George A.
Zachariadis
*,
Aristidis N.
Anthemidis
,
Emmanouil I.
Daftsis†
and
John A.
Stratis
Laboratory of Analytical Chemistry, Department of Chemistry, Aristotle University, GR-54124, Thessaloniki, Greece. E-mail: zacharia@chem.auth.gr
First published on 25th November 2004
A novel non-chromatographic on-line cold vapour atomic absorption spectrometric (CV-AAS) method for sequential mercury speciation at the ng l−1 level was developed based on the selective retention of inorganic mercury on polytetrafluoro ethylene (PTFE) using a dual manifold. A column packed with PTFE turnings was used for inorganic mercury separation from the sample solution via the efficient retention on the sorbent material of the pyrrolidine dithiocarbamate complex Hg(PDC)2. On the other hand, the PDC complex of methylmercury (CH3HgPDC) is barely adsorbed, thus facilitating its direct determination after reduction by NaBH4 and subsequent on-line thermal dissociation of the resulting hydride. Inorganic mercury in the presence of methylmercury species is determined in a parallel manifold due to the fact that the later one cannot be reduced by SnCl2. The recovery of the proposed method was evaluated for drinking water, sea-water and urine samples.
Our previous research has proved the ability of PTFE turnings to act as a strong absorber of the pyrrolidine dithiocarbamate (PDC) complex of inorganic mercury.2 In contrast to inorganic mercury, we observed that the retention of the pyrrolidine dithiocarbamate complex of methylmercury is negligible, and to our knowledge, this discrimination has not been applied for mercury speciation purposes.
The aim of this work was to develop a novel on-line CVAAS method for mercury speciation based on the different retention times of the two species on the PTFE sorbent material.
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Fig. 1 FI on-line determination of mercury species by CVAAS; APDC, 0.05% m/v APDC solution; HCl, 1.5 mol l−1 HCl solution; R1, 3% m/v NaBH4 solution; R2, 2.5% m/v SnCl2 solution; WS, washing solution, 1.5 mol l−1 HCl; W, waste; SC separation column; P1, P2, P3 peristaltic pumps; IV1, IV2, injection valves; SV1, SV2, SV3, selection valves; GLS-1, GLS-2, gas–liquid separator/reactor; HT, electrically heated tube; AAC, atomic absorption cell. (a) Injection valves IV1 and IV2 in “A” position. (b) Injection valves IV1 and IV2 in “B” position. |
The FI on-line cold vapour generation dual manifold and its operation are shown schematically in Fig. 1. It consists of three peristaltic pumps (Watson-Marlow Model 205U/BA, Gilson Model Minipuls 3), two six-port two-position injection valves, IV1 and IV2 (Reodyne, USA) with a separation column (SC) on IV1, three eight-port selection valves, SV1, SV2 and SV3 (Valco, C252) and two integrated gas–liquid separators/reactors, GLS-1 and GLS-2. Tygon pumping tubes were used for aqueous solutions delivery.
The separation column (SC), 100 mm length, 4 mm id, which was packed with PTFE turnings (ca. 0.1 mm width, 1.3 g), was produced in our laboratory as described previously.2 The advantages of using PTFE turnings as packing material are the very good stability and resistance to strong chemicals and the excellent affinity for dithiocarbamate metal complexes, as is reported elsewhere.11 In addition the geometry of turnings allows high sample flow rates with low back pressure, facilitating the high sampling frequency.
The integrated gas–liquid separator/reactor (GLS), 100 mm length and 26 mm id, has been introduced and described previously.12 On the outlets of the two GLSs, a selection valve SV3 was elaborated to facilitate the sequential transportation of CH3HgH and Hg0 to the AAC through the HT. With this manifold the released volatile compounds were collected into the upper part of each GLS until SV3 is opened.
Step | Time/s | Valve positions | Pumps | Delivered mediuma | Flow rate/ml min−1 | Operation | ||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
IV1 | IV2 | SV1 | SV2 | SV3 | P1 | P2 | P3 | |||||
a In all steps except 3 and 4, the flow through cell is purged by N2 at 200 ml min−1 flow rate. b Two separate sample lines were used simultaneously with a flow rate of 12.0 ml min−1 in each one. | ||||||||||||
Sampleb | 12.0 | |||||||||||
1 | 50 | A | A | 1 | 1 | 3 | ON | OFF | OFF | APCD | 0.6 | Sample loading |
HCl | 1.2 | |||||||||||
2 | 10 | A | A | 2 | 2 | 3 | OFF | ON | OFF | NaBH4 | 4.8 | Reductant loading and reduction |
SnCl2 | 6.0 | |||||||||||
3 | 10 | A | A | 3 | 2 | 1 | OFF | OFF | OFF | N2 | 200 | Methyl mercury measurement |
4 | 10 | A | A | 4 | 3 | 2 | OFF | OFF | OFF | N2 | 200 | Inorganic mercury measurement |
5 | 30 | B | A | 4 | 4 | 3 | OFF | OFF | ON | HCl | 10 | Washing of column and GLS evacuation |
Waste | 24 | |||||||||||
6 | 10 | B | B | 4 | 4 | 3 | OFF | OFF | ON | H2O | 10 | HCl removing from column |
In step 1 (Fig. 1), sample and APDC streams were merged together towards the separation column (SC), where only Hg(PDC)2 complex could be retained. Thus, the GLS-1 was filled with a solution containing only CH3Hg(PDC). In the same time an equal sample volume was pumped directly into the GLS-2. Meanwhile, the heated tube (HT) and the atomic absorption cell (AAC) were purged by a continuous nitrogen stream. During step 2, NaBH4 and SnCl2 solutions were loaded to the GLS-1 and GLS-2, respectively, in order to reduce the two mercury species. During this step the outlets of the two GLSs were closed, thus resulting in the collection of CH3HgH and Hg0 in GLS-1 and GLS-2, respectively. In step 3 the generated (in GLS-1) methylmercury hydride vapour was separated from the liquid mixture and transported to the AAC through HT by the stream of N2. In the HT the hydride was thermally dissociated to elemental mercury vapour. During this step the absorbance of methylmercury was measured. In step 4, SV3 was turned to position “2” and the released mercury vapour in GLS-2 was transported to AAC and the absorbance measured.
According to the above observation, a determination of the two mercury species using SnCl2 as the selective reductant for Hg2+ in the presence of CH3Hg+ and NaBH4 for CH3Hg+ after a preceding separation of Hg2+ is feasible. In order to minimize the time for the determination of the two species and to avoid problems of subsequent use of the two reductant solutions in the same manifold, a simultaneous determination using a dual manifold was preferred, as is described above (Fig. 1, Table 1). Preliminary experiments showed that it is more convenient to liberate and measure the methylmercury hydride first, in order to avoid a pressure increase due to the produced nascent hydrogen and the subsequent restriction to mercury vapour evolution.
Another point to mention is the formation of volatile hydride CH3HgH from the reduction of the CH3Hg(PDC) by NaBH4 in acidic medium instead of atomic mercury vapour, which is produced from the reduction of Hg(PDC)2 by SnCl2. For this reason, in order to measure methylmercury species a thermal decomposition of the CH3HgH is necessary. 5 The decomposition/atomization temperature was studied and the minimum temperature for efficient atomization of the methylmercury hydride was found to be in the range 650–700 °C, thus 700 °C was adopted for further study. At this temperature, no significant decrease in the sensitivity of inorganic mercury determination was observed. Finally, with the proposed speciation procedure, the use of strong acids or volatile organic solvents for analyte elution before the reduction is avoided and an extra oxidation step is not necessary.
The optimum pH range for Hg(PDC)2 formation was between 2.0 and 3.1. Thus, the effect of the sample pH on the retention of CH3Hg(PDC) complex was studied just in the range between 2.0–3.1. At this range the retention of methylmercury was less than 4–7%, consequently the sample pH was adjusted to 2.5. A 0.05% m/v APDC solution was used throughout, in order to ensure complete retention in case of the presence of other metals.
According to previous work2 a 12.0 ml min−1 sample flow rate was selected for the separation of CH3Hg+ in the GLS-1 for high sensitivity and sufficient sampling frequency. The same sample flow rate was used for sample loading in the GLS-2.
The effect of the NaBH4 concentration was investigated in the range 0.3–3.0% m/v and maximum signal was obtained at 3% m/v NaBH4. A volume of 0.8 ml of NaBH4 was adequate for a 10 ml sample as was proved in a preliminary experiment. Thus, a 4.8 ml min−1 NaBH4 flow rate for 10 s was adopted. The flow rate of SnCl2 was fixed at 6.0 ml min−1 for 10 s in order to introduce 1 ml, which is a sufficient volume for the reduction.
Parameter | Hg2+ | CH3Hg+ |
---|---|---|
Sample volume | 10 ml | 10 ml |
Sampling frequency | 30 h−1 | 30 h−1 |
Linear range | 0.07–5.0 μg l−1 | 0.12–7.0 μg l−1 |
Regression equation ([Hg] in μg l−1) | 0.0392[Hg2+] + 0.0037 | 0.0183[CH3Hg+] + 0.0002 |
Correlation coefficient (r) | 0.9996 | 0.9993 |
Detection limit (cL) | 0.04 μg l−1 | 0.08 μg l−1 |
Precision (sr, n = 10, 1.5 μg l−1) | 2.7% | 7.1% |
The linear range of inorganic mercury is not limited by the presence of methylmercury because the latter cannot be reduced by SnCl2. However, the linear range of methylmercury is practically not affected in the presence of inorganic mercury up to 2 μg l−1 concentration levels. At a higher concentration of Hg2+ the retention of inorganic mercury in the PTFE column is not quantitative, so the samples should be diluted at the expense of methylmercury sensitivity. The determination of inorganic mercury species by SnCl2 as reducing agent is not affected by the presence of Zn2+, Cu2+, Co2+, Fe2+, Fe3+, Cr3+ and Al3+ up to 5 mg l−1. On the other hand, if an ion affects the complexation and retention of inorganic mercury, it may also affect the determination of CH3Hg+ species. It was found that concentrations up to 2 mg l−1 of Zn2+, Cu2+, Co2+, Fe2+, Fe3+, Cr3+ and Al3+ did not produce significant interference.
Added/μg l−1 | Found/μg l−1a | |||
---|---|---|---|---|
Sample | Hg2+ | CH3Hg+ | [Hg2+] ± s | [CH3Hg+] ± s |
a Mean ± s based on five replicates. | ||||
Drinking water | ||||
0.00 | 0.00 | <0.04 | <0.08 | |
1.50 | 1.50 | 1.44 ± 0.09 | 1.58 ± 0.14 | |
1.00 | 2.00 | 1.03 ± 0.05 | 1.84 ± 0.15 | |
Sea-water | ||||
Coastal sea-water I | 0.00 | 2.00 | <0.04 | 2.05 ± 0.21 |
2.00 | 0.00 | 2.16 ± 0.09 | <0.08 | |
2.00 | 2.00 | 2.10 ± 0.11 | 1.97 ± 0.18 | |
2.00 | 5.00 | 2.12 ± 0.11 | 4.81 ± 0.48 | |
Coastal sea-water II | 0.00 | 0.00 | 0.05 | <0.08 |
Estuarine water | 0.00 | 0.00 | 0.09 ± 0.01 | <0.08 |
Human urine | ||||
Sample A | 0.00 | 2.00 | 0.10 ± 0.01 | 2.25 ± 0.20 |
2.00 | 0.00 | 1.99 ± 0.12 | <0.08 | |
2.00 | 2.00 | 2.10 ± 0.08 | 2.28 ± 0.23 | |
2.00 | 5.00 | 2.05 ± 0.10 | 4.72 ± 0.42 | |
Sample B | 0.00 | 0.00 | 0.22 ± 0.03 | <0.08 |
Footnote |
† Part of his PhD Thesis. |
This journal is © The Royal Society of Chemistry 2005 |