Lyndsey
Hendriks
*a,
Robert
Brünjes
b,
Sara
Taskula
b,
Jovana
Kocic‡
c,
Bodo
Hattendorf
c,
Garret
Bland§
d,
Gregory
Lowry
d,
Eduardo
Bolea-Fernandez¶
e,
Frank
Vanhaecke
e,
Jingjing
Wang
f,
Mohammed
Baalousha
f,
Marcus
von der Au
g,
Björn
Meermann
g,
Timothy Ronald
Holbrook||
h,
Stephan
Wagner**
h,
Stasia
Harycki
i,
Alexander
Gundlach-Graham
i and
Frank
von der Kammer
*b
aTOFWERK AG, Thun, Switzerland. E-mail: lyndsey.hendriks@tofwerk.com
bDepartment of Environmental Geosciences, University of Vienna, Vienna, Austria. E-mail: frank.kammer@univie.ac.at
cSwiss Federal Institute of Technology (ETH), Zurich, Switzerland
dCarnegie Mellon University (CMU), Pittsburgh, USA
eGhent University, Department of Chemistry, Atomic & Mass Spectrometry – A&MS research group, Ghent, Belgium
fUniversity of South Carolina (USC), Columbia, USA
gFederal Institute for Materials Research and Testing (BAM) – Division 1.1 – Inorganic Trace Analysis, Berlin, Germany
hHelmholtz-Centre for Environmental Research (UFZ), Leipzig-Halle, Germany
iIowa State University (ISU), Ames, USA
First published on 16th June 2023
This study describes an interlaboratory comparison (ILC) among nine (9) laboratories to evaluate and validate the standard operation procedure (SOP) for single-particle (sp) ICP-TOFMS developed within the context of the Horizon 2020 project ACEnano. The ILC was based on the characterization of two different Pt nanoparticle (NP) suspensions in terms of particle mass, particle number concentration, and isotopic composition. The two Pt NP suspensions were measured using icpTOF instruments (TOFWERK AG, Switzerland). Two Pt NP samples were characterized and mass equivalent spherical sizes (MESSs) of 40.4 ± 7 nm and 58.8 ± 8 nm were obtained, respectively. MESSs showed <16% relative standard deviation (RSD) among all participating labs and <4% RSD after exclusion of the two outliers. A good agreement was achieved between the different participating laboratories regarding particle mass, but the particle number concentration results were more scattered, with <53% RSD among all laboratories, which is consistent with results from previous ILC studies conducted using ICP-MS instrumentation equipped with a sequential mass spectrometer. Additionally, the capabilities of sp-ICP-TOFMS to determine masses on a particle basis are discussed with respect to the potential for particle density determination. Finally, because quasi-simultaneous multi-isotope and multi-element determinations are a strength of ICP-TOFMS instrumentation, the precision and trueness of isotope ratio determinations were assessed. The average of 1000 measured particles yielded a precision of below ±1% for intensity ratios of the most abundant Pt isotopes, i.e.194Pt and 195Pt, while the accuracy of isotope ratios with the lower abundant isotopes was limited by counting statistics.
Inductively coupled plasma mass spectrometry (ICP-MS) is a well-established analytical technique for multi-element analysis with high sensitivity and precision, and its potential for single-particle analysis was initially outlined in 2003 by Degueldre et al.3 Subsequently, a rapid development of the technique, with improved hardware and dedicated software, took place, leading to a continuously growing number of publications in the field.4–6
Today, single-particle ICP-MS (sp-ICP-MS) is a widely accepted technique within the scientific community and is routinely applied for the determination of particle size and number concentration of metallic and metal–oxide NPs in various sample types.7 The methodology has already been validated through several interlaboratory comparisons (ILC) using ICP-MS instrumentation equipped with a quadrupole-based (QMS) or sector-field (SFMS) mass spectrometer.8–10 However, in spite of their successful use in many routine applications, the information attainable by sequential scanning-based ICP-MS instrumentation still remains limited for NP analysis. The ion cloud produced by a nanoparticle gives rise to a short transient event with a duration of approximately 200–1000 μs;11,12 and despite the development of sp-ICP-QMS and -SFMS with dwell time <1 ms for monitoring of these fast transient signals, sequential mass analysers can only be used to monitor signals from one or a maximum of two nuclides with different mass-to-charge (m/z) ratios.13 Even in these multi-m/z approaches, a short time delay is required for ion clearance after m/z-switching, and so a fraction of the signal is unavoidably lost, which results in only partial detection of two or more nuclides per particle transient event. Subsequently, the observation of only an unknown fraction of a particle event per nuclide hampers accurate quantification.
Although this fast-switching dual-element method is a non-negligible step in the direction of multi-element sp-ICP-MS, the measurement of only one or two nuclide types per NP event is not sufficient for many applications, ranging from NPs analysis in the environment, to nanotoxicology studies, to biological and medical applications, to NP characterization in material sciences, to forensics. As an example, the determination of the intrinsic elemental “fingerprint” of NPs allows one to answer the question of whether the NPs detected are of natural or anthropogenic origin.14–16 Comparatively, for nanotoxicology studies, in which cells are exposed to NPs and their uptake is investigated, multi-element information is required to shed some light onto possible assimilation mechanisms.17 For forensics and geochronology questions, the elemental and isotopic signatures contained in the individual NPs could provide key information regarding their origin and (trans-)formation.18 The common denominator in all previous applications relies on fast and simultaneous multi-element detection. While multi-element detection is possible with single-collector instruments, a long analysis time is required to repeatedly determine all nuclides of interest and address a sufficient number of NP events for reliable statistics. Furthermore, this approach provides an averaged multi-element composition for ensembles only, and not a multi-element composition on an individual particle basis.19 Multi-collector (MC) ICP-MS instruments with Nier–Johnson geometry and an array of ion counting detectors allow for simultaneous multi-element data collection but only within a limited m/z range. The number of analytes that are recordable in the specific mass range is limited to 9–15 isotopes depending on the number of collectors on the instrument.20 Wider m/z ranges can principally be acquired using Mattauch–Herzog type MC-ICPMS21 but our experience with the only commercial instrument currently available indicates that the signal/noise of the Faraday-strip-based detection system prevents the acquisition of low intensity, short signals from individual NPs.
Consequently, in order to gain a more comprehensive picture, not only is simultaneous and full multi-element detection required, but this should take place on an individual particle basis.
A fundamental solution to surmount the shortcomings of scanning-type mass analysers is the use of (quasi-)simultaneous full-spectrum mass analysers, such as a time-of-flight mass spectrometer22,23 (TOFMS). With its high-speed mass spectral acquisition and simultaneous monitoring of all nuclides, ICP-TOFMS is a game-changing technology in terms of the use of ICP-MS in multi-element single-particle analysis.4,24,25 While the lead in sp-ICP-MS taken by QMS and SFMS instruments can be explained by the initial limited sensitivity of ICP-TOFMS instruments, current designs have improved significantly and now provide sensitivities comparable to QMS instruments.23,26 The same fundamental principles described elsewhere4 apply to single-particle experiments with ICP-TOFMS, in which a dilute suspension of NPs is introduced into the plasma to generate individual ion clouds. The difference here, as opposed to sequential mass analysers, is that the full composition of each ion cloud is measured, providing multi-elemental composition information for every individual particle. Thanks to the fast and simultaneous detection capabilities of TOFMS instruments, the full elemental mass range (m/z 6 to m/z 238) can be recorded at time scales appropriate for single-particle analysis. This feature is particularly attractive for screening purposes of NPs mixtures, as a priori knowledge of the particle composition is not required and the complete elemental fingerprints of the different NPs types can be revealed. However, it should be noted that although sp-ICP-TOFMS holds great promise, it also brings about specific challenges, such as those regarding thresholding, data evaluation, and accurate multi-element NP detection. The underlying principle of multi-element particle analysis is that, if multiple mass-channels present coincident signals, these are assumed to stem from the same particle. However, although unlikely, these signals may originate from independent particles, which are reaching the plasma at the same time. Consequently, the particles will not be viewed as independent particles but instead as a multi-element particle. The probability of such events can be determined by coincidence analysis and limited using adequate dilution.25
The capabilities of sp-ICP-TOFMS have already been demonstrated through numerous different case studies, including multi-element NP characterization,26,27 distinguishing between naturally occurring (NNPs) and engineered nanoparticles (ENPs),16,28,29 analysis of surface water30–32 and wastewater samples,33 soil samples,34–36 gunshot residues,37,38 microplastics,39,40 as well as more exotic samples such as polar ice dust41 and space-station dust particles.42 While all these works highlighted the benefits of TOFMS for multi-element NP analysis, the sp-ICP-TOFMS methodology has not yet been validated. Hence, compared to previous ILCs, the ILC presented here aimed to assess the performance of sp-ICP-TOFMS for the characterization of Pt NPs, in terms of mass, size, and particle number concentration (PNC). An additional aim was to assess the precision and trueness of isotope ratio determination on a single-particle basis.
Nominal 50 nm Pt | Nominal 70 nm Pt | Nominal 100 nm Au | |
---|---|---|---|
Diameter ± STD (TEM) | 46 ± 4 nm | 70 ± 4 nm | 97 ± 11 nm |
Mass concentration | ∼0.05 mg mL−1 | ∼0.05 mg mL−1 | ∼0.05 mg mL−1 |
Particle concentration (calculated) | 4.6 × 1010 particles per mL | 1.3 × 1010 particles per mL | 5.7 × 109 particles per mL |
Particle surface | Bare (citrate) | Bare (citrate) | Bare (citrate) |
Solvent | 2 mM sodium citrate | 4 mM sodium citrate | 2 mM sodium citrate |
The NP workflow in the TOFpilot software, i.e. Single-Particle Analysis, includes experiment setup and subsequent data processing modules. Quantification is based on the method developed by Pace et al.46 using liquid standards for sensitivity calibration and the particle size method for the determination of the TE. The TOFpilot user interface facilitates the setup of a complete sequence, including blanks, ionic standards, NP standards, and NP samples, as well as data acquisition parameters such as integration time, measurement time, and dilution factor. At the end of the sequence, the data is automatically processed, and the experiment output is summarized in a pdf report, which includes detailed graphical results of the calibration curves and the relevant histograms (integrated signal intensity and mass distributions). The processed data is all saved in the form of csv-files for further post-processing. The SOP for this particular workflow is provided in the ESI.† A TOFpilot version of 2.8.8 or higher was recommended for data evaluation.
The major parameters to be reported were particle mass, Pt-isotope ratios, PNC, and particle size. While the first three parameters are determined from the raw data through data treatment in TOFpilot, the size and standard deviation were calculated individually by the participants. The mass can be converted into an equivalent spherical size assuming the density of the material is known (see eqn (1)):
![]() | (1) |
It should be noted here that based on the visual information provided by the TEM images, the Pt NPs under investigation are not solid spheres but aggregates of smaller Pt NPs. Thus, smaller sizes (respectively lighter masses) and higher PNC can be expected as opposed to the values stated by the manufacturer. In this regard a particle size determined by sp-ICP-MS should rather be considered as mass equivalent spherical size (MESS) than its microscopic appearance.
For the individual laboratory results, the individual average masses and standard deviations are reported and the overall mass average and SD of all nine laboratories have been taken as the apparent true values to calculate the individual laboratory z-scores according to eqn (2):
![]() | (2) |
Since no suitable standard reference material for a multi-isotope NP was available at the time, the correctness of the particle size and particle number concentration determination could not be assessed by comparison to the true value. Hence, the average of all participating laboratories was considered as the apparent true value, as long as the reported results were not scattered too much or did not show strong systematic deviations. Deviations from manufacturer values are also discussed.
For the isotope ratio precision, despite the lack of suitable reference material, the natural abundances of the different Pt isotopes can be used to calculate the true isotope ratios, with their abundance ratios to 195Pt spanning from 0.0004 to 0.9736. The relative abundances according to IUPAC and the IRMM-010 certified reference material are: 190Pt = 0.01289%, 192Pt = 0.7938%, 194Pt = 32.81%, 195Pt = 33.79%, 196Pt = 25.29% and 198Pt = 7.308%.48 Due to the low abundance of 190Pt, the measurement of its relative abundance was omitted and only the isotope ratios of 192Pt, 194Pt, 196Pt and 198Pt relative to 195Pt were requested from the participating laboratories in this study.
The results regarding particle mass and size, PNC, and isotope ratios are discussed separately in the following sections. The linearity of the method was not investigated specifically here, but has been addressed elsewhere and covers six orders of magnitude for dissolved ionic standards,23 and >4 orders of magnitude at the single-particle level, which translates to ∼1.5 orders of magnitude in terms of NP diameter.49 Additional parameters such as repeatability and robustness were not requested from the participants and therefore will not be discussed here.
It should be emphasized here that the size value delivered by the manufacturer was determined directly by TEM and DLS measurements, as opposed to sp-ICP-MS, which is not an imaging technique. In sp-ICP-MS, the counts produced by each NP are recorded and converted to mass using adequate calibration46 and subsequently to particle diameter (i.e. size), using two non-negligible assumptions. The first is that the NPs are of spherical shape, and the second is that the density of the NPs is equal to that of the bulk material (see eqn (1)). Consequently, the interpretation of the analytical results regarding a potential underestimation of the particle mass and size with respect to the expected values has two implications: (1) either the particles are porous, and thus the assumption that the density of the NPs is equal to that of the bulk material does not apply, or (2) the method under investigation, i.e. sp-ICP-TOFMS, is not suited for mass and size determination of Pt NPs.
To explain the systematic underestimation of the Pt NP sizes by sp-ICP-TOFMS as compared to the nominal values reported by the manufacturer, the apparent densities of the NPs were calculated by solving eqn (1) for ρ. The determined densities were 14.5 and 12.8 g cm−3 for the 50 and 70 nm NPs, respectively, as opposed to the bulk density of Pt (21.45 g m−3). While this may appear to be unlikely at first sight, seven out of nine laboratories reported size diameters within 0.5 SD of the average size. The two outlying laboratories reported values far above or far below the measured average (see Fig. 1). The reported values were consistently different from the nominal values, which were known to the operators, but consistent among the participating laboratories. Therefore, there is no indication of operator bias. It has been reported that while the density assumption has been shown to be reliable for NPs composed of gold, it may not apply for all other types of particles.4 For example, for silicon dioxide the density may range from 1.9 g cm−3 to 2.6 g cm−3 depending on its crystal structure. Previous ILCs have demonstrated that the true particle size can be calculated quite accurately from the mass determined via sp-ICP-MS.9,10 Furthermore, the relative mass concentrations reported in the isotope ratio analysis were exact to <1%, which would suggest that most of the calibrations in the lab were incorrect in the same direction and magnitude, which is very unlikely. Subsequently, the relative deviation from the nominal value should be similar for the 50 and 70 nm Pt NPs, which is not the case.
Further inspection of the TEM images from the manufacturer clearly showed that the Pt NPs under investigation were not solid, bulk-like materials but presented a rather porous character and appeared to be formed from agglomerates of smaller particles. Consequently, the actual density must be lower than that of the solid particle density, and lighter masses can be expected. The work of Sikder et al. further supports this observation as they synthesized Pt NPs of different sizes based on the agglomeration of smaller Pt NPs.50 Bolea-Fernandez et al. collected TEM images from the same type of particles (same manufacturer and size, different batch) and also concluded that in contrast to solid Ag and Au NPs these Pt particles are aggregates composed out of much smaller primary particles.51 Consequently based on previous work, the hypothesis of lower density has been verified and can be explained by physicochemical properties as the particles are formed from aggregates of smaller particles.
LAB no. | PNC nominal 50 nm NPs (particles per mL) | PNC nominal 70 nm NPs (particles per mL) |
---|---|---|
1 | 7.20 × 1010 | 1.50 × 1010 |
2 | 1.48 × 1010 | 9.54 × 109 |
3 | 7.70 × 1010 | 2.27 × 1010 |
4 | 5.62 × 1010 | 2.36 × 1010 |
5 | 3.13 × 1010 | 8.99 × 109 |
6 | 1.21 × 1010 | 8.68 × 109 |
7 | 4.67 × 1010 | 2.68 × 1010 |
8 | 2.59 × 105 | 2.68 × 105 |
9 | 5.75 × 1010 | 7.58 × 109 |
PNC mean | 4.60 × 1010 | 1.54 × 1010 |
PNC SD | 2.45 × 1010 | 7.86 × 109 |
PNC RSD | 53% | 51% |
PNC are typically underestimated in sp-ICP-MS, and this observation has several potential causes.52,53 A prime cause is particle loss due to the NPs sticking onto the walls of the sample vial and the walls of the sample introduction system. A second contributing factor is the settling of NPs over time, but no dynamic study was performed in this case to verify this phenomenon. The accuracy of the TE can be considered as a third parameter as this one will substantially influence the results. Indeed, by preparing ionic Au calibration solutions in MilliQ water rather than stabilizing them with HCl, a loss of ionic Au may be observed and lead to an apparent lower TE, which subsequently results in a PNC overestimation with a size underestimation. It should be noted that aged ionic standards may also impact the accuracy of the TE. Additionally, it cannot be excluded that the initial PNC was altered during the division into multiple aliquots. Last but not least, the reliability of the expected value is questionable. NP suspensions provided by commercial manufacturers such as NanoComposix are not characterized to the same extent as NIST materials, i.e., the NP size distributions are based on TEM measurement of roughly 100 NPs. The PNC is not measured by counting particles, but rather calculated based on the total mass concentration (g mL−1) and the average size determined by TEM, relying on the assumption that the NPs have the same density as the bulk material. However, as discussed previously, this last assumption is likely not valid. If this assumption were wrong, then the calculated average mass per particle would be incorrect as well as the “specified” PNC. These conclusions are consistent with results reported by Minelli et al.,52 where PNC determination was compared between population-averaging methods such as small angle X-ray scattering (SAXS), centrifugal liquid sedimentation (CLS) and ultraviolet-visible spectroscopy (UV-VIS) and particle-counting methods such as particle tracking analysis (PTA) and sp-ICP-MS. Results showed that PNCs determined by particle-counting methods, such as sp-ICP-MS, are more accurate than population-averaging methods, which are based on a theoretical model with various parameters requiring additional information (i.e., NPs morphology and density).
However, a closer look into the measured results revealed in some cases an overestimation of the PNC. As the expected value is determined from the mass concentration, the observed overestimation could be explained by a higher measured number of smaller particles or particles with a lower density, as previously discussed. While the TEM images provided by the manufacturer, suggest that the size appears correct, the particles show undefined edges with a “fluffy” character. Consequently, using the previously determined densities for both samples, namely 14.5 and 12.8 g cm−3, new PNCs were calculated resulting in values of 8 × 1010 and 2 × 1010 particles per mL.
In addition to the particle mass, size, and PNC, the participants were asked to report the isotope ratios relative to the most abundant isotope 195Pt (33.8%) for 4 different Pt isotopes. The results are presented in Table 3. While the results for the higher abundant isotopes 194Pt (32.8%) and 196Pt (25.3%) were reported by all laboratories for both particle sizes, the ratios involving the lower abundant isotopes 192Pt (0.8%) and 198Pt (7.3%) were not reported by all laboratories. Reporting of the single particle based SD values was not required according to the ILC data reporting template. Seven laboratories voluntarily provided SD data from which the RSD was calculated and reported (see Table 3). As no reference material was available for isotope ratio measurements, it was assumed here that the Pt used in the production of the NPs presents the same isotopic composition as that of the IRMM-010 standard and that the production of the NPs does not induce additional isotope fractionation.†† However, minor deviations in the isotopic composition from the IRMM-010 standard cannot be excluded, as already reported for environmental samples.60
Lab no. | 192Pt/195Pt | 194Pt/195Pt | 196Pt/195Pt | 198Pt/195Pt | ||||
---|---|---|---|---|---|---|---|---|
50 nm Pt | 70 nm Pt | 50 nm Pt | 70 nm Pt | 50 nm Pt | 70 nm Pt | 50 nm Pt | 70 nm Pt | |
1 | n.a | n.a | 48% | 29% | 51% | 29% | n.a | n.a |
2 | n.a | n.a | n.a | n.a | n.a | n.a | n.a | n.a |
3 | 53% | 30% | 28% | 23% | 30% | 16% | 37% | 29% |
4 | 55% | 38% | 37% | 19% | 39% | 21% | 44% | 32% |
5 | 75% | 41% | 44% | 27% | 48% | 31% | 53% | 44% |
6 | n.a | n.a | 43% | 22% | 46% | 24% | 47% | 34% |
7 | n.a | 46% | 43% | 21% | 41% | 21% | 57% | 31% |
8 | n.a | n.a | n.a | n.a | n.a | n.a | n.a | n.a |
9 | n.a | 37% | 42% | 24% | 42% | 26% | 47% | n.a |
Table 4 and Fig. 4 show the deviations of the different isotope ratios 194Pt/195Pt, 196Pt/195Pt and 198Pt/195Pt for the nominal 50 nm and 70 nm Pt NPs, in percent with respect to the corresponding values in the IRMM-010 reference material in a graphical manner. As per the instructions, a minimum of 1000 particles was recommended to be measured, hence the determined isotope ratios are based on the average of a minimum of 1000 particles. From the reported data, the isotope ratios were determined from ∼100 events for the 198Pt/195Pt and up to ∼4700 for the 194Pt/195Pt and showed good precision when averaged. Overall, the deviations of the measured isotope ratio for the higher abundant isotopes 194 and 196 are below ±1% and can be regarded as in excellent agreement considering that the ratios were determined on extremely short transient signals (below 1 ms) and a single isotope mass below 1 fg. Generally, results show more variations in the measured ratios with smaller particle size and lower relative abundance of the isotopes. These observations can be explained by the fact that smaller mass fractions in the particles produce signal intensities closer to the limits of detection, making them challenging for accurate quantification. Indeed at low count rates, the precision of the isotope ratio measurements is governed by counting statistics as illustrated in Fig. 5.29 Hence, as for spherical particles the mass scales with the third order of particle size, the precision of single particle determinations improves accordingly with increase of particle size: for the 50 nm NPs ratio RSDs between 28 and 48% were obtained for 194Pt/195Pt, which decreased to 19 to 29% for the 70 nm NPs. With this in mind, the poor results obtained for the less abundant isotopes 192Pt and 198Pt (between −0.83% and +252%) are expected to improve for larger particle sizes, namely from at least ∼100 nm for 198Pt and ∼200 nm for 192Pt.
![]() | ||
Fig. 5 Overview of the 194Pt/195Pt signal ratio from 70 nm Pt NPs with Poisson-Normal Confidence Bands (95% CI) demonstrating that the RSD is limited by counting statistics. |
Lab no. | 192Pt/195Pt | 194Pt/195Pt | 196Pt/195Pt | 198Pt/195Pt | ||||
---|---|---|---|---|---|---|---|---|
50 nm Pt | 70 nm Pt | 50 nm Pt | 70 nm Pt | 50 nm Pt | 70 nm Pt | 50 nm Pt | 70 nm Pt | |
1 | n.a | n.a | 38% | −0.71% | −29.0% | 0.09% | n.a | n.a |
2 | 9.85% | 67.0% | 0.02% | −0.40% | 0.22% | 0.22% | −1.70% | −2.16% |
3 | 471% | 119% | 1.46% | −0.40% | 1.56% | −0.71% | 11.6% | −6.29% |
4 | 495% | 205% | 0.20% | 0.53% | −0.77% | −1.06% | 33.9% | −5.79% |
5 | 676% | 180% | 0.89% | −0.12% | 0.30% | −1.21% | 29.1% | −8.48% |
6 | n.a | n.a | −1.06% | −0.76% | −0.44% | −0.43% | 49.0% | −0.83% |
7 | 252% | 252% | 2.39% | 1.36% | 1.42% | 2.76% | 1.06% | 5.65% |
8 | 493% | 104% | 0.64% | −0.30% | −0.31% | −0.58% | 31.4% | −2.62% |
9 | n.a | n.a | −0.77% | 0.46% | −2.25% | 4.04% | −4.11% | n.a |
Average | 385% | 162% | 4.64% | −0.04% | −3.25% | 0.35% | 18.8% | −2.93% |
Stand. dev. | 259% | 75.1% | 12.6% | 0.7% | 9.7% | 1.8% | 19.7% | 4.6% |
Recent work by Gundlach-Graham et al. have provided deeper insight and comprehension into the noise of ICP-TOFMS instrument, and have led to the development of new tailored thresholds for sp-ICP-TOFMS particle identification.64–67 Consequently, future improvements to the workflow include direct calculation of the MESSs and respective standard error, as well as the implementation of a tailored algorithm, such as the Compound Poisson Thresholding, for more robust particle detection.
Finally, because the data presented here demonstrate that sp-ICP-TOFMS can successfully be employed to determine both the NP mass and size, PNC and isotope ratios of constituent elements, it is our opinion that the developed SOP for sp-ICP-TOFMS using the particle workflow in TOFpilot has been validated and that the methodology of sp-ICP-TOFMS deserves its place in the analytical toolbox for NP analysis. This ILC also had the benefit of providing a platform to the participating laboratories to compare and benchmark their measurement capabilities.
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d3nr00435j |
‡ Current address: Lonza DPS, Basel, Switzerland. |
§ Current address: Department of Obstetrics, Gynecology and Reproductive Sciences, Program on Reproductive Health and the Environment, University of California San Francisco, San Francisco, California, USA. |
¶ Current address: University of Zaragoza, Aragón Institute of Engineering Research (I3A), Department of Analytical Chemistry, Pedro Cerbuna 12, 50009 Zaragoza, Spain. |
|| Current address: Friedrich-Schiller-Universität Jena, Institut für Physikalische Chemie, Jena, Germany. |
** Current address: Hochschule Fresenius gem. Trägergesellschaft mbH, Institute for Analytical Research, Germany. |
†† The validity of this assumption was confirmed by NanoComposix. |
This journal is © The Royal Society of Chemistry 2023 |