Levent Pelit*,
İlknur Bağatır,
Füsun Okçu Pelit and
F. Nil Ertaş
Ege University, Faculty of Science Chemistry Department, 35100 Bornova-Izmir, Turkey. E-mail: levent.pelit@ege.edu.tr; ilknur.bagatır@ege.edu.tr; fusun.okcu@ege.edu.tr; niler@mail.ege.edu.tr; Fax: +90 2323888264; Tel: +90 2323111778
First published on 4th July 2014
This study describes a rapid, simple and sensitive spectrophotometric method for determination of Hg(II) ions in saline samples by a single-drop microextraction (SDME) technique. The method is based on the extraction of dithizone (DTZ) complex of mercury(II) into an undecanol droplet which serves as the organic phase, and then the absorbance of the colored complex is measured at 490 nm by using a microvolume quartz cuvette. This procedure provides a simple, rapid, cost-efficient and, most of all, a green method for detecting mercuric ions by minimizing the organic solvent consumption. A variety of parameters affecting the signal, such as pH, DTZ concentration, sample and extraction solvent volume, extraction time and temperature and salt effects were optimized. Under optimized conditions the linear range was found between 3.2 × 10−8 and 5.0 × 10−7 mol L−1 (6.4–100.8 μg L−1) and the detection limit was calculated as 9.6 × 10−9 mol L−1 (1.9 μg mL−1) attained by a high enrichment factor of 203. The performance and accuracy of the method were compared with those of atomic fluorescence spectrometry. Validation of the proposed method was performed for determination of mercury in saline samples including sea water, mineral water, thermal spring water, and table and rock salt samples, which is difficult to analyze by conventional methods.
Inorganic mercury occurs naturally in the environment and is also released as a consequence of human activities. Surface waters in the vicinity of industrial areas are important indicators for mercury pollution.5,6 The amount of total mercury is usually in the range of 0.5–5 ng mL−1 in natural and fresh waters and increases to several μg mL−1 levels in contaminated waters.7 For drinking water, the EPA recommends a limit of 2 ng mL−1.8 Therefore, analytical monitoring of trace amounts of mercury in surface waters is of great significance for public health safety and environmental pollution control.
Numerous analytical techniques have been used for the determination of trace levels of mercury in water samples, including atomic absorption spectrometry,9 cold vapor atomic absorption spectrometry,10 atomic fluorescence spectrometry (AFS),11,12 inductively coupled plasma with optical emission spectrometry13 and mass spectrometry14 along with X-ray fluorescence spectrometry.15
Although these methods provide sensitive tools for mercury determination in environmental samples, their application to saline samples is cumbersome due to the impairment of direct analysis resulting from the high ionic strength of such samples.16 For this purpose, in situ solid-phase preconcentration methods were utilized for avoiding interferences and improving the sensitivity of the method.7,17
Electrochemical methods provide a more economical and yet sensitive tool for mercury determination in saline samples. A study carried out in the authors' lab has revealed that the mercury content of table salt samples can be determined at a gold film electrode by anodic stripping voltammetry.18 The interference arising from high chloride content was eliminated by applying a medium-exchange after the deposition step.
Spectrophotometric methods, on the other hand, are some of the most common methods due to their simplicity and inexpensive instrumentation with reasonable sensitivity for determination of mercuric ions.19–23 However, mercuric ions usually exist in the environment at trace levels in rather complicated matrices, and thus extraction and pre-concentration procedures are essential in photometric detection.7 After complexation of mercury(II) with different types of reagents, the complexes are extracted in chloroform, toluene, xylene or carbon tetrachloride prior to the measurement.24 However, the use of these solvents is to be avoided due to their toxicity, and they display some drawbacks such as large consumption of reagent, high volatility and low enrichment factor. As a result greener and faster methods for monitoring the trace levels of mercury are being sought.
Among the currently available extraction and preconcentration methods, miniaturized preconcentration methods have been attempted for liquid–liquid extraction systems based on single-drop microextraction (SDME),25,26 solidified floating organic drop microextraction (SFODME),27 and dispersive liquid–liquid microextraction (DLLME)28 for the determination of mercuric ions in different samples. These techniques have recently aroused a great interest, due to their favorable characteristics of simplicity, rapidity, cost-effectiveness and minimized toxic and flammable organic solvent consumption.29 High enrichment factor can be easily obtained by SDME since microliter volumes of liquid drops are used.30 Previously, organic solvents like carbon tetrachloride, cyclohexane, toluene, m-xylene, and n-octane have been used in SDME as the extracting phases.30–32 However, the use of such solvents in SDME is limited due to their high rate of dissolution and evaporation in addition to emulsion formation during extraction.33 Recently, low-volatility compounds such as ionic liquids34–36 have been used instead of toxic, flammable and water-miscible organic solvents. As an alternative to ionic liquids, a greener solvent, undecanol, was used as the extracting phase in a recent study.27 Mercuric ions were complexed with diethyldithiocarbamate, and then extracted into fine droplets of 1-undecanol. After cooling in an ice bath, the solidified microdrop was transferred for determination by cold vapor AFS.
The present study includes the early findings of a novel method which utilizes a microdroplet of undecanol as the extracting solvent for the first time for Hg(II) ions complexed with dithizone (DTZ). The absorbance of the colored complex trapped in the droplet is then measured by using a microvolume quartz cuvette. The optimization of experimental conditions, possible interferences, analytical characteristics and method validation were investigated in detail. The applicability of the method for saline samples was also investigated.
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| Fig. 1 The absorption spectrum and the color of undecanol phase after DTZ and Hg(II)–DTZ extraction. | ||
The effect of pH on the extraction efficiency was investigated by using 0.01 M Britton–Robinson (BR) buffer solutions in a wide range of pH. As shown in Fig. 2, the absorbance of the extracted solution has a maximum in the pH range of 6.5–8.0, and therefore pH 7.2 was chosen. Buffer type and concentration were also studied. Phosphate buffers at the same pH were tested and no significant difference was observed in a concentration range of 0.03–0.1 mol L−1. Therefore, 0.1 mol L−1 phosphate buffer at pH 7.2 was finally selected.
Temperature is another important parameter to be optimized for an efficient extraction. As shown in Fig. 3, the absorbance of Hg(II)–DTZ in undecanol phase is highly dependent on the temperature, having a maximum at 45 °C. The decline in the signal for higher temperatures can be explained by the instability of the complex. Consequently, further extraction processes were carried out at 45 °C.
For accurate and precise analysis, extraction time should be optimized since mass transfer of the complex between water and undecanol phases is time dependent. The effect of the extraction time on the signal was investigated between 5 and 45 min and plotted against the measured absorbance (Fig. 4). Extraction efficiency is substantially increased with increasing extraction time up to 15 min and then shows a plateau after 20 min. Hence, the experiments were carried out using 20 min optimal extraction time.
The dependence of the extraction efficiency on the solvent volume was investigated in the range of 5–100 μL. An undecanol nanodrop was picked from a solution containing 7.5 × 10−6 M Hg(II) and 1.5 × 10−5 M DTZ. A stable and relatively strong signal was observed in the range of 5–20 μL (Fig. 5). Considering that mass transfer of the complex into the organic phase occurs only by diffusion, a concentration gradient is produced in the drop for non-equilibrium conditions, thereby explaining the lower extraction efficiency observed for larger volumes.
In the next step, the sample volume was changed in the range of 1.0–20 mL with the undecanol volume kept constant at 15 μL. The extraction efficiency increased with sample to organic phase volume ratio as shown in Fig. 6. Here, 10 mL of sample volume was chosen since the reassembling of the microdrop distributed into higher sample volumes is more challenging.
It is well known in liquid-phase microextraction that the addition of salt to the sample solution can increase the mass transfer of hydrophobic compounds into the extract phase (salting-out effect). On the other hand, the salt dissolved in the sample solution can change the physical properties of the Nernst diffusion layer altering the extraction kinetics.37 Therefore, salt concentration in the sample solution should be optimized. In this study, the salting-out effect was investigated by addition of NaCl to the sample in the range 0.02–0.50 mol L−1. As shown in Fig. 7, the extraction efficiency of Hg(II)–DTZ complex increased up to 0.1 mol L−1 NaCl concentration and at higher NaCl concentration no significant change was observed. On the basis of these results, further experiments were performed at 0.1 mol L−1 NaCl concentration.
In terms of sensitivity, instrumental parameters were also taken into consideration and the light path was changed from 0.2 mm to 1 mm to improve the absorbance signal for low Hg(II) concentration. Also, agitation of the sample solution allows an enhancement of the extraction kinetics as a result of the reduction of the Nernst diffusion film. Agitation of sample reduces the time required to reach equilibrium between the sample solution and undecanol phase. In this work, the effect of the agitation rate was studied in the range 50–250 rpm. The extraction efficiency increased with increasing stirring rate up to 250 rpm (Fig. 8). Larger agitation rates were avoided since the fine undecanol droplets dispersed into the solution cannot be easily collected. Thus, 250 rpm was selected as a compromise between sensitivity and the practicality of the method.
The last parameter to be optimized is the DTZ concentration which is expected to have a direct influence on the extraction efficiency of the Hg(II) complex. Generally, low ligand concentrations result in inefficient complex formation, but high concentrations would also reduce the absorbance signal as the free ligand tends to dissolve in undecanol phase. Therefore, the effect of DTZ concentration was examined in the range of 1.0 × 10−6 to 2.0 × 10−6 mol L−1 and absorbance at 490 nm was plotted against DTZ concentration after baseline correction (Fig. 9). The signal has a maximum at 1.5 × 10−6 mol L−1 and this concentration was selected for further studies.
| Linear working range | (3.2–50) × 10−8 (mol L−1) | 6.4–100.8 (μg L−1) |
| Linear equation | A = 1.61 × 106[C] − 0.0116 | |
| (R2) | 0.9989 | |
| LOD | 9.6 × 10−9 (mol L−1) | 1.9 (μg L−1) |
| LOQ | 3.2 × 10−8 (mol L−1) | 6.4 (μg L−1) |
| RSD % (intra-day) (n = 7) | 8.5 | |
| RSD % (inter-day) (n = 7) | 13.4 | |
| Enrichment factor | 203 | |
The repeatability of the method, expressed as relative standard deviation (RSD), was evaluated by extracting seven consecutive aqueous samples spiked at 1.0 × 10−7 mol L−1 with Hg(II). Furthermore, the inter-day reproducibility was estimated by performing the calibration procedure over five consecutive days.
The enrichment factor is defined as the ratio of the final analyte concentration in the extracting phase to the initial aqueous sample concentration. Hg(II) content of a 5 × 10−8 M Hg(II) solution was determined by the AFS method prior to and after the procedure was applied. The enrichment factor was calculated as 203 which can be ascribed to the high sensitivity of the photometric method.
| Foreign ion added | Interference/metal ratio (M/M) |
|---|---|
| Zn2+ | 1 |
| Cu2+ | 5 |
| Pb2+ | 50 |
| Ni2+, Co2+, Ca, Cd, Mg | 500 |
| Cd2+, Cr3+ | 5000 |
| Al3+, Bi3+, Fe2+, Fe3+, K+, Mn2+ Br−, NO3−, SO42− | No interference |
Another solution is to use EDTA as masking reagent. In fact, Zn(II) ions severely interfere in the measurement yielding a strong absorption at 490 nm not only due to its competition for DTZ, but also the ability of the complex to transfer to the undecanol phase Therefore, this co-extraction results in elevated signal formation which can be simply eliminated by adding EDTA so as to be 0.01 mol L−1 in the mixture. By this means the interference of Zn(II) and other interfering ions can be prevented up to 5.0 × 10−4 mol L−1 without any change in the signal of Hg(II) at ppb level.
For this purpose the Hg(II) standard solutions were added into sample so as to be 2.0 × 10−8, 1.0 × 10−7, and 5.0 × 10−7 mol L−1 and their recovery values were calculated. The recovery assays were replicated three times and acceptable recovery values were obtained (Table 3). The same samples were also analyzed with a reference AFS method for the verification of the accuracy of the method. The results are presented in Table 3. As can be seen from the results, mercury content of the samples found by the proposed method was in good agreement with AFS results.
| Sample type | Hg(II) found by | Spiked Hg(II) (mol L−1) | Recovery (%) | |
|---|---|---|---|---|
| Proposed method | AFS | |||
| a LOD for AFS is 35 ng L−1. | ||||
| Sea water | <LOD | 0.19 μg L−1 | 2.0 × 10−8 | 88.9 ± 7.2 |
| 1.0 × 10−7 | 100.4 ± 5.1 | |||
| 5.0 × 10−7 | 86.6 ± 3.7 | |||
| Thermal spring water | <LOD | <LODa | 2.0 × 10−8 | 114.6 ± 8.8 |
| 1.0 × 10−7 | 98.6 ± 3.8 | |||
| 5.0 × 10−7 | 102.3 ± 3.4 | |||
| Mineral water | <LOD | 0.23 μg L−1 | 2.0 × 10−8 | 112.4 ± 5.5 |
| 1.0 × 10−7 | 98.9 ± 3.7 | |||
| 5.0 × 10−7 | 100.2 ± 2.9 | |||
| Table salt | 0.78 μg kg−1 | 0.64 μg kg−1 | 2.0 × 10−8 | 113.4 ± 10.1 |
| 1.0 × 10−7 | 88.0 ± 5.6 | |||
| 5.0 × 10−7 | 100.3 ± 8.2 | |||
| Iodized table salt | 7.73 μg kg−1 | 8.14 μg kg−1 | 2.0 × 10−8 | 110.9 ± 6.1 |
| 1.0 × 10−7 | 103.4 ± 3.5 | |||
| 5.0 × 10−7 | 99.2 ± 2.2 | |||
| Rock salt | 0.15 μg kg−1 | 0.12 μg kg−1 | 2.0 × 10−8 | 102.3 ± 6.8 |
| 1.0 × 10−7 | 102.6 ± 4.2 | |||
| 5.0 × 10−7 | 100.9 ± 2.3 | |||
| Method | Sample type | Sample prep. technique | Extraction solvent type | LOD (ng mL−1) | RSD (%) | Enrichment factor | Lit. |
|---|---|---|---|---|---|---|---|
| a ETV: electrothermal vaporization; AAS: atomic absorption spectroscopy; SDME: single-drop microextraction; HS-SDME: headspace single-drop microextraction; APDC: ammonium pyrrolydine dithiocarbamate; SFODME: solidified floating organic drop microextraction; ETV-ICP-MS: electrothermal vaporization inductively coupled plasma mass spectrometry; CV-AAS: cold vapor atomic absorption spectroscopy; CV-AFS: cold vapor atomic fluorescence spectrometry; HPLC: high-performance liquid chromatography; UV-VIS: UV-visible spectroscopy; DLLME: dispersive liquid–liquid microextraction; ISFME: in situ solvent formation microextraction. | |||||||
| ETV-AAS | River water | SDME | m-Xylene | 0.01 | 6.1 | 970 | 1 |
| ETV-AAS | Water fish | HS-SDME | Thiourea, APDC | 5 | 3.3 | — | 2 |
| ETV-AAS | Mineral, tap water | SFODME | Undecanoic acid | 0.07 | 2.1 | 430 | 38 |
| ETV-ICP-MS | Water | SDME | Ionic liquid | 0.0098 | 5.2 | 50 | 34 |
| CV-AAS | Sea water | HS-SDME | Ionic liquid | 0.01 | 4.6 | 75 | 35 |
| CV-AFS | Human saliva | SFODME | Undecanol | 0.025 | 4.1 | 182 | 27 |
| HPLC | Tap, river, waste water | SDME | Ionic liquid | 22.8 | 11.6 | 3 | 36 |
| UV-VIS | Tap, river water | SDME | Carbon tetrachloride | 0.2 | 4.9 | 69 | 32 |
| UV-VIS | Water | DLLME | Ionic liquid | 3.9 | 1.7 | 18.8 | 39 |
| UV-VIS | Mineral, river, sea water | ISFME | Ionic liquid | 0.7 | 1.94 | 37 | 16 |
| UV-VIS | Drinking, river, sea water | DLLME | Carbon tetrachloride | 3.3 | 1.9–5.8 | 64 | 28 |
| UV-VIS | Saline samples | SDME | Undecanol | 1.9 | 8.5 | 203 | This work |
In comparison to these techniques, the method proposed in this study offers an inexpensive and rapid way for determining trace amounts of Hg(II) in various samples. Attention was paid to all saline samples including sea water, thermal spring and mineral water, rock and table salt, which can be complicated with other methods even those employing expensive and sophisticated instruments.
The method also has a potential to be exploited for field analysis by using a miniaturized photometer coupled with a compact extraction system with a greener solvent. The LOD level is well below the required limit8 and allows us to use the method for screening of pollutants in a number of environmental samples without the need of a sophisticated system. In comparison to other microextraction techniques,38,39 this method has the advantage of extracting in a microdrop which does not require time-consuming freezing and melting steps as is the case for SFODME. By using a multi-vessel extraction system, a set of 6 samples can be simultaneously analyzed in less than 30 min.
A standard 0.1 mol L−1 solution of Hg(II) ions was prepared in 0.1 mol L−1 HCl solution by dissolving a weighed portion of HgCl2 (Merck Darmstadt, Germany) immediately before use. Working standard solution of Hg(II) was prepared by appropriate dilution of the stock standard solution with 0.1 mol L−1 (pH 7.2) phosphate buffer solutions. Standard DTZ solution (7.5 × 10−4 mol L−1) was prepared daily by dissolving an appropriate amount of the reagent in ethanol. Universal BR buffer solutions were prepared by mixing equimolar (0.04 mol L−1) phosphoric, boric and acetic acid solutions and by dropwise addition of 0.2 mol L−1 NaOH to provide a wide range (2–10) of pH. Tin chloride reducing agent (3% w/v) was used in AFS studies. All standards and extracted samples were stored at 4 °C in the dark. All glassware was soaked in 10% nitric acid for at least 24 h before use and then rinsed with ultrapure water.
A Varian, Cary 100 Bio UV-Vis spectrophotometer with a matched Hellma ultra-micro tray cell was used for recording the UV-visible absorption spectra. A PSA 10.004 Merlin Plus atomic fluorescence spectrometer (Kent, UK) was used for the determination of mercury. Cold vapor AFS measurements were made with a PSA 10.004 (PS Analytical, Sevenoaks, Kent, UK), which consisted of a PSA 20.099 random access model auto-sampler, continuous-flow vapor generation system and a fluorescence detector. Automated continuous-flow vapor generation system (PSA 10.003) was used to generate gaseous mercury. The generated mercury was then detected by utilizing a 254 nm interference filter to achieve wavelength isolation and reduction of background scatter (Merlin, PSA 10.023). Wet gas from the gas–liquid separator was continuously dried by using a semi-permeable Nafion membrane dryer tube (Perma Pure Products, USA). The salinity of the water samples was calculated by measuring the conductivity using a Metler Toledo FG3 system.
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| Fig. 10 A laboratory-made extraction vessel for SDME consisting of a thermostatic glass cell connected to a circulating water bath. | ||
Iodized table salt, non-iodized table salt and rock salt samples were obtained commercially from a local market and 0.6000 g of the salt samples were weighed precisely. The same procedure as described above was applied to the salt samples except addition of NaCl. The resultant samples were then subjected to SDME and subsequently analyzed by UV-visible spectrophotometry.
Consequently, the method is appropriate for automation and can be adapted to portable systems for field analysis.
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