Recent progress and applications of thermal lens spectrometry and photothermal beam deflection techniques in environmental sensing

This paper presents recent development and applications of thermal lens microscopy (TLM) and beam deflection spectrometry (BDS) for the analysis of water samples and sea ice. Coupling of TLM detection to a microfluidic system for flow injection analysis (µFIA) enables the detection of microcystin-LR...

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Bibliographic Details
Published in:Sensors
Main Authors: Franko, Mladen, Goljat, Leja, Liu, Mingqiang, Budasheva, Hanna, Žorž, Mojca, Korte, Dorota
Format: Other/Unknown Material
Language:English
Published: MDPI 2023
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Online Access:https://repozitorij.ung.si/IzpisGradiva.php?id=7822
https://repozitorij.ung.si/Dokument.php?id=25276&dn=
https://repozitorij.ung.si/Dokument.php?id=27637&dn=
https://plus.cobiss.net/cobiss/si/sl/bib/135854851
https://hdl.handle.net/20.500.12556/RUNG-7822-a30dee95-b0ce-a65b-e51f-d06888628e7a
Description
Summary:This paper presents recent development and applications of thermal lens microscopy (TLM) and beam deflection spectrometry (BDS) for the analysis of water samples and sea ice. Coupling of TLM detection to a microfluidic system for flow injection analysis (µFIA) enables the detection of microcystin-LR in waters with a four samples/min throughput (in triplicate injections) and provides an LOD of 0.08 µg/L which is 12-times lower than the MCL for microcystin-LR in water. µFIA-TLM was also applied for the determination of total Fe and Fe(II) in 3 µL samples of synthetic cloudwater. The LODs were found to be 100 nM for Fe(II) and 70 nM for total Fe. The application of µFIA-TLM for the determination of ammonium in water resulted in an LOD of 2.3 µM for injection of a 5 µL sample and TLM detection in a 100 µm deep microfluidic channel. For the determination of iron species in sea ice, the BDS was coupled to a diffusive gradient in the thin film technique (DGT). The 2D distribution of Fe(II) and total Fe on DGT gels provided by the BDS (LOD of 50 nM) reflected the distribution of Fe species in sea ice put in contact with DGT gels.