Hunter B. Andrews*a,
C. Derrick Quarles Jr
b,
Toya Beiswengerc,
Joseph Petrus
d,
Bence Paul
de and
Benjamin T. Manard
*f
aRadioisotope Science and Technology Division, Oak Ridge National Laboratory, USA. E-mail: andrewshb@ornl.gov
bElemental Scientific Inc., USA
cNuclear Nonproliferation Division, Oak Ridge National Laboratory, USA
dElemental Scientific Lasers, USA
eSchool of Geography, Earth and Atmospheric Sciences, The University of Melbourne, Parkville, Victoria, Australia
fChemical Sciences Division, Oak Ridge National Laboratory, USA. E-mail: manardbt@ornl.gov
First published on 10th March 2025
Laser-induced breakdown spectroscopy (LIBS) mapping enables rapid elemental and spatial analysis of solid samples. In this work, surrogate TRi-structural ISOtropic (TRISO) particles with various layers consisting of Zr, W, C, and Si were used to demonstrate the use of a new thickness measurement tool developed to analyze elemental images generated from LIBS maps. Zr particles with varying outer-layer thicknesses ranging from 16 to 32 μm were measured with scanning electron microscopy with energy dispersive spectroscopy (SEM-EDS) and LIBS with both a complementary metal-oxide-semiconductor (CMOS) detector and an intensified charged coupled device (ICCD) detector. LIBS maps of particles were completed using CMOS and ICCD spectrometers with effective spatial resolutions of 4 and 2 μm, respectively. The novel thickness measurement tool identified layer regions within a LIBS map and then identified the locations of the boundaries between these layers. The tool then generated up to 1000 random profiles stemming radially from the center region, which were used to measure the layer thickness/radius. This image analysis tool demonstrated LIBS's ability to provide values comparable with SEM-EDS (3.7% relative difference) along with a 95% reduction in measurement time. Furthermore, the precision of these measurements was on par with the SEM-EDS measurements at <15% relative standard deviation. Following the analysis of the Zr particles, W particles with increased complexity (e.g., five versus three layers) were analyzed using both the CMOS and ICCD spectrometers simultaneously. The spatial dimensions were extracted with an average relative difference of 2.7% and an average relative standard deviation of 9%.
In this study, we examine the use of LIBS and demonstrate a developed image analysis tool to extract spatial dimensions of surrogate advanced nuclear fuel particles. These TRi-structural ISOtropic (TRISO) particles are an advanced nuclear fuel designed with the core of the particle being the nuclear material (e.g., U) and several subsequent layers being used to contain any fission products and prevent damage to the nuclear material during any accident scenario.9,10 Additionally, because these particles are made to be accident tolerant, they can be difficult to characterize via bulk digestion methods, making laser ablation approaches ideal. The layers of these TRISO particles include both light and heavy elements (e.g., C and W) with each layer having various thicknesses. The thicknesses of these layers are critical to the role they play within the TRISO particles. With thousands of TRISO particles being loaded into a single fuel pebble, it is important to ensure that the production of these particles is consistent, necessitating rapid, high-throughput analysis.
A few potential techniques can be considered as analytical approaches to investigate these particles: X-ray fluorescence (XRF),11,12 scanning electron microscopy with energy dispersive spectroscopy (SEM-EDS),13–16 laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS),17–19 and LIBS.20,21 XRF has difficulties with light-element detection. Although SEM-EDS has the required sensitivity, it requires a vacuum environment and can be time-consuming for high-resolution mapping. LA-ICP-MS can provide fast, high-resolution mapping but may struggle with lighter elements and has large consumable costs. Lastly, LIBS offers full elemental sensitivity, can be performed rapidly at high resolutions, and can be located at manufacturing facilities for these particles. A previous study demonstrated the use of LIBS to extract the layer dimensions on surrogate TRISO particles from 2D maps in less than 5 min compared with 150 min line scans from an SEM-EDS measurement.20,21 Furthermore, with a known particle, standard layer thicknesses could be measured via depth profiling in less than 10 s.
The goal of this study is to expand upon the previous proof-of-concept study and demonstrate how high-resolution LIBS mapping capabilities combined with novel image analysis tools can enhance mapping capabilities for surrogate TRISO particles. TRISO particles manufactured with layers of varying thicknesses were analyzed using SEM-EDS and LIBS with a multichannel spectrometer using complementary metal-oxide-semiconductor (CMOS) detectors and a more sensitive spectrometer with an intensified charged coupled device (ICCD) detector. The collected data were used to construct 2D elemental maps and then analyzed using a developed novel image analysis tool to extract layer dimensions. The measurement accuracy, measurement precision, and measurement times were compared to demonstrate the true capabilities of the high-resolution LIBS mapping and image analysis tools for analyzing unknown layered particles.
All particles were mounted in epoxy, cross-sectioned, and polished to a 0.2 μm finish for SEM-EDS and LIBS analysis. Epoxy was poured in three steps, with at least 60 s of vacuum applied after each addition to minimize bubbles. The pucks were then inverted and backfilled with epoxy to fill gaps and ensure all particles were fully encased at the beginning of grinding. Grinding and polishing were accomplished with SiC paper (500, 800, then 1200 grit) and 5 mN of force to avoid potential cracking. After the tops of all cores were exposed, the sample was backfilled with epoxy again to fill gaps between the cores and subsequent layers to avoid cracking. Polishing was completed using a TriDent cloth and a 3 μm diamond suspension, followed by then with a ChemoMet polishing cloth and a 0.5 μm diamond suspension. Further specifics on this sample preparation can be found elsewhere.13 Note that slight deviations from the true midplane of the particle may lead to differences between layer dimensions and the nominal dimensions at the midplane. To account for this, all samples measured were compared with SEM-EDS measurements, which were treated as the expected dimensions.
All data visualization and analysis were performed in the iolite 4 data-processing platform (ESL).24 Briefly, the LIBS spectra were imported and baseline subtracted using a rolling-ball approach available within the iolite 4 software.25 Note, while the rolling-ball approach was sufficient for streamlined baseline correction, future quantification models should evaluate other correction approaches. The baseline-subtracted spectral peaks were then integrated to provide emission peak areas, which were mapped in iolite by correlating the spectra with x, y, z positions using the laser log file locations. All developed measurement tools were also integrated within the iolite 4 software.
![]() | (1) |
The precision of the measured values was evaluated based on their standard deviations (SDs). SD is a measure of how dispersed the data are in relation to the mean. All SDs described herein are two standard deviations (2SD). To facilitate comparison between different particles, the percent relative standard deviation (% RSD) was used:
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Lastly, to compare measurement methods with one another and consider both their mean values and their variance, zeta scores were used. A zeta score, ζ, indicates how far a value deviates from its expected value considering the combined uncertainties of the expected and measured values:
![]() | (3) |
If a zeta score is less than 1, then the difference between the values is less than one SD of the combined uncertainty. This indicates the measurements are consistent with one another. If the zeta score is between 1 and 2, then a slight discrepancy exists, but it is not significant when the combined uncertainty is considered. Although a zeta score between 2 and 3 indicates poor agreement between measurements. A zeta score greater than 3 indicates the values do not agree with one another even if their uncertainties are considered.
Images were created from collected LIBS measurements using typical workflows. Two measurement options were created: a manual measurement option, where the mouse is used to draw a line and the details of that line are reported (line option), and an automated layer thickness measurement tool (thickness option). The line tool reports the line's starting and ending x, y positions; the length, width, and height of the line; and the angle of the line (e.g., Fig. S1‡). The thickness tool provides a user interface for automated layer thickness measurements. The analyst can select which part of the image the algorithm should look for layers in, which is useful for images containing multiple particles. The user then selects which algorithm to use to find the layers and which LIBS signal the analysis should be based on.
In this study, the contours algorithm (scikit-image, find_contours) was used.14 Briefly, the algorithm takes a 2D array, and the user defines a threshold value (between 0 and 1). The threshold value is then scaled to the selected elemental signal (i.e., threshold of 0.5 would be halfway between the minimum and maximum value). The function searches for areas where the pixel values change from below to above the specified threshold value, denoting the presence of a boundary between layers. Note, this threshold value must be optimized for the measurement under consideration (see Section 3.2 for further information). These pixels are then traced together to form the contours that outline each region on the image. After the contours are calculated, a series of measurement profiles is placed on the image. The user can select the number of profiles to be drawn (1–1000) and the orientation of the profiles: horizontal, vertical, or drawn radially outward from the centroid of the innermost layer. If the latter is chosen, then each line begins at the median of the layers' centroids or the center of the inner layer for nonsymmetric particles. The lines then randomly radiate outward to the edge of the image. The distance between layer intersections with the line is then recorded for each line. The set of lines creates a series of measurements that can then be used to calculate layer statistics, such as median, minimum, and maximum thickness, along with the uncertainty (2SD) of the mean. An example of this calculation being applied to a Zr particle is shown in Fig. 1.
The number of profiles used in the thickness measurement tool was investigated prior to comparing the thicknesses determined with each measurement mode. The number of random profiles was varied from 5 to 1,000, with 10 replicates each, to compare the impact on the average uncertainty and the precision of the measured layer thickness. Fig. 2 shows the average % RSD of the thickness measurements and the precision of the mean thickness (n = 10 replicates) as a function of the number of profiles for all three layers. A few clear trends were identified. The greater the number of profiles used, the lower the uncertainty in the layer thickness and the higher the precision in the mean thickness. Logically, if too few profiles were used, then the tool would not fully capture the variance of the outer layer. Generally, the precision of the mean continued to decrease proportionally to the inverse of the square root of the number of profiles. This indicates that 1000 profiles should be used in the thickness measurement tool to obtain the most precise thickness measurements for these particles. Another interesting finding was that the % RSD values for all ICCD measurements were lower than their CMOS counterparts. This can likely be attributed to the better spatial resolution and sensitivity to boundaries between layers when mapping samples with the ICCD spectrometer. This effect was more pronounced for the core and intermediate PyC layer, but the thickness measurement of the outer layer relied on these inner dimensions, so this improvement may have compounded.
The CMOS measurements were made at 200 Hz with a 20 μm square spot and 16 μm overlap (i.e., an effective resolution of 4 μm). Overlap between ablation spots, also known as dosage, has been demonstrated to increase spatial resolution while maintaining a spot size large enough for effective LIBS signals.26 With an 80% overlap in both directions, the dosage for these CMOS measurements was 25 shots per spot. This provided a broadband elemental map in less time, with an individual particle being mapped in 6 min. However, this spectrometer was less sensitive than the ICCD as illustrated when comparing Fig. 3(b) and (d). The ICCD measurements were taken at 90 Hz with a 7 μm square spot and a 5 μm overlap (i.e., an effective resolution of 2 μm). The ICCD collection settings corresponded to a dosage of 12 shots per spot. It is important to note this spot size was not possible using the CMOS spectrometer given the decrease in emitted light from the smaller plasma. The use of the ICCD with the smaller ablation spot size generated maps with 50% higher spatial resolution than the CMOS maps and greater sensitivity at the interfaces between layers, although these measurements took 22 min per particle, a 267% increase in measurement time compared with the CMOS. To better understand the benefit of this time-resolution trade-off, the accuracies of the layer thicknesses determined from both measurement modes were compared. Note that both LIBS measurements saved significant time compared with SEM-EDS measurements, which took approximately 2 h per particle; the CMOS and ICCD reduced the measurement time by 95% and 81.7%, respectively, compared with SEM-EDS mapping. Given that this reduction in time is for a single particle, when multiple particles are considered the time savings would compound whereas the sample preparation time would remain constant for up to roughly 30 particles per mount.
The nine Zr particles were analyzed with SEM-EDS and then mapped with both the CMOS and ICCD collection configurations. The Zr elemental maps of selected particles using each technique are shown in Fig. 4. The strongest Zr emission peaks without spectral interferences were selected for each spectrometer (414 nm and 481 nm for the CMOS and ICCD, respectively). Weaker emission peaks provided similar maps; however, the layer interfaces were less sharp due to their reduced response. The sharpness in layer boundaries in the ICCD maps differed starkly from the CMOS results. This can be attributed to the increased sensitivity and higher spatial resolution. The ICCD maps more closely resembled the quality of the SEM-EDS maps; however, the CMOS maps still provided the spatial distribution needed to extract layer dimensions. Because these Zr particles differed in their outer-layer thicknesses, the following comparison of the measurements focuses on this outer layer. The measured thickness of the PyC layer and the measured core diameter agreed with the SEM-EDS values (55.5 ± 10.45 and 229 ± 58 μm, respectively) regardless of the measurement mode (see Tables S1 and S2‡). Note that because samples were cross-sectioned and mounted, the core and PyC layer dimensions were more subject to effects of not being at the true center plane of the sample; however, the outer ZrC layer was less affected given its distance from the center of the spherical particle.
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Fig. 4 SEM-EDS, CMOS, and ICCD maps of Zr distribution in ZrC particles with outer layers ranging from 16 to 32 μm. |
The ZrC layer dimensions were calculated using n = 1000 profiles. The threshold value used to fine-tune thickness measurement accuracy was varied between 0.2 and 0.45. Values outside this range did not result in proper contour mapping. The results for the thickness tool processing of the CMOS and ICCD measurements as a function of threshold value are shown in Fig. 5. Notably, the CMOS quantities varied more as a function of threshold value compared to the ICCD values. This was likely due to the differences in the spatial resolution and sensitivity of the ICCD spectrometer more sharply increasing the signal intensity at the layer interface. Despite this, the SEM-EDS values could be used to determine an optimal threshold value for each measurement mode. Thresholds of 0.4 and 0.25 were determined to provide the most accurate results for the CMOS and ICCD measurements, respectively. These thickness values are shown in Table 1.
Sample tag | ZrC layer thickness (μm) | Zeta score |ζ| | |||
---|---|---|---|---|---|
SEM-EDS (manual) | CMOS (tool) | ICCD (tool) | CMOS | ICCD | |
21 | 19.4 ± 2.1 | 17.8 ± 3.3 | 18.8 ± 2.8 | 0.41 | 0.18 |
35 | 16.11 ± 0.95 | 16.5 ± 3.3 | 16.4 ± 2.3 | 0.11 | 0.13 |
40 | 19.1 ± 2.4 | 19.8 ± 3.1 | 18.1 ± 2.4 | 0.18 | 0.29 |
41 | 20.2 ± 3.5 | 19.5 ± 3.3 | 19.6 ± 2.8 | 0.14 | 0.14 |
42 | 20.0 ± 2.6 | 20.2 ± 3.0 | 18.8 ± 2.5 | 0.07 | 0.34 |
43 | 22.6 ± 2.2 | 23.7 ± 3.1 | 22.2 ± 2.6 | 0.30 | 0.12 |
44 | 33.8 ± 3.3 | 34.7 ± 3.9 | 33.0 ± 2.9 | 0.17 | 0.20 |
45 | 31.0 ± 1.6 | 30.9 ± 3.3 | 30.7 ± 2.6 | 0.03 | 0.10 |
46 | 31.6 ± 4.9 | 33.7 ± 4.3 | 29.0 ± 3.0 | 0.33 | 0.45 |
Using these threshold values, the SEM-EDS, CMOS, and ICCD measurements were all in agreement with one another. The uncertainties of the provided thickness measurements were similar, with average % RSD values of 11.1%, 14.4%, and 12.1% for the SEM-EDS, CMOS, and ICCD approaches, respectively. The uncertainties for LIBS-based measurements (n = 1000) were likely limited based on the true variance of the deposited layer itself. Note that the thickness measurement tool eliminates user bias in the measurement of layers because all profiles randomly radiate from the center of the particle with much larger sampling statistics, whereas the manual SEM-EDS measurements rely on the user selecting measurement points. Furthermore, the average values for % RD between the SEM-EDS results and the CMOS and ICCD measurements were 3.7% and 5.3%, respectively. To better compare the measured values, the zeta scores were calculated. A zeta score with an absolute value less than 1 represents strong consistency between the anticipated value (SEM-EDS) and the experimental value (LIBS). Both the CMOS and ICCD results had zeta scores well below 1. Overall, the CMOS measurements are the preferred approach because their results are consistent with SEM-EDS while providing broadband elemental coverage at rapid testing rates.
The thickness measurement tool was used to extract the core radius and layer dimensions for each of these particles. Threshold values were toggled in a similar manner as in the Zr particle study until all layers converged about their SEM-EDS expected values. The core radius was determined using the Zr 414 nm CMOS data with a threshold of 0.6. The Si layer thickness was determined from the Si 251 nm CMOS data with a 0.6 threshold. The inner PyC layer could not be readily detected by the thickness tool because of its limited intensity; however, the difference between the internal radius of the Si layer and the previously calculated Zr core radius was used to infer the inner PyC layer thickness. The outer PyC layer dimensions were calculated with the C 247 nm CMOS data and a 0.4 threshold value. Lastly, the W 505 nm ICCD data were used to determine the thickness of the outer layer using a 0.5 threshold. All values were calculated using 1000 profiles. The thickness tool results are compared with SEM-EDS values in Table 2.
Particle | Layer radius/thickness (μm) | ||||
---|---|---|---|---|---|
Core | Inner PyCa | Si | Outer PyC | W | |
a LIBS inner PyC values were calculated from the differences between core radii and Si layer inner diameter values from the thickness tool. | |||||
W1 (SEM-EDS) | 201.1 ± 2.2 | 12.0 ± 2.5 | 37.7 ± 2.8 | 186 ± 33 | 47.6 ± 3.1 |
W1 (LIBS) | 204.7 ± 4.2 | 11.6 ± 5.2 | 36.7 ± 3.1 | 182 ± 32 | 49.1 ± 7.3 |
W2 (SEM-EDS) | 201.3 ± 3.0 | 12.0 ± 2.2 | 38.3 ± 2.6 | 191 ± 29 | 48.0 ± 4.5 |
W2 (LIBS) | 204.2 ± 5.1 | 11.7 ± 5.9 | 38.0 ± 2.9 | 195 ± 25 | 51.3 ± 5.9 |
W3 (SEM-EDS) | 199.9 ± 1.5 | 14.9 ± 2.3 | 38.1 ± 3.5 | 173 ± 15 | 47.8 ± 3.9 |
W3 (LIBS) | 203.2 ± 3.1 | 13.3 ± 4.0 | 38.4 ± 2.6 | 192 ± 25 | 49.1 ± 7.9 |
Avg (SEM-EDS) | 200.8 ± 1.2 | 13.0 ± 1.3 | 38.0 ± 1.7 | 183 ± 13 | 47.8 ± 2.1 |
Avg (LIBS) | 204.0 ± 2.2 | 12.2 ± 2.8 | 37.7 ± 1.6 | 189 ± 16 | 49.8 ± 4.0 |
Overall, the thickness tool – determined dimensions agreed with the values manually measured with SEM-EDS, with an average % RD of 2.7%. All zeta values for both individual particle layer thicknesses were in agreement (<1) between the methods. The average % RSD values for the LIBS measurements were below 10% for all layers except the inner PyC layer. This exception was due to the propagated uncertainty for the inner PyC, which was due to the inner PyC being calculated from the core and Si layer measurements. The largest differences between the SEM-EDS and LIBS values were in the two outermost layers. This can be attributed to the nonsymmetric shape of the outer PyC and W layers (Fig. 6). Using a greater number of profiles in the thickness tool likely leads to a more representative measurement of the variance of the PyC layer. Despite its nonsymmetric shape, the W layer appeared relatively uniform in thickness. The increased variance in the LIBS data may have been due to the profiles stemming from the center of the particle and not necessarily passing through the W layer perfectly perpendicularly to the interfaces. In terms of production monitoring, this measured variance may prove beneficial by aiding in diagnosing particle batches with large amounts of asymmetry.
The analysis of more complex surrogate TRISO particles further demonstrated the value of LIBS mapping with simultaneous CMOS and ICCD spectrometers. These W particles were mapped in 17 min, and the layer elemental compositions and spatial dimensions were extracted with an average % RD of 2.7% and an average % RSD of 9%. Because LIBS saves time compared with SEM-EDS, and because of the other characteristics of LIBS (e.g., fieldable, low capital and operational costs, wide elemental coverage), LIBS could be used for monitoring production batches on-site. This would enable rapid research and development on chemical vapor deposition effects on layer thicknesses (as demonstrated with the Zr particles) and permit quality assurance on existing procedures. For typical batches consisting of thousands of particles, rapid analysis would be necessary for quality control. Continued studies applying image analysis tools to LIBS mapping applications can further extend the applicability of LIBS over a range of solid-sample opportunities. Elemental quantification, although not a focus of this study, could also be readily implemented. The measurement of major and trace element compositions could be readily implemented within this workflow. Lastly, as research and development on TRISO fuel continues, the methods presented here can be used to analyze fuel after irradiation to examine layer performance and fission product distributions and could even be coupled with LA-ICP-MS for monitoring isotope ratios.
Footnotes |
† This manuscript has been authored in part by UT-Battelle, LLC, under contract DE-AC05-00OR22725 with the US Department of Energy (DOE). The US government retains and the publisher, by accepting the article for publication, acknowledges that the US government retains a nonexclusive, paid-up, irrevocable, worldwide license to publish or reproduce the published form of this manuscript, or allow others to do so, for US government purposes. DOE will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan (http://energy.gov/downloads/doe-public-access-plan). |
‡ Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4ja00471j |
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