Open Access Article
Hunter B.
Andrews
*a,
Zachary
Murphy
c,
Mauro
Martinez
bf,
John
Lucchi
b,
Vasileios
Anagnostopoulos
c and
Matthieu
Baudelet
*bcde
aRadioisotope Science and Technology Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA. E-mail: andrewshb@ornl.gov
bNational Center for Forensic Science, University of Central Florida, Orlando, Florida, USA. E-mail: baudelet@ucf.edu
cChemistry Department, University of Central Florida, Orlando, Florida, USA
dCREOL—The College of Optics and Photonics, University of Central Florida, Orlando, Florida, USA
eAnthropology Department, University of Central Florida, Orlando, Florida, USA
fNow at Department of Environmental Medicine and Public Health, Icahn School of Medicine at Mount Sinai, New York, New York, USA
First published on 18th November 2025
Technetium (Tc) is a very important element that is encountered in many aspects, from its presence in radioactive waste and its potential environmental impact to its use as a medical radioisotope. Its detection and quantification in liquid samples is traditionally cumbersome, involving detailed sample preparation and analysis by mass spectrometry or scintillation. This article demonstrates the first comprehensive emission spectral analysis of Tc from a liquid sample by immobilization in a polymer and analysis by laser-induced breakdown spectroscopy (LIBS). A survey of LIBS spectra was completed to identify the strongest analytical lines for quantification of trace Tc in the presence of Mo. The quantification of Tc in a Mo-containing matrix was selected because Tc radioisotopes are the daughter products of Mo isotope decay. The first reported calibration curves by LIBS are provided with limits of detection and quantification down to 0.710 µg mL−1 and 1.39 µg mL−1, respectively. Ultimately, this study demonstrated the feasibility of trace Tc quantification using LIBS and will serve as a reference for future research related to monitoring this radioactive species.
The most abundant isotope of Tc, 99Tc, has a half-life of 2.13 × 105 years, and it is one of the most important radionuclides for assessing the safety of environmental radioactivity and radioactive waste management.6,7 When Tc is exposed to the atmosphere or any moderately oxidizing environment, it is found in the form of pertechnetate (TcO4−). Pertechnetate is highly soluble, does not sorb onto sediments, and migrates at the same velocity as groundwater.8 Under reducing conditions, Tc is found in the +4 valence state: it hydrolyzes in the presence of water but is encountered as sparingly soluble TcO2 in the absence of water.9 Furthermore, in the +4 oxidation state, Tc has been reported to complex with ligands such as carbonates, citrate, and natural organic matter.10–12
Because of its very low environmental concentration, the sample preparation, preconcentration, and chemical separation for removal of interferences are crucial steps for accurately determining 99Tc concentrations in environmental samples. Several methods have been used in the past to determine 99Tc in aqueous samples: gas flow with Geiger–Müller counter after anion exchange pretreatment in seawater,13 proportional counting after solvent extraction in radioactive waste,14 inductively coupled plasma mass spectrometry (ICP-MS) for water samples after solid-phase extraction,15–17 accelerated mass spectroscopy in seawater,18 and a sequential injection separation system in conjunction with liquid scintillation counting for tank waste samples.19 Thus, the goal of this study was to investigate the detection and quantification of trace 99Tc using laser-induced breakdown spectroscopy (LIBS) as an alternative analytical technique. LIBS is a powerful technique increasingly being applied in the nuclear field because of its versatility in application and sensitivity.20 LIBS has been investigated in many situations for in-field environmental sampling and is being developed as an online monitoring tool for MSRs and thus the potential quantification of Tc could be extended to these monitoring applications.21 Furthermore, LIBS requires minimal sample preparation compared with other analytical techniques.
LIBS is recognized as a rapid and sensitive technique that generally provides elemental analysis at levels of parts per million in most substrates.22 Although several studies have mentioned the potential application of LIBS to detecting Tc,23–25 Tc has not been extensively studied by LIBS, and most studies relied on using surrogate species. To the best of the authors' knowledge, only one previous literature study by Samek et al. reported three Tc LIBS emissions from a single 1000 µg mL−1 sample during the analysis of liquid samples.26 In this study by Samek et al. the detection limit of Tc was estimated to be 25 mg L−1 using a single point response.
Thus, this article provides a full demonstration of Tc emission spectroscopy by LIBS and its quantification at trace concentrations (i.e., <1000 µg mL−1) in an aqueous solution after immobilization in a polyvinyl alcohol (PVA) film. Additionally, the calibration system that was investigated included Mo at competing concentrations to examine the feasibility of monitoring Tc concentrations in a nuclear system containing the parent isotope Mo, such as an MSR. A comprehensive emission peak survey under concentrated and trace concentrations was performed to provide a knowledge base for future Tc LIBS studies.
| Nominal solution (µg mL−1) | Measured solution (µg mL−1) | Measured film (µg g−1) | |||
|---|---|---|---|---|---|
| Mo | Tc | Mo | Tc | Mo | Tc |
| 0 | 0 | — | — | — | — |
| 50 | 0 | 41.8 ± 0.2 | — | 2223.6 ± 217.3 | — |
| 0 | 50 | — | 54.79 ± 1.81 | — | 2288.0 ± 92.7 |
| 50 | 1 | 48.5 ± 2.8 | 1.42 ± 0.06 | 2461.7 ± 211.6 | 54.0 ± 4.2 |
| 50 | 5 | 49.0 ± 0.7 | 5.84 ± 0.21 | 2212.8 ± 110.3 | 232.7 ± 19.5 |
| 50 | 10 | 49.2 ± 2.7 | 11.53 ± 0.72 | 2335.1 ± 242.5 | 466.5 ± 17.3 |
| 50 | 25 | 46.9 ± 1.9 | 28.22 ± 1.23 | 2087.0 ± 177.7 | 1162.5 ± 58.7 |
| 50 | 50 | 48.6 ± 3.9 | 53.96 ± 2.06 | 2247.9 ± 106.9 | 2337.0 ± 93.1 |
| 50 | 100 | 48.8 ± 1.6 | 106.78 ± 2.86 | 2160.4 ± 159.4 | 4542.6 ± 169.4 |
An Ar background atmosphere (flow of 1 L min−1) was employed to avoid interaction with N and O in the air. The Tc and Mo in PVA films were analyzed to build calibration curves using a 100 µm spot size, accumulating spectra created while moving the sample at a speed of 1000 µm s−1 over a 5 mm line (e.g., 50 shots per line, no overlap between shots). In total, 30 lines were performed per sample. CZ spectrometer calibration spectra were collected with a grating with 2400 lines per millimeter. Data processing was performed using MATLAB (R2015a, MathWorks), Origin (2022 SR1, OriginLab Corporation), and Python 3.
| Ion | Wavelength (nm) | Relative intensity | A (108 s−1) | E low (eV) | E high (eV) | g low | g high |
|---|---|---|---|---|---|---|---|
| a Relative intensity is the background corrected intensity relative to the strongest Tc peak. | |||||||
| II | 254.32 | 1.00 | 4.10 | 0.000000 | 4.873618 | 7 | 9 |
| II | 260.99 | 0.88 | 3.80 | 0.000000 | 4.748942 | 7 | 7 |
| II | 264.70 | 0.59 | 3.70 | 0.000000 | 4.682537 | 7 | 5 |
| II | 321.20 | 0.38 | 1.90 | 1.564333 | 5.423234 | 5 | 5 |
| II | 323.70 | 0.53 | 1.90 | 1.564333 | 5.393432 | 5 | 7 |
| I | 363.61 | 0.91 | 1.57 | 0.318998 | 3.727869 | 10 | 12 |
| I | 371.89 | 0.51 | 1.05 | 0.403061 | 3.736048 | 8 | 10 |
| I | 403.16 | 0.88 | 1.01 | 0.318998 | 3.393421 | 10 | 10 |
| I | 426.22 | 0.52 | 0.40 | 0.000000 | 2.908075 | 6 | 6 |
| I | 429.70 | 0.76 | 0.42 | 0.000000 | 2.884532 | 6 | 8 |
![]() | ||
| Fig. 1 Identified strong emissions for Tc in trace conditions. Spectra for a blank sample and nominally 50 µg mL−1 Mo. Each subplot shows different wavelength windows from the same spectra. | ||
The strongest Tc emission peak is the singly-ionized peak at 254.32 nm. The two nearby Tc II peaks also exhibit strong emissions, scaling in accordance with their degeneracy-weighed transition probability (gA) factors. The two remaining Tc II emission lines provide weaker emissions and are in regions that have Mo emissions. As for Tc I lines, the 363.61 and 403.16 nm emissions are the strongest and are on par with the strongest ionized emissions. These strong lines may be preferred over Tc II lines for quantification because of the decreased effect of electron density and self-absorption on neutral emission lines. Although this emission survey was performed with the higher-sensitivity CZ spectrometer, these strong emissions were all observed in the broadband multichannel spectrometer, but the signal-to-noise levels were lower. This result has implications for monitoring Tc in less-tailored LIBS devices for online monitoring in nuclear applications.
The figures of merit for the multichannel calibration models for Tc peaks with >0.75 relative intensity (see Table 2) are detailed in Table 3. All peaks provided calibration curves with R2 > 0.99 and LODs < 10 µg mL−1. These figures of merit offer promise for monitoring Tc using a multichannel spectrometer to monitor nuclear streams, such as the effluent of an MSR. Most MSR LIBS work has focused on using multichannel spectrometers because of their reduced footprint, broadband coverage, and robustness for deployed systems.32 The calibration curve for 429.70 nm is shown in Fig. 2; the other multichannel spectrometer calibration plots are provided in the SI.
| Emission peak | Concentration range (µg mL−1) | R 2 | LOD (µg mL−1) | LOQ (µg mL−1) |
|---|---|---|---|---|
| 254.32 nm Tc II | <100 | 0.9940 | 5.97 | 11.9 |
| 260.99 nm Tc II | <100 | 0.9934 | 6.84 | 13.6 |
| 363.61 nm Tc I | <100 | 0.9937 | 6.88 | 13.5 |
| 403.16 nm Tc I | <100 | 0.9945 | 6.73 | 13.2 |
| 429.70 nm Tc I | <100 | 0.9983 | 4.45 | 8.80 |
![]() | ||
| Fig. 2 Tc calibration curve based on the 429.70 nm emission peak from the multichannel spectrometer. | ||
In addition to the broadband calibration, two spectral windows identified from the emission survey were selected for further investigation of Tc quantification using the CZ ICCD spectrometer. The first window, centered at 397 nm, contained several strong, neutral Tc peaks (398.49, 403.16, and 404.91 nm) without any interreferences from Mo. The second window, centered at 319 nm, contained weaker, singly ionized Tc peaks (319.52, 321.20, 323.70, and 328.20 nm), as well as an interference from the neutral 319.39 nm Mo I resonance peak. Portions of the collected spectral windows are shown in Fig. 3 as a function of Tc concentration.
The broadband spectra and CZ ICCD spectra were checked for correlated signals (outside of Mo or Tc) to identify a normalization technique, although none proved viable over a standard background correction. A calibration model was developed for each peak, along with the corresponding LOD and LOQ. A summary of these univariate calibrations is provided in Table 4.
| Emission peak | Concentration range (µg mL−1) | R 2 | LOD (µg mL−1) | LOQ (µg mL−1) |
|---|---|---|---|---|
| a Model developed using curve fitting. | ||||
| 398.49 nm Tc I | <100 | 0.9929 | 2.77 | 5.26 |
| 403.16 nm Tc I | <100 | 0.9986 | 0.710 | 1.39 |
| 404.91 nm Tc I | <100 | 0.9895 | 4.32 | 8.14 |
| a319.52 nm Tc II | <25 | 0.9828 | 6.51 | 12.7 |
| 321.20 nm Tc II | <25 | 0.9980 | 2.19 | 4.29 |
| 323.70 nm Tc II | <25 | 0.9982 | 2.10 | 4.12 |
| 328.20 nm Tc II | <25 | 0.9834 | 6.39 | 12.5 |
The univariate calibration model for the Tc I 403.16 nm emission proved to be the best. A plot of this model is shown in Fig. 4, highlighting its linearity across the concentration range. Because this peak has strong emission, detection in the range of parts per billion is possible with a LOD of 0.710 µg mL−1. This peak was also used for a multichannel spectrometer calibration; thus, the improvement in detection performance is estimated to be a factor of approximately 8.5 when using the ICCD-equipped spectrometer. The other neutral Tc peaks in this window also perform well, although with slightly reduced qualities of fit. Calibration model plots are provided for the remaining lines in the SI.
![]() | ||
| Fig. 4 Tc I 403.16 nm emission signal from LIBS collected using the CZ ICCD spectrometer as a function of Tc concentration. The error bars correspond to 2× standard error (n = 60). | ||
The ionized Tc emissions exhibited signs of self-absorption. This behavior is shown in Fig. 5, in which the emission area versus concentration trend bends from one linear regime to another reduced slope around 25 µg mL−1. Self-absorption is the result of emitted photons being absorbed by atoms within the plasma itself. As the concentration of the analyte grows, the number of atoms within the plasma capable of absorbing these photons grows in turn. This phenomenon is especially true early in the plasma lifetime, when ionized species are more dominant, which is why this behavior affects the singly ionized emissions and the neutral lines appear unaffected in this concentration range (i.e. 25–100 µg mL−1).22 Interestingly, this behavior is not shown in the ionized line calibrations using the multichannel spectrometer. This may be a result of the lower resolving power and/or the optical configuration of the broadband spectrometer, which uses a fiber bundle.
![]() | ||
| Fig. 5 Self-absorption behavior of the 323.70 nm Tc II emission peak collected on the CZ ICCD spectrometer versus concentration. Note that error bars correspond to 2× standard error (n = 60). | ||
This nonlinear behavior can be fit using second-order polynomials or using a log–log transformation with a linear fit. However, for this study, the detection and quantification at trace concentrations were the focus; therefore, only the lower linear regimes were fit to estimate the detection limits of singly ionized emissions. The figures of merit of these calibration models are provided in Table 3, and individual calibration plots are provided in the SI. The 323.70 nm Tc II line provides the best fit and detection limits for the ionized peaks that were examined. The other 321.20 nm ionized peak demonstrates detection capabilities similar to the neutral lines, albeit at a far-reduced concentration range.
The presence of Mo shown in the neutral Mo 319.39 nm emission significantly interfered with the singly ionized Tc emission peak at 319.52 nm. To develop a univariate model using this peak, separation of the two peaks was required. This separation was done by fitting two Voigt profiles to the known emission wavelength centers using the 50 µg mL−1 Mo and 100 µg mL−1 Tc sample spectra. The two fitted peaks, as well as their sum, are shown in Fig. 6a compared with the measured spectrum. These peaks were then scaled to each sample's spectrum using a least squares fit. The scaled fits for 319.52 nm Tc II were then integrated to form a calibration model similar to those previously described (Fig. 6b).
![]() | ||
| Fig. 6 (a) Peak fitting of Mo and Tc emissions at 319 nm and (b) corresponding calibration model. The error bars in (b) correspond to 2× standard error (n = 60). | ||
Again, the singly ionized emission showed self-absorption behavior, resulting in only concentrations nominally <25 µg mL−1 Tc being regressed to assess detection limits. As expected for an interfered peak, the fit was slightly weaker, with an R2 of 0.9828, and the detection limits were elevated to 6.51 µg mL−1 Tc. However, many scenarios with emission peaks will likely have interferences and the ability to detect Tc at low micrograms-per-milliliter levels through deconvolution, which is significant for the prospect of monitoring sample streams using LIBS.
Successful quantification of trace Tc in a Mo-containing matrix was achieved with both broadband and narrowband spectrometers, with LODs down to 0.710 µg mL−1 in aqueous samples. The presence of Mo is expected in reactor conditions when monitoring Tc concentrations and would act as a potential source of interfering peaks. Fortunately, in this study it was not detrimental for Tc analysis thanks to fitting of the emission peaks and the appropriate choice of spectral ranges for analysis and calibration models. However, further studies are needed on Tc determination in more complex matrices, such as geological and mineral samples to simulate environmental contamination and molten salt matrices.
Supplementary information (SI): a sample preparation schematic, additional calibration curves, and complete emission surveys. See DOI: https://doi.org/10.1039/d5ja00319a.
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