Changes in concentrations of potentially toxic elements during storage of hard river water samples at low temperatures using different sample preservation procedures
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Published:2023-08-23
Issue:12
Volume:23
Page:4173-4186
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ISSN:1439-0108
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Container-title:Journal of Soils and Sediments
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language:en
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Short-container-title:J Soils Sediments
Author:
Milačič RadmilaORCID, Marković Katarina, Marković Stefan, Ščančar Janez, Jolánkai Zsolt, Clement Adrienne, Musa Ildikó, Kardos Máté Krisztián, Zoboli Ottavia, Zessner Matthias
Abstract
Abstract
Purpose
According to standard procedure recommended by the Water Framework Directive (WFD), dissolved concentrations of potentially toxic elements (PTEs) in river water are determined by inductively coupled plasma mass spectrometry (ICP-MS) in filtered (0.45 µm) and acidified (pH 2) samples. Properly prepared and stored composite samples can enhance the temporal representativity of monitoring without increasing analytical costs. For this purpose, the WFD recommends freezing, which can preserve the species integrity and prevent adsorption processes of PTEs.
Methods
Low storage temperature in hard water samples can trigger precipitation of calcium carbonate (CaCO3) and subsequent co-precipitation of PTEs. To test and determine to what extent co-precipitation with CaCO3 can influence the determination of PTE concentrations, composite river water samples from two case study catchments in Hungary (Zagyva and Koppány) were prepared following two different sample preservation procedures. To study the behavior of PTEs in river water during storage, in the first procedure, samples were frozen, and they were thawed, filtered, and acidified directly prior to the analysis. In the second procedure, samples were filtered on-site and acidified prior to freezing to prevent precipitation of CaCO3 and then only thawed to carry out the chemical analyses. Concentrations of PTEs were determined by ICP-MS.
Results
A statistical evaluation of the results using Student’s t-test revealed significant differences between the two sample preservation procedures, suggesting that PTEs were largely co-precipitated with CaCO3 if the samples were not acidified prior to freezing.
Conclusion
When establishing protocols for sample preservation procedures, the phenomenon of co-precipitation of PTEs with CaCO3 should be considered if the samples were not acidified before freezing. Therefore, to prevent co-precipitation of PTEs with CaCO3, samples should be filtered and acidified before freezing.
Funder
Interreg Danube Transitional Programme Interreg Danube Transnational Programme Javna Agencija za Raziskovalno Dejavnost RS Széchenyi Plan Plus program
Publisher
Springer Science and Business Media LLC
Subject
Stratigraphy,Earth-Surface Processes
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