist in the form of HgS(aq) which was hardly adsorbed by AC.
Increasing DOM concentration led to more dissolved phase of Hg in “Hg + DOM” condition. The proportion of “dissolved Hg” increased 31% from DOM concentration 0.25 to 20 mg C L− 1. Simultaneously, the proportion of “Hg in AC” decreased 47%. Thiol groups on DOM binding with Hg could separate Hg from the adsorption phase of AC and stabilize Hg in the dissolved phase.
Overall, the presence of Cl− increased the Hg adsorption on AC. It is a positive effect for AC application in thin layer capping. However, sulfide and DOM significantly decreased qe due to the formation of Hg-S and Hg-DOM. In particular, the negative effect of DOM should be overcome in future application.
Availability of data and materials
All data generated or analyzed during this study are included in this published article and its supplementary information files.
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This work was financially supported by the Environmental Protection Administration, Taiwan under Grant no. 107c000734. The opinions expressed in this paper are not necessarily those of the sponsor.
This work was financially supported by the Environmental Protection Administration, Taiwan under Grant no. 107c000734.
The authors declare they have no competing interests.
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Chen, C., Ting, Y., Ch’ng, BL. et al. Influence of sulfide, chloride and dissolved organic matter on mercury adsorption by activated carbon in aqueous system. Sustain Environ Res 30, 22 (2020). https://doi.org/10.1186/s42834-020-00065-5
- Activated carbon
- Dissolved organic matter