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Short Note

Zinc(II) Adsorption by Low-Carbon Shungite: The Effect of pH

Institute of Waste Management and Circular Economy (IAK), Technische Universität Dresden, Pratzschwitzer Str. 15, 01796 Pirna, Germany
*
Author to whom correspondence should be addressed.
Water 2018, 10(4), 422; https://doi.org/10.3390/w10040422
Submission received: 12 March 2018 / Revised: 29 March 2018 / Accepted: 30 March 2018 / Published: 3 April 2018
(This article belongs to the Section Wastewater Treatment and Reuse)

Abstract

:
Shungite is a carbonaceous rock which is abundant in Karelia (Russian Federation). Large deposits of shungite with low levels of carbon (approx. 10% C) are also found in Kazakhstan, where it is mined under the trade name Taurit (Koksu Mining Company). Although Taurit has been reported to be used as an adsorbent for hazardous compounds in water treatment, there is very little precise data about its adsorption capacity or the compounds adsorbed. In this study, the ability of Taurit to adsorb Zn(II) was investigated and Freundlich isotherms were determined for both distilled water and tap water. Taurit was found to have a high buffer capacity leading to pH values > 7.0 in aqueous solution. Because dissolved zinc precipitates as Zn(OH)2 under alkaline conditions, the pH must be carefully controlled and kept ≤7.0. Despite the small inner surface area (BET) of Taurit (13.4 m2 g−1), Freundlich coefficients for distilled water (Kf = 2.4, n = 4.0) and tap water (Kf = 1.5, n = 2.5) were similar to other adsorbents. Our results indicate that Taurit could provide a cheap alternative to activated carbon since both substances have a similar adsorption capacity (at least for Zn(II)).

1. Introduction

Deposits of shungite, a carbonaceous rock, are mainly found in the Russian Federation. Although sometimes defined as a mineral, it does not appear in the international list of minerals [1]. Shungite’s carbon content varies, resulting in different qualities and prices, and in some cases is nearly 100% (‘noble shungite’). It is mainly used as black pigment in industry. High qualities have a lustrous sheen and are often used as talismans. Poor-quality shungite (i.e., with a carbon level <10%) is used in the polymer industry and mainly produced in Kazakhstan under the brand name Taurit (Koksu Mining Company). Shungite has been known for decades to contain fullerenes, the main aspect addressed by relevant scientific articles [2]. Shungite can theoretically be used as a filter material in wastewater treatment and water purification [3]. Therefore, it may be possible to use Taurit as a substitute for activated carbon (AC) in for example water treatment plants. However, reliable information about the possible use of Taurit or other forms of shungite for this purpose is scarce. Shungite has been investigated as a matrix for the immobilization of microorganisms [4]. The study addressed the treatment of contaminated water from the Botakhan oilfield in the Makat district (Atyrau region, Kazakhstan). The use of carbonaceous matrices in this field is well known and many studies have been conducted on activated carbon [5]. However, to our knowledge, neither low- nor high-carbon shungite is currently used as a substitute for activated carbon. A small experiment involving Taurit and fuel hydrocarbons demonstrated no noteworthy adsorption [6]. Then again, in another experiment, Taurit demonstrated a promising affinity for inorganic compounds. Kenzhebayev et al. examined the successful adsorption of aluminum on Taurit [7]. In the present study, we explored the ability of Taurit to remove Zn(II) from aqueous solutions—a useful function since high zinc concentrations can cause health problems such as stomach cramps, vomiting, skin irritations, and anemia [8].

2. Materials and Methods

2.1. Characterization of Taurit

Taurit (black powder) was supplied by GHI, Pirna, and used without being treated in any way (e.g., by washing) as this may have affected its properties. Since no datasheet was provided, the shape of the particles was analyzed by microscope (Nikon Eclipse 50i, Nikon Corporation, Tokyo, Japan). The grains were found to have an average diameter of 10.8 ± 3.2 µm and a maximum diameter of 17 µm. More accurate grading was not possible for our experiments.
The surface area (BET) of the Taurit particles was determined by the Institute for Groundwater Management, Technische Universität Dresden, to be 13.4 m2 g−1. The micropore volume was 0.0047 mL g−1.
The elemental composition of the Taurit sample used was determined by X-ray fluorescence analysis (RFA determination, Spectro XEPOS, Spectro Analytical Instruments GmbH & Co. KG, Kleve, Germany). Total carbon (5.4%) and total organic carbon (5.2%) were determined in an elemental analyzer (multi EA 2000, Analytik Jena AG, Jena, Germany). Although oxygen and hydrogen were not determined, Si and many other elements are known to be present in Taurit, mainly as oxides [3]. Given this information, the composition of the Taurit used was calculated to be 70.6% SiO2, 11.3% Al2O3, 5.9% Fe2O3, 2.5% K2O, and trace amounts of some elements (Ca, Mg, etc.). The elements detected are presented in Supplementary Materials.

2.2. pH Tests

Experiments to determine the optimal pH for adsorption (pH 2.5–7.0) were conducted as batch sorption studies in 100 mL gastight vessels each containing 40 mL aqueous solution and 1 g Taurit. The suspensions were agitated (150 rpm, 1 day) and nitric acid was used for pH adjustment.
Precipitation experiments were conducted in duplicate and without Taurit. Zinc solutions (50 mg L−1) were prepared in 100 mL gastight flasks and stirred for 24 h. The initial pH values (7.0, 8.6, 9.6, and 10.9) were monitored with an electrode (WTW, Weilheim, Germany) and continuously adjusted with diluted sodium hydroxide or nitric acid. To remove the precipitated zinc, all solutions were filtered before analysis in a stainless steel pressure filter holder (type SM16249) equipped with a 0.2 µm cellulose acetate filter (Sartorius, Göttingen).

2.3. Buffer Capacity of Taurit

The acid neutralization capacity of soil samples was measured as described by Rowell [9]. In each test, after a suspension of 1 g Taurit and 30 mL distilled water had been placed inside a 100 mL vessel, 1 M nitric acid was gradually added. Twelve samples and one blind sample (without acid) were prepared in parallel, resulting in 13 different pH values between 2.5 and 9.4. The mixtures were shaken for 24 h in an overhead shaker (Reax 20, Heidolph, Schwabach, Germany) at a frequency of 3 min−1. Due to a small pH shift during the first minute, the pH values were determined again after 5 min. At the end of the experiment, the pH values were measured again and found to have remained constant over this time. The acid neutralization capacity was determined in mmol H+ g−1 pH−1.

2.4. Batch Sorption Studies

A stock solution of zinc sulfate (100 mg L−1) was produced. The grade of ZnSO4 was defined as “pure for analysis” (Grüssing GmbH, Filsing, Germany) and used as received. Water was purified with a Milli Q system (Millipore, Merck KGaA, Darmstadt, Germany). Taurit was weighed and placed inside vessels. Batch sorption experiments were carried out in 22 mL gastight vessels (headspace vials) containing 20 mL of water and the suspensions were agitated (150 rpm, seven days) in a conventional shaker (SM-30 Control, Edmund Bühler GmbH, Hechingen, Germany) at room temperature with different quantities of Taurit (0.1, 0.2, 0.3, 0.4, 0.5, 0.6, 0.8, and 1.0 g 20 mL−1). The pH was 5.6 in distilled water and 7.0 in tap water throughout the experiments. To determine the required contact time, a long-time experiment (21 days) was performed with a 500 mL gastight vessel and 5 g Taurit. The final concentration of metals was determined with an atomic absorption spectrophotometer (AAS Spectrometer 4100, Perkin-Elmer GmbH, Berlin, Germany). Each adsorption experiment was carried out twice; each metal was determined in triplicate. The data shown are mean values of all assays. The percentage of metal removal and the quantity of metal ions adsorbed by the Taurit were calculated by the following equations:
% removal = ((C0Ce) C0−1) 100
qe = ((C0Ce)V) m−1
where C0 and Ce are the initial and equilibrium concentration of metal ions in solution respectively, qe the amount of zinc ions adsorbed at equilibrium, V the solution volume, and m the mass of Taurit. The Freundlich isotherm equation qe = kf Ce1/n can be written in the linear form
log qe = log kf + 1/n log Ce,
where qe and Ce are the equilibrium concentrations of Zn in the adsorbed and liquid phases in mg g−1 and mg L−1, respectively, and kf and n are the Freundlich constants related to the sorption capacity and sorption intensity, respectively.

3. Results and Discussion

3.1. Influence of pH

To assess the influence of pH, zinc adsorption was primarily tested from pH 2.5 to 7.0. Figure 1 shows the results.
The highest removal efficiency was achieved at pH 7.0, and so further adsorption experiments were carried out at neutral pH. Zinc adsorption cannot be determined under alkaline conditions because substantial amounts of solid zinc hydroxide are formed at pH values > 7.0. Therefore, previous studies mainly examined zinc adsorption at pH ≤ 7.0 [10,11,12]. Some studies investigated zinc adsorption on activated carbon or zeolite over a wide pH range [13,14,15,16]. In these cases, a pH of 6.5 to 7.0 proved optimal for zinc adsorption, which tallies with our findings. Interestingly, however, some authors did not observe zinc precipitation under alkaline conditions [13,14,15,16]. One study even reported dissolved zinc in concentrations of up to 30 mg L−1 at pH 10.0 [17], which is clearly impossible because the solubility product of zinc is too low [18]. Lim et al. [19] investigated zinc adsorption on powdered fish bones from pH 2.0 to 10.0. The authors found that Zn2+ removal increased drastically (by up to 100%) at a pH between 6 and 10. However, further experiments were carried out at pH 5 because metal precipitation occurred at alkaline pH values. The contradiction in the authors’ statement (“best removal” at pH 5 and “100% removal” at pH 9) was not discussed. Therefore, we decided to conduct a small experiment regarding the influence of alkaline pH on zinc precipitation. Experiments (without Taurit) were conducted at four different pH values. In each case, the zinc concentration at the beginning was 50 mg L−1. The solutions were filtered and the zinc concentration in solution was determined. Table 1 shows the results.
First of all, it proved difficult to achieve a stable pH in aqueous solution. Contact between alkaline solutions and air has to be avoided due to the formation of carbonic acid. A non-adjusted solution in a parallel vessel with air contact exhibited a pH decrease from 10.5 to 8.2 over a period of a few hours. Additionally, when the consumption of the available OH by zinc ions was complete, the pH sharply increased. The reason is presumably the formation of different Zn(OH)x species which trapped the hydroxide ions for a long time. The zinc species markedly affected the pH value. The behavior of the zinc species Zn2+ and Zn(OH)+ corresponds to a buffer system. Higher OH concentrations lead to the formation of Zn(OH)+ while the addition of H+ releases Zn2+ ions. The addition of excess alkaline leads to the precipitation of zinc(II) as Zn(OH)2. This reaction is nearly quantitative at pH 9–10.
As expected, at alkaline pH values, nearly no dissolved zinc was detected due to the formation of insoluble Zn(OH)2. Zinc concentrations at pH ≥ 9.6 were near the detection limit (0.02 mg L−1). The slightly higher concentration at pH 10.9 may come from the slow formation of Zn(OH)3, which may take a few days. A corresponding experiment—the dissolution of solid zinc hydroxide at different pH values—was performed by Reichle et al. [18]. The concentration of zinc in these solutions usually approached constancy in about 10 days. Buffer reactions of zinc and zinc hydroxide may have led to pH values ≤ 7.0 in some experiments, preventing zinc precipitation. An indication of this can also be seen in the Materials and Methods parts of some studies examining pH. The phrase “initial pH values” was used very often [13,14,15,16], leading to the conclusion that the pH was not continuously measured in these studies.
Taurit may contain soluble compounds which could influence the pH value. Therefore, the impact of different Taurit masses on the pH was investigated. Figure 2 shows the results.
Evidently, Taurit can release some compounds into aqueous solutions followed by an increase in pH. At pH values > 7.0, metal removal is increased due to the formation of metal hydroxide precipitation. Presumably, protons are bound on the Taurit surface and ions are released—i.e., Na, K, Ca, etc.—by carbon into the solution (see Section 3.2). This behavior has been observed also at natural adsorption materials on carbon basis [20].
Since the pH has a strong influence on the transformation of zinc species and therefore on their solubilities, the pH has to be carefully controlled during adsorption experiments.

3.2. Acid Neutralization Capacity (ANC)

Because the pH value has a strong impact on adsorption behavior and also on the formation of various zinc species, the acid neutralization capacity of Taurit was determined. Figure 3 shows the results.
Despite the lack of detailed information about the structure and surface area of Taurit, it can be assumed that ion exchange processes are responsible for this behavior. In the neutral or weak alkaline region, the surface of Taurit is covered with cations like K+ and Ca2+. The functional groups on the surface of Taurit have a weakly acidic character, i.e., protonation takes place at pH ≤ 8.0 and the metal ions are dissolved. These ion exchange processes evidently play an important role. The course of the graph is typical of different buffer systems of soil. The decrease in pH is dependent on the kinetics and the quantity of buffer substances. For pH > 4.0, an ANC of 59 mmol H+ kg−1 pH−1 was determined. For pH < 4.0, ANC was 240 mmol H+ kg−1 pH−1. Table 2 shows some buffer capacities of different types of soil [9].
The high ANC of Taurit at pH < 4.0, which even exceeds the ANC of peat, may be explained by the dissolution of mineral components of Taurit consuming high amounts of acid, similar to siliceous rocks [9]. Since the surface of Taurit is increasingly covered with protons under acidic conditions, positive zinc ions are pushed back and the adsorption capacity of Taurit has an optimum at pH 7.0.

3.3. Contact Time

Figure 4 shows the long-term adsorption behavior of Zn(II) at pH 5.6 (distilled water) at room temperature (5 g Taurit, 500 mL distilled water, pH 5.6, 110 mg L−1 Zn(II)).
Adsorption on Taurit clearly takes longer compared to other adsorbents. In the literature, data of adsorption experiments with reported equilibrium times of >1 day are rare. Sotelo et al. [21] reported adsorption times for activated carbon of 3 days (caffeine) and 14 days (diclofenac). The adsorption of Zn(II) was nearly complete after three days and only continued to a small extent. After one week (168 h), it was evidently finished. Therefore, further experiments were carried out with an adsorption time of seven days each. Unfortunately, no data about equilibrium times for the adsorption of organic or inorganic compounds on shungite was found in the literature. However, a wide variety of adsorption times for both activated carbon and silica were found, which may serve as an indication. Krishnan et al. [17] investigated the adsorption of Zn(II) on sulfurized activated carbon and found it to be complete after 4 h. Shrestha et al. [22] examined Zn(II) adsorption on coconut shell-based activated carbon fibers and found an optimal contact time of just 50 min. A good overview of the adsorption of Zn(II) on various minerals containing natural silica is provided in Malamis and Katsou [23], the authors examining 254 related articles. The equilibrium times were mostly <24 h.

3.4. Adsorption Experiments

The pH was monitored and maintained ≤7.0 at all times. At this pH, the soluble compounds Zn2+ and Zn(OH)+ are the main species. Figure 5 shows Freundlich isotherms for the adsorption of Zn(II) on Taurit in distilled water and tap water, respectively (T = 25 °C, 0.1–1.0 g Taurit, 20 mL water, 100 mg L−1 Zn(II)). The pH was 5.6 in distilled water and 7.0 in tap water.
The adsorption behavior of zinc on Taurit was similar in both experiments. Nonlinear approximation gave correlation coefficients R2 of 0.9728 (distilled water) and 0.9735 (tap water), respectively.
Table 3 shows some Freundlich isotherm parameters for zinc adsorption on zeolite (silica) and activated carbon reported by other authors.
The adsorption of Zn(II) on Taurit was similar to other adsorbents i.e., the Freundlich coefficients were within the same range. This is surprising given the small BET surface of Taurit (13.4 m2 g−1) and the small micropore volume (0.0047 mL g−1). It indicates that Zn(II) adsorption is much more dependent on the concentration of specific active sites on the surface of the Taurit rather than the total surface area available. However, adsorbents’ efficiency for the removal of heavy metals should also be estimated under conditions similar to those found in water or wastewater samples. For a practical approach, a limit value for zinc in water has to be taken into account. The WHO has published a permissible limit for zinc (drinking water) of 3 mg L−1 [8]. This was used as an adequate regulation value. Classifying Taurit compared to other adsorbents entails monitoring the efficiency (i.e., the adsorption capacity) achieved at the limit concentration of zinc. Some of the above-mentioned studies [26,27] were carried out with residual zinc concentrations of 3 mg L−1. The corresponding Freundlich isotherms showed an uptake qe of 1.5, 1.7, 2.5, and 12 mg g−1 which is largely similar to Taurit with an uptake of 2.3 and 3.2 mg g−1 for tap water and distilled water, respectively. Therefore, Taurit seems to have adsorption capacities similar to activated carbon, at least for the adsorption of Zn(II). Taurit could therefore provide a cheap alternative. The actual price on the world market per ton for activated carbon used in wastewater treatment—including supply to Europe—is approx. five times higher than for Taurit [28].

3.5. Influence of Sulfate Concentration

Whether sulfate plays a role during zinc adsorption could not be ruled out. Therefore, sulfate concentrations were monitored throughout. To assess any sulfate adsorption, a zinc sulfate solution and increasing masses of Taurit were tested (20 mL zinc sulfate solution with 150 mg L−1 sulfate). Table 4 shows the results.
With one exception, the longer the contact time, the higher the adsorption of sulfate. However, the results were illogical because increasing Taurit masses led to the lower adsorption of sulfate. A blank was tested (1 g Taurit without sulfate) and this solution also contained sulfate (6.8 mg L−1). No zinc was found. Distilled water contained no sulfate. The molar mass of sulfur is 32.06 g mol−1 and sulfate 96.06 g mol−1. RFA determination of Taurit indicated a sulfur content of approx. 0.02%. 20 mg sulfur (0.624 mmol) in 20 mL solution could theoretically lead to 3000 mg L−1 sulfate (theoretical value) in the 20 mL vials used. Obviously, only a small percentage of the sulfur within Taurit is sulfate. The results indicate that although a small amount of sulfate can be adsorbed on Taurit, it can also be released to a certain degree, masking the adsorption effects. Any influence of the low sulfate concentrations on zinc adsorption is presumably low and was therefore neglected.

4. Conclusions

Despite the fact that BET surface area of Taurit is insignificant, a remarkable adsorption of Zn(II) was observed. However, the reasons for the long equilibrium time are not clear. Therefore, some unknown factors e.g., ion exchange processes must have a strong impact on adsorption behavior which have to be identified in further studies.
Although a (theoretically possible) fullerene content and its presumable influence on adsorption were not investigated, any fullerene content in Taurit ought to be low due to the small percentage of organic carbon. During adsorption experiments, the solution’s pH has to be carefully controlled and adjusted as it greatly affects the solubility of zinc. Additionally, the formation of Zn(OH)2 can lead to unexpected pH jumps. Our studies indicate that low-carbon shungite (Taurit) could be used as an alternative adsorbent for Zn(II) from water. Furthermore, due to the slight alkaline release of Taurit, enhanced metal removal could be accomplished by the precipitation of zinc. To our knowledge, this is the first scientific study to indicate the possible application of Taurit for water purification.

Supplementary Materials

The following are available online at https://www.mdpi.com/2073-4441/10/4/422/s1. Table S1: Results of the chemical characterization of the Taurit used. Average values for three replicates with coefficients of variation always <5%.

Acknowledgments

We would like to thank the Federal Ministry of Education and Research (BMBF) for kindly funding this work (project KoneFP, grant no. 01DK15003). We would also like to thank Paul Jakubczyk (GHI) for supplying the Taurit as well as D. Burghardt and D. Degenhardt from the Institute for Groundwater Management, Technische Universität Dresden, for determining its BET surface area. We gratefully acknowledge the support of the German Research Foundation and the Open Access Publication Funds of SLUB/TU Dresden.

Author Contributions

Axel R. Fischer conceived and designed the experiments; Luisa Sgolik and André Kreller performed the experiments and analyzed the data; Axel R. Fischer wrote the paper; Christina Dornack corrected and improved it.

Conflicts of Interest

The authors declare no conflicts of interest.

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Figure 1. Influence of pH on zinc adsorption on Taurit.
Figure 1. Influence of pH on zinc adsorption on Taurit.
Water 10 00422 g001
Figure 2. Influence of Taurit mass on pH.
Figure 2. Influence of Taurit mass on pH.
Water 10 00422 g002
Figure 3. Acid neutralization capacity of Taurit (a) until pH 4.0 and (b) from pH 4.0.
Figure 3. Acid neutralization capacity of Taurit (a) until pH 4.0 and (b) from pH 4.0.
Water 10 00422 g003
Figure 4. Effect of contact time on the adsorption of Zn(II).
Figure 4. Effect of contact time on the adsorption of Zn(II).
Water 10 00422 g004
Figure 5. Freundlich isotherm for the adsorption of Zn(II) on Taurit: (a) distilled water; (b) tap water.
Figure 5. Freundlich isotherm for the adsorption of Zn(II) on Taurit: (a) distilled water; (b) tap water.
Water 10 00422 g005
Table 1. Dissolved zinc concentrations at different pH values (start: 50 mg L−1).
Table 1. Dissolved zinc concentrations at different pH values (start: 50 mg L−1).
pH 7.0pH 8.6pH 9.6pH 10.9
54.4 mg L−10.34 mg L−10.02 mg L−10.06 mg L−1
Table 2. Buffer capacities of various soil types (mmol H+ kg−1 pH−1).
Table 2. Buffer capacities of various soil types (mmol H+ kg−1 pH−1).
SandClayHumusPeat
168080128
Table 3. Freundlich isotherm parameters for zinc adsorption.
Table 3. Freundlich isotherm parameters for zinc adsorption.
AuthorsAdsorbentBET (m2 g−1)kf (mg Zn/gads)/(mg/L)n
[24]Zeolite 4A-1.1412.200
[24]Zeolite 13X-0.8012.315
[24]Bentonite-0.6272.377
[13]Zeolite30–600.0153.058
[25]Zeolite260.9241.89
[14]Sulfurated AC-20.70.32
[15]AC6080.161.0
[17]AC100641.633.214
[22]Coconut AC-0.95743
[26]AC-2.412.22
[27]AC76810.055.54
[27]AC (F-400)9871.0222.05
[27]AC (F-300)8631.8273.38
This studyTaurit/dist H2O13.42.44.0
This studyTaurit/tap H2O13.41.52.5
Table 4. Adsorbed sulfate mass (mg sulfate/mg Taurit) in %.
Table 4. Adsorbed sulfate mass (mg sulfate/mg Taurit) in %.
Taurit Mass (g)24 h 7 Days
0.13.79.2
0.23.99.2
0.33.15.9
0.42.02.9
0.53.32.0
0.61.13.9
0.81.23.9
1.001.3
1.100

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MDPI and ACS Style

Fischer, A.R.; Sgolik, L.; Kreller, A.; Dornack, C. Zinc(II) Adsorption by Low-Carbon Shungite: The Effect of pH. Water 2018, 10, 422. https://doi.org/10.3390/w10040422

AMA Style

Fischer AR, Sgolik L, Kreller A, Dornack C. Zinc(II) Adsorption by Low-Carbon Shungite: The Effect of pH. Water. 2018; 10(4):422. https://doi.org/10.3390/w10040422

Chicago/Turabian Style

Fischer, Axel R., Luisa Sgolik, André Kreller, and Christina Dornack. 2018. "Zinc(II) Adsorption by Low-Carbon Shungite: The Effect of pH" Water 10, no. 4: 422. https://doi.org/10.3390/w10040422

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