Evaluation of the Homogeneity of the Uranium Isotope Composition of NIST SRM 610/611 by MC-ICP-MS, MC-TIMS, and SIMS

Abstract

As analytical and microanalytical applications employing uranium isotope ratios increase, so does the need for reliable reference materials, particularly in the fields of geochemistry, geochronology, and nuclear forensics. We present working values for uranium isotopic data of NIST 610/611 glass, collected by multicollector inductively-coupled plasma mass spectrometry (MC-ICP-MS), multicollector thermal ionization mass spectrometry (MC-TIMS), and secondary ion mass spectrometry (SIMS). The presence of depleted U, and, in this case, measureable ²³⁶U, makes NIST 610/611 an ideal candidate for a uranium isotopic reference material for nuclear materials. We analyzed multiple chips of three different NIST 611 wafers and found no heterogeneity in ²³⁴U/²³⁸U, ²³⁵U/²³⁸U, and ²³⁶U/²³⁸U within or between the wafers, within analytical uncertainty. We determined working values and uncertainties (using a coverage factor of two) using data from this study and the literature for the following U isotope ratios: ²³⁴U/²³⁸U = 9.45 × 10⁻⁶ ± 5.0 × 10⁻⁸; ²³⁵U/²³⁸U = 2.38555 × 10⁻³ ± 4.7 × 10⁻⁷; and ²³⁶U/²³⁸U = 4.314 × 10⁻⁵ ± 4.0 × 10⁻⁸. SIMS data show ²³⁵U/²³⁸U is reproducible to within 1% (within analytical uncertainty) in a single wafer, at a scale of 25 μm. Multiple studies have demonstrated homogeneity between wafers of NIST 610 and NIST 611, thus the data reported here can be considered representative of NIST 610 as well.

1. Introduction

Uranium isotope ratios are useful signatures in U series geochemistry [1,2,3], radiochronometry/geochronology [4,5], nuclear forensics and nuclear nonproliferation studies [6,7]. Microanalytical techniques including secondary ion mass spectrometry (SIMS) and laser ablation inductively-coupled mass spectrometry (LA-ICP-MS) have made high precision, spatially resolved analysis of U isotope ratios possible, which has yielded new insights into complex materials [8,9,10,11]. For example, the isotopes of U in glassy fallout debris from a historical nuclear test have been shown to be heterogeneously distributed [12,13]. This spatially-resolved data may provide valuable information missed via bulk analysis methods. Expanded use of microbeam isotope ratio measurement techniques has highlighted a growing need for homogenous and well-characterized uranium isotope microbeam standards [10,14]. The NIST SRM 600 series of glass standards were prepared by the National Bureau of Standards (now National Institute of Standards and Technology, NIST) for use as calibration standards for in-situ trace element analysis. Although these glass standards are not certified with respect to U isotope composition, they can be useful to assess precision and accuracy of U-series laser ablation measurements [10,14]. Several natural glass reference materials have well characterized uranium isotope compositions [15,16], but natural glasses do not contain measurable ²³⁶U and thus may not be ideally suited for the high precision and accuracy required for microanalytical assessment of nuclear materials. The NIST SRM 600 series glasses, however, were made using a depleted U source containing measurable ²³⁶U. NIST SRM 610/611 is a good candidate for a microbeam U isotopic standard, as previous work has indicated that U is homogenously distributed [17,18,19,20]. Of the NIST SRM 600 series glasses, NIST 610/611 has the highest concentration of U (nominally 500 μg/g U), which is particularly important for the very low abundance isotopes of ²³⁴U and ²³⁶U. Published data on the U isotopic composition of NIST 610/611 exist [17,18,19,20], but results vary by technique [14,17,18], and no effort has been specifically aimed at constraining the U isotopic homogeneity [14,17,21].

Here we determine working values for the U isotope composition of NIST 610/611 and investigate the suitability of the reference glass as a microbeam U isotopic reference material. The homogeneity of NIST SRM 610/611 U isotope composition was examined by dissolution and bulk analysis of multiple fragments of glass from three different lots, as well as ion microprobe measurements. We report new working values for the following U isotope ratios for NIST SRM 610/611: ²³⁴U/²³⁸U, ²³⁵U/²³⁸U, and ²³⁶U/²³⁸U.

2. Samples

The NIST 600 series trace element glass standards were prepared by doping a base glass of the following composition: 72% m/m SiO₂, 12% CaO, 14% Na₂O, and 2% Al₂O₃ with sixty-one trace elements in varying concentrations, nominally 500 μg/g (NIST 610 and 611), 50 μg/g (NIST 612 and 613), 1 μg/g (NIST 614 and 615), and 0.02 μg/g (NIST 616 and 617) [22,23]. Odd and even numbered glasses from the same series differ only in wafer size: 12 × 3 mm (even numbers) and 12 × 1 mm (odd numbers). Most elements are present in lower abundances than the nominal concentrations due to dilution by addition of the trace element mixture or loss during manufacturing [23,24,25]. Depletions in siderophile and chalcophile elements (likely lost to crucibles and/or the furnace), depletions in volatiles (in particular the alkali elements and boron), formation of 3D compositional cords during the caning process, and loss of elements from the glass surface have been observed [18,19,23,24].

Despite documented heterogeneities in the NIST 600 series glass standards, studies have demonstrated that the concentration of U is homogeneously distributed between wafers and within single wafers of NIST SRM 610/611 [17,18]. Barnes et al. [17] randomly sampled glasses along the entire length of the 100 kg glass canes during production and found that U was homogeneous, including between NIST 610 and 611 wafers. Previous bulk analysis of small chips (150 mg) of NIST 610 showed no variation in U concentration, within a reproducibility of ≤1% [20]. Microbeam measurements indicate that U concentration is homogeneously distributed between wafers at scales of 10 μm to 1 cm, within uncertainties of 0.2% to 1% [19,20]. In this study, three wafers of NIST 611 from three different lots were broken into chips. Two 40–60 mg chips of each wafer were dissolved for analysis. Uranium isotope ratios were measured on purified U fractions from each sample using multicollector inductively coupled plasma mass spectrometry (MC-ICP-MS), and U isotope ratio measurements were made on a smaller subset of samples using multicollector thermal ionization mass spectrometry (MC-TIMS). The isotopic homogeneity of NIST 611 glass on a scale of tens of microns was evaluated by measuring ²³⁵U/²³⁸U ratios along a transect of 25 µm points in a single piece of the SRM by secondary ion mass spectrometry (SIMS).

3. Methods

3.1. Dissolution and Uranium Purification

Chips of SRM 611 (40–60 mg) were dissolved in PFA vials in four mL of 16 M HNO₃ and four mL 28.9 M HF. The vials were capped and placed on a hotplate to digest at 110 °C for 24 h. Samples were uncapped and evaporated to dryness at 120 °C. In cases where fragments of undigested material remained, the initial digestion step was repeated. Sample residue remaining following evaporation was dissolved in eight mL 16 M HNO₃. Aliquots of 20–30 μg U were taken by mass, evaporated to dryness, and re-dissolved in five mL of 9 M HCl for U purification. Procedural blanks were subjected to the same dissolution and U purification processes. Purified U fractions were prepared for analysis using an anion exchange resin (BioRad AG 1 × 4, 100–200, 0.8 mL column volume). Eluted U fractions were evaporated to dryness at 110 °C then converted to a nitrate form by dissolving each residue in 1 mL 16 M HNO₃ and evaporating to dryness at 110°C. Muticollector ICP-MS sample fractions were re-suspended in 0.32 M HNO₃ for analysis. All reagents were prepared using ultra-high purity acids (Fisher Optima^TM grade) and triple distilled H₂O (18.2 MΩ cm). Sample preparation and chemistry was carried out in a Class 100 exhausted laminar flow work station within a class 10,000 clean chemistry laboratory at Los Alamos National Laboratory (LANL).

3.2. Multicollector Inductively Coupled Plasma Mass Spectrometry (MC-ICP-MS)

Uranium isotope ratio measurements were made using a Thermo Neptune MC-ICP-MS at LANL. Measurements were in low mass resolution mode (m/Δm = 400) using a high stability dual quartz spray chamber, a PFA-ST nebulizer (Elemental Scientific), and a two jump routine with the collector configuration shown in Table 1. Replicate U isotope ratio measurements were made on purified U aliquots from each chip of dissolved glass on three separate days. The following general instrument operating parameters were used: an RF power of 1230 W, a cool gas flow rate of 16 L/min, an auxiliary gas flow of 0.94 L/min, and a sample gas flow rate of 0.9 L/min. Instrument operating conditions were optimized daily, and baseline measurements and Faraday gain calibrations were performed at the beginning of each analytical session. Instrumental U blanks were run between each sample and reference material and were subtracted online during analysis. A two-stage rinse protocol utilizing continuous rinse stations was employed between each sample, standard and blank, where the first rinse consisted of 90–120 s in 0.16 M HNO₃–0.01 M HF followed by a 90–120 s rinse in 0.32 M HNO₃. A sample-standard bracketing routine was followed during each analysis session, where every two samples were bracketed by two U isotopic reference materials diluted to a U concentration similar to the samples. A ²³⁶U-free reference material, NIST SRM U960 (natural U metal that is the same material as NBL CRM-112A [26]), was run as one reference material with each analysis set to assess and correct ²³⁵UH⁺ contributions at ²³⁶U. Average observed hydride contribution, measured as 236.05/²³⁸U in U960, was 1.35 × 10⁻⁶.The reference materials NBL CRM-U010 [27], and NBL CRM-U-005-A [28] were used for mass bias correction. Mass bias corrections were calculated and applied externally using an exponential mass fractionation law. Each respective isotope ratio measured in a reference material was used to mass bias correct the same ratio measured in a sample, which for minor isotopes makes it possible to correct for relative gain differences between electron multiplier and Faraday detectors not otherwise captured and corrected. Uncertainty associated with blank subtraction and mass bias correction were propagated in quadrature for individual measurments. Uncertainties on individual measurements are dominated by uncertainties on the reference materials used for mass bias correction purposes (e.g., U-005A uncertainty on ²³⁶U/²³⁸U = 0.8% 1σ and U-010 uncertainty on ²³⁶U/²³⁸U = 0.2% 1σ). Uncertainties for other isotope ratios in these two reference materials are listed on their respective certificates. Lower concentration solutions were selected for analysis to minimize tailing effects from ²³⁸U⁺, where ²³⁸U⁺ signals ranged from 5 to 6 V on a Faraday detector and ²³⁵U⁺ signals on a Faraday detector ranged between 10 and 15 mV. Tailing from ²³⁸U⁺ into ²³⁶U⁺ was examined using standard reference materials and was determined to be negligible at m/z = 236 and absent at m/z = 234. In consideration of the elevated ²³⁶U/²³⁸U ratio of NIST SRM 610/611 (²³⁶U/²³⁸U nominally = 4.3 × 10⁻⁶) and minimal tailing from ²³⁸U⁺, no tailing correction was applied.

3.3. Multicollector Thermal Ionization Mass Spectrometry (MC-TIMS)

Uranium isotope ratios were measured in aliquots of five samples by TIMS. Multicollector TIMS measurements were made using an IsotopX Isoprobe-T multicollector TIMS instrument using the collector configuration shown in Table 1. Aliquots of each sample were loaded on a bed of colloidal graphite. Graphite used for U loading was cleaned extensively prior to use to minimize U blank contribution. Large U aliquots (500 ng) of each sample and corresponding reference materials were loaded on triple Re filament assemblies where U isotopes were collected simultaneously on Faraday and Daly detectors (Table 1). Uranium isotopic analyses were run using a three magnet jump method, where minor U isotopes were measured on the axial Daly detector and all other isotopes were measured on Faraday detectors. Baseline measurements and detector gain calibrations were run daily. Ratios of ²³⁴U/²³⁸U, ²³⁵U/²³⁸U, and ²³⁶U/²³⁸U were used to determine the Faraday/Daly relative gain. The average measured 236.05/²³⁸U in U960 was 3.7 × 10⁻⁹ with an uncertainty overlapping zero, which indicated that tailing effects and ²³⁵UH⁺ contributions were negligible. No tailing or hydride corrections were made. External mass bias corrections were calculated using an exponential mass fractionation law and the following reference materials: NBL CRM-112A [26], NBL CRM-U-010 [27], and NBL CRM-U-500 [29], and uncertainties on individual measurements due to mass bias correction were propagated in quadrature. Standard reference materials were run at similar concentrations to the samples. Each respective isotope ratio measured in a reference material was used to mass bias correct the same ratio measured in a sample, which for minor isotopes makes it possible to correct for relative gain differences between the Daly and Faraday detectors not otherwise captured and corrected.

Table 1. The axial ion counter used on the IsotopX Isoprobe-T is a Daly electron photomultiplier detector that is linear up to greater than three million cps. The axial ion counter on the Neptune multicollector inductively-coupled plasma mass spectrometry (MC-ICP-MS) consists of a discrete dynode secondary electron multiplier. The L1 Faraday detector on the IsotopX Isoprobe-T thermal ionization mass spectrometry (TIMS) instrument is the axial Faraday detector, moved to the L1 position, which allows for simultaneous use of the axial Faraday and the Daly detector. Cup positions were aligned before MC-ICP-MS and multicollector thermal ionization mass spectrometry (MC-TIMS) analysis sessions using NBL CRM-U-500. Faraday gain calibrations were run prior to each analytical session using a controlled internal voltage.

IsotopX Isoprobe-T MC-TIMS Collector Configuration
Magnet Configuration	L1	Daly	H1	H2	H3	H4	H5
Jump 1		234U	235U	236U		238U
Jump 2		235U	236U		238U
Jump 3	235U	236U		238U
Thermo Neptune MC-ICP-MS Collector Configuration
Magnet Configuration	L1	SEM	H1	H2	H3	H4
Jump 1		234U	235U	236U		238U
Jump 2	235U	236U		238U

Table 1. The axial ion counter used on the IsotopX Isoprobe-T is a Daly electron photomultiplier detector that is linear up to greater than three million cps. The axial ion counter on the Neptune multicollector inductively-coupled plasma mass spectrometry (MC-ICP-MS) consists of a discrete dynode secondary electron multiplier. The L1 Faraday detector on the IsotopX Isoprobe-T thermal ionization mass spectrometry (TIMS) instrument is the axial Faraday detector, moved to the L1 position, which allows for simultaneous use of the axial Faraday and the Daly detector. Cup positions were aligned before MC-ICP-MS and multicollector thermal ionization mass spectrometry (MC-TIMS) analysis sessions using NBL CRM-U-500. Faraday gain calibrations were run prior to each analytical session using a controlled internal voltage.

IsotopX Isoprobe-T MC-TIMS Collector Configuration
Magnet Configuration	L1	Daly	H1	H2	H3	H4	H5
Jump 1		234U	235U	236U		238U
Jump 2		235U	236U		238U
Jump 3	235U	236U		238U
Thermo Neptune MC-ICP-MS Collector Configuration
Magnet Configuration	L1	SEM	H1	H2	H3	H4
Jump 1		234U	235U	236U		238U
Jump 2	235U	236U		238U

3.4. Secondary Ion Mass Spectrometry (SIMS)

A single wafer of NIST 611 was polished to 1 μm with diamond suspension, mounted in indium, and coated with ~30 nm of gold. In situ ²³⁵U/²³⁸U measurements were made using a CAMECA IMS 1280 SIMS at LANL using a focused ¹⁶O⁻ beam of 20 nA with a net energy of 23 keV (+13 keV primary accelerating voltage). Secondary ions were detected using a single electron multiplier. The transfer section was tuned to image an 80 μm field of view, with a contrast aperture of 400 μm and a field aperture of 4000 μm. Entrance slits were set at 122 μm. A 50 eV energy window was used, with the inner edge set to 5 eV higher than the peak in the energy distribution. Mass resolving power (MRP) was set to 4000, as this MRP was adequate to resolve a likely ²⁰⁷Pb²⁸Si⁺ interference on ²³⁵U. A 40 μm² rastered area was pre-sputtered for 120 s, and then reduced to a 25 μm² rastered area during analysis. Analyses consisted of 5 blocks of 10 cycles, with counting times of 2 s for ²³⁵U and ²³⁸U. Prior to each analysis, automatic centering routines were employed for mass calibration, energy, and beam centering in the transfer section, for a total analysis time of 25 min. An in-house glass standard doped with NBL CRM-U-500 [29] was used for instrument and detector set up, with final tuning performed on NIST 611 immediately prior to analysis. Data was corrected for dead time and background using manufacturer software.

4. Results and Discussion

Results of individual MC-ICP-MS and MC-TIMS measurements of U isotope ratios in 40–60 mg pieces of NIST SRM 611 and individual measurement uncertainties are shown in Figure 1 (see also Supplementary Table S1). Estimates of uncertainty shown for individual measured isotope ratios are standard deviations on internal independent observations propagated in quadrature, with a coverage factor of two, calculated in accordance with ISO 98-1:2009 [30]. Individual measurement uncertainties were dominated by uncertainties on U isotope compositions of reference materials used for mass bias correction. For ²³⁴U/²³⁸U and ²³⁶U/²³⁸U, the weighted mean working values and expanded uncertainties listed in Table 2 were calculated using MC-ICP-MS and MC-TIMS data collected in this study only. For ²³⁵U/²³⁸U, data and uncertainties reported by Stirling et al. [14] were included in the weighted mean working value. The expanded uncertainties represent a pooled standard deviation, with a coverage factor of two, for the data from Table 2 and Figure 1, including data from Stirling et al. [14] for ²³⁵U/²³⁸U. The results of Barnes et al. [17] and Duffin et al. [21] were excluded from the weighted mean working values and expanded uncertainties listed in Table 2.

Table 2. Working U isotope ratios values for NIST SRM 610/611.

	234U/238U	235U/238U	236U/238U
Mean *	9.45 × 10−6	2.39555 × 10−3	4.314 × 10−5
Uncertainty **	5.0 × 10−8	4.7 × 10−7	4.0 × 10−8

Notes: ^* Mean = weighted mean of 35 MC-ICP-MS and MC-TIMS measurements from this study. The ²³⁵U/²³⁸U weighted mean includes nine measurements from Stirling et al. [14]. ^** Uncertainty = pooled standard deviation of all analytical sessions and literature data, where appropriate, with a coverage factor of two: .

Table 2. Working U isotope ratios values for NIST SRM 610/611.

	234U/238U	235U/238U	236U/238U
Mean *	9.45 × 10−6	2.39555 × 10−3	4.314 × 10−5
Uncertainty **	5.0 × 10−8	4.7 × 10−7	4.0 × 10−8

Notes: ^* Mean = weighted mean of 35 MC-ICP-MS and MC-TIMS measurements from this study. The ²³⁵U/²³⁸U weighted mean includes nine measurements from Stirling et al. [14]. ^** Uncertainty = pooled standard deviation of all analytical sessions and literature data, where appropriate, with a coverage factor of two: .

4.1. Matrix Complications When Using NIST SRM 610/611 as a U isotope Microbeam Standard

Femtosecond laser ablation ICP-MS results reported by Duffin et al. [21] do not overlap results reported in this study nor those reported by Stirling et al. [14] (Figure 1). While the origin of this poor agreement is not entirely clear, it is likely influenced by transient ^194–198Pt^36–40Ar⁺ polyatomic interferences that affect ²³⁴U⁺, ²³⁵U⁺, ²³⁶U⁺, and ²³⁸U⁺ (Table 3), with ^194–198Pt⁴⁰Ar⁺ interferences generating the greatest contributions [21]. The NIST 600 series glasses were produced via melting base glass materials in a large Pt crucible within a Pt-Rh lined furnace [17,22]. Eggins and Shelley [18] documented Pt-rich heterogeneities (Cu-Pt domains) within NIST 600 series glasses. If Pt-rich domains are encountered during microbeam sampling, the contributions by the interferences listed in Table 3 become non-trivial. NIST SRM 610/611 contains 453.3 µg/g total U [31], and using the working values listed in Table 2, this equates to 0.002 µg/g ²³⁴U, 1.08 µg/g ²³⁵U, and 0.02 µg/g ²³⁶U. Sylvester and Eggins [24] reported a Pt concentration in NIST SRM 610 of approximately 3 µg/g. Uranium-234 is the most affected by Pt-Ar interferences, both because of the greater number of Pt-Ar interferences at mass 234 (Table 3), and because it is the least abundant U isotope in NIST SRM 610/611. Indeed, the ²³⁴U/²³⁸U ratios reported by Duffin et al. [21] exhibit the poorest agreement with data from this study and Stirling et al. [14] (Figure 1). A mass resolving power of >2000 is required to mitigate the Pt-Ar interferences listed in Table 3, and the resulting lower transmission makes the measurement of the minor U isotopes more challenging.

Figure 1. Results of individual U isotope measurements of NIST SRM 610/611 from three MC-ICP-MS analysis sessions and one MC-TIMS session are plotted against the weighted mean (dotted line) and expanded uncertainty (Unc.; grey shaded area) of data from this study. Literature data point uncertainties either were not reported or are smaller than the symbols. (A) Individual measurements of ²³⁴U/²³⁸U. The data point from Stirling et al. [14] was calculated from their reported activity ratio using ²³⁴U T_1/2 = 245,250 years (Cheng et al. [32]) of and ²³⁸U T_1/2 of 4.468 × 10⁹ years (Jaffey et al. [33]). (B) Individual measurements of ²³⁵U/²³⁸U. Data from Stirling et al. [14] are included in the weighted mean and expanded uncertainty. (C) Individual measurements of ²³⁶U/²³⁸U.

Figure 1. Results of individual U isotope measurements of NIST SRM 610/611 from three MC-ICP-MS analysis sessions and one MC-TIMS session are plotted against the weighted mean (dotted line) and expanded uncertainty (Unc.; grey shaded area) of data from this study. Literature data point uncertainties either were not reported or are smaller than the symbols. (A) Individual measurements of ²³⁴U/²³⁸U. The data point from Stirling et al. [14] was calculated from their reported activity ratio using ²³⁴U T_1/2 = 245,250 years (Cheng et al. [32]) of and ²³⁸U T_1/2 of 4.468 × 10⁹ years (Jaffey et al. [33]). (B) Individual measurements of ²³⁵U/²³⁸U. Data from Stirling et al. [14] are included in the weighted mean and expanded uncertainty. (C) Individual measurements of ²³⁶U/²³⁸U.

Table 3. Polyatomic interferences affecting uranium isotopes.

234U	194Pt40Ar+	196Pt38Ar+	198Pt36Ar+	204Pb30Si+	206Pb28Si+
ΔM	0.12	0.11	0.11	0.09	0.09
MRP	2019	2066	2218	2486	2613
235U	195Pt40Ar+	206Pb29Si+	207Pb28Si+
ΔM	0.12	0.09	0.09
MRP	2013	2528	2579
236U	196Pt40Ar+	198Pt38Ar+	206Pb30Si+	207Pb29Si+	208Pb28Si+
ΔM	0.12	0.11	0.10	0.09	0.09
MRP	1996	2053	2425	2533	2566
238U	198Pt40Ar+	208Pb30Si+
ΔM	0.12	0.10
MRP	1975	2371

Table 3. Polyatomic interferences affecting uranium isotopes.

234U	194Pt40Ar+	196Pt38Ar+	198Pt36Ar+	204Pb30Si+	206Pb28Si+
ΔM	0.12	0.11	0.11	0.09	0.09
MRP	2019	2066	2218	2486	2613
235U	195Pt40Ar+	206Pb29Si+	207Pb28Si+
ΔM	0.12	0.09	0.09
MRP	2013	2528	2579
236U	196Pt40Ar+	198Pt38Ar+	206Pb30Si+	207Pb29Si+	208Pb28Si+
ΔM	0.12	0.11	0.10	0.09	0.09
MRP	1996	2053	2425	2533	2566
238U	198Pt40Ar+	208Pb30Si+
ΔM	0.12	0.10
MRP	1975	2371

Lead-Si⁺ polyatomic interferences may also negatively impact the accuracy of U isotope ratios measured using microbeam techniques, requiring an MRP of 2200–2600 (Table 3). Fortunately lead is relatively uniformly distributed in NIST SRM 610/611 [18], such that one can assume the contribution of Pb-Si⁺ interferences will be more uniform than Pt-Ar⁺ interferences. In general, U isotope ratios measured by LA-ICP-MS are acquired in low mass resolution due to loss in ion transmission at higher mass resolutions. Should NIST SRM 610/611 be used as a microbeam U isotopic reference material, careful consideration should be given to the potentially problematic nature of its trace element-rich matrix. NIST 610/611 can be used as a U isotope microbeam reference material with higher confidence where it is possible to measure U isotope ratios at higher mass resolution. For example, the 1280 SIMS does not suffer the same significant loss of ion transmission at high mass resolution that small geometry SIMS and other mass spectrometry techniques experience.

4.2. Uranium Isotopic Homogeneity of NIST SRM 610/611

The suitability of NIST SRM 610/611 as a U isotopic microbeam standard is largely dependent on the U isotopic homogeneity of each wafer. Uranium isotope ratios measured in 6 chips of NIST SRM 611, each representing 10%–20% of the total mass of the different wafers, are plotted against the weighted mean ²³⁵U/²³⁸U ratio determined in this study in Figure 2A. These data indicate that NIST SRM 610/611 is isotopically homogeneous on a macroscopic scale (1000s of microns). The U isotopic homogeneity of NIST SRM 610/611 was evaluated on smaller scale by SIMS. Analyses of ²³⁵U/²³⁸U were performed with 100 μm spacing along a single transect from the wafer edge toward the center (total distance 3900 μm) at a MRP sufficient for resolving the polyatomic interferences listed in Table 3 (Supplementary Table S2). The dotted line shown in Figure 2 represents the mean of all SIMS results, and the gray area represents a 2σ uncertainty on the mean. Individually measured ²³⁵U/²³⁸U are reproducible to within <1% at the 1σ level at 25 μm resolution (probe raster size), with RSDs on the order of 0.8% to 1.1% for individual spots (Figure 2). Within the limits of SIMS counting statistics, ²³⁵U/²³⁸U shows no compositional heterogeneity in the wafer. Homogeneity of NIST 610/611 can also be assessed from Duffin et al. [21]. The authors did not explicitly examine homogeneity, but they report >100 data points, each representing a 30 s raster, in their Figure 2. We calculated uncertainties for ²³⁴U/²³⁸U, ²³⁵U/²³⁸U, and ²³⁶U/²³⁸U from their average atom % values for each isotope, which results in 2σ uncertainties of ≤0.3% for all ratios, again lending support to the U isotopic homogeneity of NIST 610/611.

Figure 2. (A) The results of an individual ²³⁵U/²³⁸U measurement from each of the 40–60 mg pieces from the wafers of NIST SRM 611 (represent 10%–20% of the mass of each wafer) are shown against the weighted mean (orange dotted line) and expanded uncertainty (grey shaded area) determined for the SRM in this study. (B) The ²³⁵U/²³⁸U ratios measured by SIMS along a 3.9 mm transect across NIST SRM 611 are plotted against the mean of all SIMS measurements. These results indicate that NIST SRM 610/611 is homogeneous on a scale from 10s of µm to 1000s of µm.

Figure 2. (A) The results of an individual ²³⁵U/²³⁸U measurement from each of the 40–60 mg pieces from the wafers of NIST SRM 611 (represent 10%–20% of the mass of each wafer) are shown against the weighted mean (orange dotted line) and expanded uncertainty (grey shaded area) determined for the SRM in this study. (B) The ²³⁵U/²³⁸U ratios measured by SIMS along a 3.9 mm transect across NIST SRM 611 are plotted against the mean of all SIMS measurements. These results indicate that NIST SRM 610/611 is homogeneous on a scale from 10s of µm to 1000s of µm.

5. Conclusions

New high precision uranium isotope ratio measurements of NIST SRM 610/611 glass were collected by MC-ICP-MS and MC-TIMS, and SIMS. Working values for ²³⁴U/²³⁸U, ²³⁵U/²³⁸U, and ²³⁶U/²³⁸U are presented, with uncertainties calculated in accordance with ISO 98-1:2009. Multiple bulk analyses of 40–60 mg aliquots by MC-ICP-MS and MC-TIMS show no U isotopic heterogeneity, and microanalysis by SIMS shows that ²³⁵U/²³⁸U is reproducible to within 1% (within analytical uncertainty) at a scale of 25 μm. We conclude that NIST 610/611 is homogeneous at 10s to 1000s of μm and is a suitable reference material for spatially-resolved uranium isotope measurements at the microanalytical scale. However, the trace element-rich matrix of the NIST SRM 600 series glasses requires analysis at higher mass resolving power (≥2000) to eliminate potential interferences for techniques that do not involve chemical separation, in particular microbeam analysis.