| Literature DB >> 35956795 |
Dawid Kucharski1, Robert Stasiuk2, Przemysław Drzewicz3, Artur Skowronek4, Agnieszka Strzelecka4, Kamila Mianowicz5, Joanna Giebułtowicz1.
Abstract
Organotin compounds (OTCs) are among the most hazardous substances found in the marine environment and can be determined by either the ISO 23161 method based on extraction with non-polar organic solvents and gas chromatography analysis or by the recently developed QuEChERS method coupled to liquid chromatography-mass spectrometry (LC-MS/MS). To date, the QuEChERS LC/MS and ISO 23161 methods have not been compared in terms of their fit-for-purpose and reliability in the determination of OTCs in bottom sediments. In the case of ISO 23161, due to a large number of interferences gas chromatography-mass spectrometry was not suitable for the determination of OTCs contrary to more selective determination by gas chromatography with an atomic emission detector. Moreover, it has been found that the derivatization of OTCs to volatile compounds, which required prior gas chromatography determination, was strongly affected by the sediments' matrices. As a result, a large amount of reagent was needed for the complete derivatization of the compounds. Contrary to ISO 23161, the QuEChERS LC-MS/MS method did not require the derivatization of OTC and is less prone to interferences. Highly volatile and toxic solvents were not used in the QuEChERS LC-MS/MS method. This makes the method more environmentally friendly according to the principles of green analytical chemistry. QuEChERS LC-MS/MS is suitable for fast and reliable environmental monitoring of OTCs in bottom sediments from the Odra River estuary. However, determination of di- and monobutyltin by the QuEChERS LC-MS/MS method was not possible due to the constraints of the chromatographic system. Hence, further development of this method is needed for monitoring di- and monobutyltin in bottom sediments.Entities:
Keywords: Odra River estuary; bottom sediments; environmental monitoring; organotin compounds; trueness; verification
Mesh:
Substances:
Year: 2022 PMID: 35956795 PMCID: PMC9370016 DOI: 10.3390/molecules27154847
Source DB: PubMed Journal: Molecules ISSN: 1420-3049 Impact factor: 4.927
Figure 1Chromatograms of organotin compounds determined in BCR sediments by (A) QuEChERS coupled to LC-MS/MS (B) ISO 23161 GC-AED method. Determination of DBT and MBT was only possible using the method ISO 23161 GC-AED. Abbreviations: MBT, monobutyltin; DBT, dibutyltin; TBT, tributyltin; TPhT, triphenyltin.
Validation parameters of QuEChERS LC-MS/MS and ISO 23161 GC-AED methods for monobutyltin (MBT), dibutyltin (DBT), tributyltin (TBT), and triphenyltin (TPhT).
| Parameters | QuEChERS (LC-MS/MS) | ISO 23161 (GC-AED) |
|---|---|---|
| Limit of quantification (LOQ) | 2.0 ng·g−1 d.w. TBT | 1.7 ng·g−1 d.w. MBT |
| Limit of detection (LOD) | 0.6 ng·g−1 d.w. TBT | 0.5 ng·g−1 d.w. MBT |
| Analytical ranges (linearity) | 2.0–4000.0 ng·g−1 d.w.; | 1.7–4000.0 ng·g−1 d.w; |
| Accuracy ( | 98.0–105.0%-TBT | 80.0–85.0%-MBT |
| Precision ( | 3.0%-TBT | 27.0%-MBT |
| Recovery ( | 93%-TBT | 79%-MBT |
a acceptance criteria: 85–115%; b acceptance criteria: ≤15%
The results of (TBT), triphenyltin (TPhT), dibutyltin (DBT), and monobutyltin (MBT) determination in real sediments samples and reference material of freshwater sediment (BCR 646) by the use QuEChERS LC-MS/MS and ISO GC-AED methods. Certified values of BCR-646: TBT-480 ng·g−1 (±80 ng·g−1), TPhT-29 ng·g−1 (±11 ng·g−1), DBT-770 ng·g−1 (±90 ng·g−1), MBT-610 ng·g−1 (±120 ng·g−1).
| QuEChERS LC-MS/MS a | ISO GC-AED | |||||
|---|---|---|---|---|---|---|
| Sample | TBT | TPhT, | TBT, | TPhT, | DBT, | MBT, |
| S1 | 29.4 ± 1.1 | <5.0 | 19.0 ± 1.1 | <3.0 | <2.4 | <1.7 |
| S2 | 177.2 ± 11.2 | <5.0 | 137.8 ± 8.3 | <3.0 | 23.4 ± 3.5 | <1.7 |
| S3 | 453.2 ± 7.4 | <5.0 | 589.1 ± 35.4 | <3.0 | 62.3 ± 9.4 | 23.9 ± 6.5 |
| S4 | 261.3 ± 12.6 | <5.0 | 291.3 ± 17.5 | <3.0 | 522.4 ± 78.4 | 177.5 ± 47.9 |
| S5 | 165.9 ± 19.3 | <5.0 | 185.4 ± 11.1 | <3.0 | 17.3 ± 2.6 | 52.3 ± 14.1 |
| S6 | 483.4 ± 11.5 | <5.0 | 573.9 ± 34.4 | <3.0 | 137.4 ± 20.6 | 19.6 ± 5.3 |
| S7 | 464.5 ± 22.7 | 15.1 ± 0.3 | 391.2 ± 23.5 | 11.0 ± 0.2 | 73.8 ± 11.1 | 46.2 ± 12.5 |
| S8 | 1667.5 ± 57.8 | 21.9 ± 0.6 | 1862.5 ± 111.8 | 29.9 ± 0.6 | 231.6 ± 34.8 | 156.7 ± 42.3 |
| S9 | 118.1 ± 4.0 | <5.0 | 97.8 ± 5.9 | <3.0 | 58.6 ± 8.8 | 99.6 ± 26.9 |
| S10 | 631.1 ± 24.6 | <5.0 | 743.4 ± 44.6 | <3.0 | <2.4 | <1.7 |
| BCR a | 484.2 ± 14.4 | 29.6 ± 1.4 | 432 ± 6.1 | 27.8 ± 1.8 | 698.0 ± 14.2 | 483.8 ± 24.7 |
a the analyses of BCR were replicated six times.
Figure 2Difference vs. mean value for tributyltin determination in real sediments samples and BCR 464 freshwater sediment. The cumulative %ISR for 11 samples was 72.7% and met acceptance criteria (≥67%) for comparability of the analytical methods tested.
Geographic coordinates, depth of sampling from the water surface, and localization name of sediments collected from the Odra River estuary.
| Sample | Geographic Coordinates | Depth of Sampling from the Surface (m) | Localization | |
|---|---|---|---|---|
| Latitude N | Longitude E | |||
| S1 | 53°51.209′ | 014°18.107′ | 1.5 | Karsibór next to Rybaczówka |
| S2 | 53°59.570′ | 014°42.332′ | 2.1 | West Dziwna River |
| S3 | 53°41.456′ | 014°25.297′ | 4.4 | Szczecin Lagoon-Brzózki |
| S4 | 53°38.538′ | 014°35.958′ | 3.5 | Roztoka Odrzańska-near to Stępnicka Bay |
| S5 | 53°33.572′ | 014°34.774′ | 1.8 | Police-Larpia |
| S6 | 53°27.621′ | 014°36.102′ | 2.2 | Sailing Canal, near Święta |
| S7 | 53°27.336′ | 014°35.434′ | 2.5 | West Odra River-Gryfia Shipyard Dock No. 5 |
| S8 | 53°27.328′ | 014°35.968′ | 2.2 | Szczecin: opposite Gryfia Island |
| S9 | 53°26.300′ | 014°35.280′ | 10.3 | Elevator “Ewa” |
| S10 | 53°23.827′ | 014°38.205′ | 3.6 | Dąbie Marina |