E. Hywel
Evans
*a,
Jorge
Pisonero
b,
Clare M. M.
Smith
c and
Rex N.
Taylor
d
aSchool of Geography, Earth, and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, UK PL4 8AA. E-mail: hevans@plymouth.ac.uk
bUniversity of Oviedo, Faculty of Science, Department of Physics, c/Calvo Sotelo s/n, 33006 Oviedo, Spain
cSt. Ambrose High School, Townhead Road, Coatbridge, Lanarkshire, UK ML5 2HT
dOcean and Earth Science, University of Southampton, NOC, Southampton, UK SO14 3ZH
First published on 20th April 2017
Strapline: This review of 163 references covers developments in ‘Atomic Spectrometry’ published in the twelve months from November 2015 to November 2016 inclusive. It covers atomic emission, absorption, fluorescence and mass spectrometry, but excludes material on speciation and coupled techniques which is included in a separate review. It should be read in conjunction with the previous review and the other related reviews in the series. A critical approach to the selection of material has been adopted, with only novel developments in instrumentation, techniques and methodology being included. There do not seem to be novel developments that really stand out this year. However, there has been steady progress in understanding how particles behave as they transit through the ICP, and how this affects ionisation and matrix interferences. Allied to advances in single particle analysis by nebulisation ICP-MS, this promises to yield useful information about the composition of nanoparticles. The development of element tagging approaches for ICP-MS has slowed considerably, largely due to the dearth of available standards for biological assays, but some advances have been made in this area which point the way forward. The number of stable isotope systems which are now examined routinely by ICP-MC-MS has grown over the period of the review. Such methods may eventually lead to new insights into isotopic fractionation effects that result from environmental and biological processes which involve these elements. There have been several novel developments in instrumentation, such as ambient desorption ionisation, using a variety of modified sources and liquid electrode plasmas for AES. These hold some promise as low-cost sources that may be incorporated into miniaturised systems of the future.
A novel take on SPME was reported by Asiabi et al.,2 who developed an electrochemical method using a stainless steel capillary tube coated internally with polypyrrole doped with polyethyleneglycoldimethacrylate (PPy-EGDMA). The sample solution was passed through the PPy-EGDMA electrode tube and Se (anionic form) extracted by applying positive potential of 0.8 V. Desorption into 150 μL of 0.1 mol L−1 NaCl was effected by applying a negative potential, and the analyte then eluted in 3.0 mol L−1 HCl for determination by HG-AAS with an LOD of 0.004 μg L−1. The method was validated by the analysis of several tap and wastewater samples and was deemed free from interferences by coexisting ions commonly found in natural waters.
Microfluidic sample preparation and introduction systems have become increasingly common for MS assays of organic compounds, in the form of chip-based assays. However, they have struggled to gain a routine foothold when coupled with atomic spectrometry. Nevertheless, Zhang et al.3 have developed a device for the microextraction of Bi from HepG2 cell lysate, followed by Bi determination by ICP-MS. Polyglycidylmethacrylate trimethylolpropane triacrylate (poly(GMA-co-TRIM)) monolithic columns were fabricated in situ on a PDMS chip. The 2.5 cm × 50 μm × 500 μm columns were surface modified with EDTA to allow SPE from 100 μL of cell lysate solution. The LOD was 0.21 ng mL−1.
The use of isotopically labelled standards which have been synthesised from scratch, e.g. by a cell culture method, are preferred. This approach was adopted by Hermann et al.,8 who synthesised 34S-labelled cysteine and methionine in vivo, using a yeast fermentation method, for IDA quantification of cysteine and methionine by ICP-QQQ-MS. Enrichment to 96.3% and 98.5%, and LODs of 1.0 and 0.56 μmol L−1, were achieved for cysteic acid and methionine sulfone, respectively. The IDA method was validated for the absolute quantification of lysozyme and ceruloplasmin protein standards after hydrolysis to individual amino acids. Deitrich et al.9 synthesised 76Se-enriched peptides for use as calibrants in the ID-ICP-QQQ-MS determination of selenoprotein P (SEPP1) after tryptic digest to release the individual peptides. Key to this was equilibration of the spike with the peptides during sample digestion and subsequent chromatographic separation so that the peptides specific to SEPP1 could be determined. In a subsequent paper, some of the same workers10 took this approach a step further by synthesising a standard and spike of the complete SEPP1 protein by cell-free E. coli protein synthesis, where Se was introduced in the form of selenomethionine. This was used to determine SEPP1 in human plasma by ID-HPLC-ICP-MS. The method was validated by analysis of BCR-637 and SRM 1950. In keeping with a metrological approach, they performed a number of different types of analysis to validate the method, including both species-specific and species-unspecific IDA of the intact proteins, and comparison with post-column, species-specific IDA of the Se-peptides. A complete uncertainty budget was also calculated with a coverage factor of k = 2. These combined approaches give confidence in the method such that, for example, the analysis of BCR-637 resulted in the sum of the individual Se species totalling to 80 ng g−1, compared with total Se of 79.6 ng g−1 and a certified value for total Se of 79 ng g−1.
Specificity of the target protein or peptide in the aforementioned studies was achieved by chromatographic separation. However, another way of achieving this is by means of an immunoassay type approach wherein an isotopic tag is applied to a specific target molecule. Research in this area has been reviewed (58 references) by Liu et al.,11 who focused on tagging with stable isotopes via antibody–antigen or nucleic acid probe vectors; multiplexing to enable determination of multiple analytes in a single shot; and absolute quantitation of biomolecules. A novel example of using a nucleic acid probe is described by Chen et al.,12 who utilised a hairpin DNA beacon probe. The probe contained numerous thymine bases which formed a thymine–Hg2+–thymine connection, such that Hg2+ was sandwiched in the hairpin of the folded DNA strand. The presence of a complementary DNA sequence (the target molecule) resulted in hybridisation and release of the Hg2+ which was detected using CVG-AFS with reduction by SnCl2. Determination of single and double stranded DNA, and proteins yielded LODs as low as 0.2 and 0.3 nM. The protein thrombin was also determined, with a LOD of 0.08 nM, using a thrombin specific aptamer to enable specificity. An additional advantage of this approach is that multiple Hg2+ ions are released for every target molecule, thereby amplifying the analytical signal. This is even more pronounced when nanoparticles, containing thousands of metal atoms per target molecule, are used as tags. For example, Liu et al.13 used an immunoreaction of caspase-3, primary antibody and gold NP labelled IgG; then subsequent determination by ICP-MS after release of the gold NPs from the immune-complex. An LOD of 0.42 ng mL−1 (0.31 nM) was obtained for caspase-3. A similar approach was adopted by Xu et al.14 for the determination of human IgG, but this time by labelling with CuO nanoparticles and determination by GFAAS. They achieved an LOD of 0.19 ng mL−1, which is comparable to ICP-MS.
A variation on this amplification method was reported by Liang et al.15 who also used a sandwich immunoassay for the determination of an organophosphorylated acetylcholinesterase adduct (OP-AChE), which is a biomarker for exposure to organophosphate pesticides and nerve agents. The OP-AChE target compound was captured from the sample matrix by chelation with TiO2 coated magnetic nanoparticles (TiO2-MNPs), which were then selectively recognised by an anti-AChE antibody attached to a protein cage nanoparticle (PCN). The PCN was packed with lead phosphate which could be released, after separation from the sample matrix, and determined by ET-AAS. The LOD was 2 pM, which is below the average AChE concentration in human plasma and erythrocytes (ca. 0.12 nM and 3 nM respectively). This compared well with an LOD of 0.02 nM obtained using electrochemical detection.
Gold NPs were used by Kanaki and Pergantis to determine the transport efficiency (TE%) of microflow and nanoflow nebulisers in ICP-MS.18 An aqueous suspension containing 60 nm gold NPs (a NIST reference material) was introduced to an ICP-MS operating in single particle mode (short dwell times and dilute samples) for the detection of individual NPs. Various flow rates ranging from 500 nL min−1 to 10 mL min−1 using various modified pneumatic nebulisers were tested and transport efficiencies were determined. In addition, the overall system sensitivity was determined for both gold NP suspensions and dissolved metal solutions. The method suggested has the potential to allow comparisons of TE% for the various micro-/nano-flow systems currently in use and those in development.
Single particle (sp) ICP-MS has proven to be a powerful technique for the detection and characterisation of aqueous dispersions of metal-containing nanomaterials. Combining high-throughput with the specificity of a single particle counting technique and the elemental specificity of ICP-MS, spICP-MS is capable of rapidly providing researchers with information pertaining to size, size distribution, particle number concentration, and major elemental composition with minimal sample perturbation. Recently, advances in data acquisition, signal processing, and the implementation of alternative mass analysers (e.g., time-of-flight) has resulted in a wider breadth of particle analyses and made significant progress toward overcoming many of the challenges in the quantitative analysis of NPs. A useful review by Montano et al. provides an overview of spICP-MS development from a niche technique to application for routine analysis, a discussion of the key issues for quantitative analysis and examples of its further advancement for analysis of increasingly complex environmental and biological samples.19 Asymmetrical flow field-flow fractionation (AF4) coupled with spICP-MS is considered to be a valuable tool for separating, characterising and quantifying engineered nanoparticles for their risk assessment and evaluation in terms of environmental exposure. Optimisation of a system for this purpose was described by Lee et al.20 Application of the same technique to the determination of silver NPs in the environment was also described by Huynh et al.21 The results obtained indicated that AF4-spICPMS is capable of detecting and quantifying silver NPs and other engineered metal NPs in environmental samples. However, the authors concluded that further studies are needed before AF4-spICPMS can become a routine analytical technique.
A heated torch integrated sample introduction system (hTISIS) has been used for direct injection of bioethanol into ICP-OES for the determination of metals and metalloids.23 Two injection modes (continuous liquid aspiration and air-segmented FI analysis) were evaluated. The matrix effects caused by ethanol–water mixtures were removed by operating the hTISIS at 400 °C in segmented injection. It was also demonstrated that the system could be operated in continuous mode at 200 °C with complete interference removal. Twenty eight samples with bioethanol contents between 55% and 100% were analysed and recoveries from 80% to 120% were obtained for 18 analytes. The analyte concentrations determined were in agreement with those obtained using a preconcentration reference method. LODs from 3 ng mL−1 for Mn to 500 ng mL−1 for Ca were obtained.
D'Ulivo25 has presented a comprehensive review (90 references) of the mechanism of CVG using tetrahydridoborate (THB), with the aim of producing a reaction model for aqueous CVG of metal and semimetal species. This was attempted by combining current knowledge of reaction mechanisms in analytical CVG with the literature on the synthesis of nanoparticles using aqueous THB and applications in catalytic hydrolysis for hydrogen production. The author outlines the current state of knowledge to be: hydrides are formed by direct transfer of hydrogen from borane species to the analyte atom; then hydrogen transfer takes place through an analyte–borane complex; and the final volatile hydrides are formed stepwise via the formation of intermediate hydrido-metal complexes. Depending on the stability of the final hydride, it can decompose to release the element in the zero valent state. Alternatively, it is possible that the intermediate hydrido-metal complex could release the element. Focusing predominantly on CVG of arsenic species, the author developed a ‘non-analytical’ reaction model which took into account some additional possibilities, viz.: the CVG of polynuclear and mononuclear substrates; formation of by-products by reaction with intermediate hydrido-metal complexes; competition between hydride formation and condensation reactions. A further conclusion was that when the analyte:borane ratio is several orders of magnitude, the rate of condensation decreases the rate of formation of hydrides and intermediate hydrido-metal complexes increases. Under these conditions the non-analytical reaction model reduces to the simpler analytical one.
Novak et al.26 investigated a planar DBD as an atom cell for CVG-AAS and compared it with the more commonly used QTA. The advantage of the DBD is that it is relatively compact and requires only a 25 kHz, HV power supply operated at 17 W. The DBD was evaluated using argon, nitrogen, helium and hydrogen as discharge gases, for the atomisation of the hydrides of As. LODs of 0.16 ng mL−1 and 0.15 ng mL−1 were obtained using the DBD and QTA respectively. Matrix interferences caused by other hydride-forming elements Bi, Sb and Se were absent below 500 ng mL−1. Interestingly, when oxygen was added to the gas flow at 7 mL min−1 it was possible to pre-concentrate arsine in the DBD, which was subsequently volatilised when the oxygen flow was stopped. A pre-concentration efficiency of ca. 100% was observed for pre-concentration periods of up to 300 s, thereby lowering the LOD to 0.012 ng mL−1.
A DBD has been used by Li et al.27 to generate volatile species for AFS detection. They investigated the effect of adding a non-ionic surfactant to the sample on the generation of volatile Cd and Hg species, in a method which they called DBD-plasma CVG. They found that the addition of Triton X-114 resulted in approximately 5-fold improvements in the fluorescence signals for Cd and Hg, with respective LODs of 2.4 and 4.5 ng L−1. They postulated that the surfactant increased the reaction rate and transport efficiency of ‘plasma assisted chemical reactions’ which produced the volatile species, though no empirical evidence of this was presented. Pyrolysis has also been used combined with CVG-AFS to improve efficiency of volatile Cd generation.28 The sample was pyrolysed at ∼500 °C in the presence of sodium formate to yield volatile Cd species. Thiourea was also added to enhance the efficiency and eliminate interference due to Cu. An LOD of 0.38 ng for 0.17 mL of sample was achieved.
Ionic liquids have also been used to modify CVG reactions, the aim generally being to enhance sensitivity or reduce interferences. Wen et al.29 investigated solid reductants of LiAlH4, SnCl2 or THB in a room temperature ionic liquid (IL) for CVG-AFS. Analyte ions were extracted from the aqueous phase into the IL by LLE then directly mixed with the solid reductant to generate volatile species of AsIII, HgIII and SbIII. Interferences from Cu, Fe, Ni, Zn and Pb were generally absent at concentration between 2.5 and 20 mg L−1. Compared to conventional CVG-AFS, absolute LODs for As, Hg and Sb were 62, 24, and 96-times lower respectively, but concentration LODs were higher because of the 10 μL sample size. A similar approach was adopted by Zeng et al.30 using LLE into a fluorine-free IL, but with thermospray FF-AAS as the method of detection. Complexation of Bi and Se with dithizone and APDC, respectively, facilitated extraction into 1-octyl-3-methylimidazolium perchlorate, where solid KBH4 was used to generate volatile species. LODs for Bi and SeIV were 8.3 and 4.8 ng mL−1, respectively.
Coutinho et al.33 developed a PVG method for the determination of Co in biological samples using a 50% formic acid solution, UV radiation at 254 and 185 nm, and ICP-OES detection. They initially encountered strong matrix interferences but these were reduced with longer irradiation times and >50-fold dilution factor, to achieve between 90% and 110% recoveries for analyses of CRMs TORT-2 and TORT-3.
Wang et al.34 investigated the effect of ferric species as ‘enhancers’ for the determination of inorganic As by PVG-AFS. They found that 15 mg L−1 of ferric chloride plus 20% acetic acid combined with 4% formic acid and 30 s UV irradiation resulted in a 10-fold signal enhancement, and yielded an LOD of 0.05 μg L−1.
An interesting coupling of a GD in pulsed mode (PGD) as secondary source for excitation/ionisation of the material provided by LA was investigated using OES.38 Emission properties of the LA-PGD plasma in each temporal region (prepeak, plateau or afterglow) of the GD pulse were evaluated for analytical lines of different elements. Resonant atomic lines showed higher emission intensity in the prepeak region compared to non-resonant lines. Non-resonant lines showed higher enhancement of the emission intensity in the afterglow region. The coupled LA-PGD system offered better linear correlation coefficients using a set of glass standards for calibration as well as lower LOD (by at least a factor of two) when compared to LIBS.
Laser ablation is a promising technique for the direct analysis of polymer samples, however, the lack of available reference materials and the presence of matrix dependent effects means that internal standardisation is necessary for quantitative analysis. Deiting et al.41 investigated: the correlation between the C released during the ablation process; the 13C signal detected by ICP-MS; and its use as an internal standard. In the study, twenty-one virgin polymer materials were ablated and the released C determined and correlated with the corresponding integrated 13C signal. A direct relationship between the ablated carbon and 13C signal was observed, demonstrating the potential ability to overcome at least some of the matrix dependent and transport effects which occur during the LA of virgin polymers.
A near-field LA system was developed for the analysis of inorganic solid samples in the nanometer resolution range.42 The instrument is based on the coupling of a nanosecond Nd:YAG laser with an AFM. The technique uses a tip enhancement effect obtained by the interaction of laser radiation with the conductive tip of the AFM maintained at a few nanometers above the sample surface. By applying this technique to conducting Au and semiconducting silicon samples, a lateral resolution of 100 nm was demonstrated. With a single laser pulse, craters of about 100 nm in diameter and a few nanometers in depth were obtained. A multi-parametric study was carried out in order to understand the effect of different experimental parameters (laser fluence, tip-to-sample distance, sample and tip nature) on the near-field LA efficiency, crater dimensions and amount of ablated material. Numerical simulations of the localised heating with a home-made 3-D code provided a good explanation for the nanometer-sized crater diameters obtained in the experiments.
LA was successfully applied to the analysis of low molecular weight solids separated on standard TLC plates.43 The ablated sample was ionised using a flowing atmospheric pressure afterglow source. The laser pointer used was capable of ablating organic compounds directly from the TLC spots and the LOD was estimated to be 35 ng cm−2 of a pyrazole derivative.
Over the last decade, the application of LA-ICP-MS in bioimaging has steadily increased. In the time covering this review, a significant number of publications describing the approach have appeared. Gundlach-Graham and Gunther44 provided a review describing trends in fast, high resolution elemental imaging by LA-ICP-MS. They reported that the recently developed low dispersion LA cells can deliver quantitative transport of ablated aerosols within 10 ms and provide enhanced sensitivity compared to conventional LA cells because the analyte ion signal becomes less diluted during aerosol transport. Combining these low dispersion cells with simultaneous ICP-MS can help to overcome the instrumental limitations of elemental imaging to deliver faster, higher resolution analyses. A review by Van Malderen et al. covers developments in the design of LA cells, the associated transport tubing assembly and their coupling to ICP-MS instrumentation.45 Recently developed low dispersion ablation cell designs have reduced the pulse response duration for a single laser shot to <10 ms, using the criterion of the full peak width at 1% of the height of the maximum signal intensity. The evolution towards these low dispersion systems was described and reported to have been profoundly influenced by: an understanding of processes driving the initial dispersion; of the design aspects of the cell and tubing that influence transport-induced dispersion and transport efficiency; and of limitations imposed by the temporal resolution of ICP-MS instruments. Rapid response LA-ICP-MS systems greatly benefit throughput and sensitivity, which are key parameters in 2D and 3D imaging at high lateral resolution. As noted earlier, the analysis and imaging of biological material has come to the forefront as a key application of LA-ICP-MS and the review described the impact of the technical developments in LA-ICP-MS systems on emerging applications, including multiplexed metal-tagged antibody detection (for immunohistochemistry), NP and compound hypo- and hyperaccumulation, and (intra-) cellular/histological studies.
The incorporation of cooling to the LA cell allows elemental imaging of soft and semi-soft samples, specifically biological tissues to be carried out. Hamilton et al.46 described the evaluation of a custom single Peltier-cooled ablation cell for this purpose. Use of the cell was successfully applied to the analysis of three different biological tissues as spatially resolved images of mapped elements were obtained whilst maintaining the structural integrity of the tissues.
A combination of LA-ICP-MS and LIBS was used for laterally resolved elemental analysis of biological samples.47 LIBS was used to overcome the inability of LA-ICP-MS to detect bulk components such as H or O. In addition to those elements, some other elements that are difficult or impossible to investigate using LA-ICP-MS (e.g. F, N, Cl), can be detected by LIBS. In the described work, tandem LA/LIBS (the simultaneous use of LIBS and LA-ICP-MS) was applied to the analysis of biological samples, with the purpose of moving towards the possibility of the complete analysis of the elemental composition of a human tumour sample. The results obtained showed good correlation with histological staining and the distribution images obtained were deemed to provide a useful basis for further medical interpretation.
Bishop et al. used triple quadrupole-ICP-MS (instead of the commonly-used single quadrupole) for elemental bioimaging using LA.48 The triple quadrupole ICP-MS was found to reduce the polyatomic interferences that can restrict the sensitivity of biologically important elements such as Fe.
Periodically, there is a flurry of research into ion sources which are capable of generating anything from the molecular ion of an organic molecule through to elemental ions. The latest iteration of this is the development of ambient desorption ionisation (ADI) sources and variations on them, which can operate on solid samples at atmospheric pressure. One such has been reported by Evans-Nguyen et al.,52 who used a modified MPT for ADI from solid samples placed in the gap between the source and the interface of an ion-trap MS. The MPT was operated at 300 W and with an argon flow rate of 68 L min−1[sic], according to the paper. This was sufficient to desorb and ionise the matrix elements direct from samples such as a coin but less successful for the determination of minor elements deposited on a filter paper. When a metal mesh substrate was used instead of filter paper amounts of Ba and Cs at 100 ng and 1 ng respectively were detected. In comparison, the same conditions were used to produce limited fragmentation of the gunshot residue (GSR) methyl centralite (100 ng) and the explosive RDX (1 μg), and application that would be useful for the simultaneous determination of firearm discharge residue components on forensic swabs. A similar set-up, called matrix assisted plasma atomisation emission spectrometry (MAP-AES) has been reported by Yuan et al.,53 who used the tail plume of a surfatron to desorb and ionise elements from salt solutions deposited on a filter paper. LODs were between ∼2 and ∼60 ng mL−1 for a number of transition elements.
Another investigation into ADI, this time using a GD as the source, has been undertaken by Marcus et al.54 They used a 75 μm i.d. × 125 μm o.d. fused silica capillary, mounted coaxially within a 500 μm i.d. × 700 μm o.d. stainless steel capillary, surrounded by a helium sheath gas flow of 0.6 L min−1. A 5% (v/v) aqueous HNO3 solution was passed through the capillary and a liquid electrode plasma generated upon application of a 60 mA, ∼850 V d.c. power supply. This was used to volatilize, ionise and excite Cu and Ni species from samples such as metallic thin films, dry solution residues, and bulk materials, with detection by OES for qualitative analysis. Given that the thermal temperature of the plasma does not exceed 300 °C they speculated that there is likely to be a vapour phase chemical process occurring, possibly related to the presence of H3O+ or the formation of volatile metal salts (with which this reviewer speculates there may be similarities with matrix modification used to influence volatility in GF-AAS?).
A softer approach to ionisation was taken by Klute et al.55 who investigated a helium DBD source, doped with CHClF2 at between 750 ppb and 150 ppm as analyte. The DBD was initiated by a square-wave voltage with a rise-time within 0.01 μs and peak-to-peak voltages up to 4 kV, at a frequency of 20 to 40 kHz. Spatiotemporal measurements of the plasma emission showed that, during a single voltage duty cycle, the plasma evolved from a soft to dissociative ionisation source. The LODs for CHClF2 were 0.7 and 1.2 ppb using the Cl 912 and the F 739 nm lines, respectively.
In a novel study, Nakadi et al.56 described a method for isotopic analysis using high resolution continuum source GF-AAS. What made this approach different was that they chose to deliberately generate diatomic species of Br from solid samples (CaBr being the preferred diatom) which have much larger isotopic shifts in their molecular spectra compared to their atomic spectra. The species were generated using a matrix modifier comprised of 500 mg L−1 palladium NP and a 10 g L−1 Ca solution in HNO3 (5% v/v). The molecular transitions of Ca79Br and Ca81Br which yielded greatest sensitivity, resolution and precision were observed at 600.492 nm and 600.467 nm respectively. The method was used for the IDA of Br in PVC-H-07-A and NIST SRM 1573a tomato leaves. Direct solid sampling was adopted and the method yielded good agreement with the certified value and 4–8% RSD precision. The LOQ was estimated to be 60 ng for 20 μL liquid samples, or 30 μg g−1 for solid samples using a sample mass of 2 mg.
A chip based LEP-OES system has been further developed by workers in Japan.57 The principle of this micro-plasma device is based on Joule heating, caused by application of a pulsed-DC voltage to an electrolyte confined in a microchannel. The vapour bubbles formed as a result contained microplasmas which were capable of exciting atomic emission of elements dissolved in solution. The techniques lends itself readily to microfabrication on a chip, however, one of the problems is low sensitivity because the PDMS material used has poor light transmission close to the UV. One way round this is to fabricate chips from quartz, but this is difficult and expensive, so an alternative approach was adopted whereby the chip design included a channel for inclusion of a Pb-selective SPE resin for pre-concentration. In a further refinement, a pneumatic membrane micro-pump was also incorporated. In this way, an LOD of 0.4 ng mL−1 was obtained for Pb.
In a completely different type of study,60 the same research group have investigated the use of interference filters with a 10 nm bandpass in conjunction with solution-cathode GD-OES. The idea was to develop a low-cost instrument. This computer-controlled filter wheel instrument provided RSDs between 0.5 and 4.6%, linear ranges of between 1.5 and 4.9 orders of magnitude, and LODs that ranged from 0.5 to 450 ppb for the alkali and alkaline earth metals. The LODs were between 2 and 43 times higher than the case with a traditional spectrometer and the instrument suffered from interferences caused by background emission due to the sample matrix, which could not be easily corrected.
Ion trap mass spectrometers have been used extensively in organic MS, but the difficulty of coupling them with many plasma sources means that they have found less favour for elemental analysis. However, if these problems can be overcome, their compact size and ability to perform MSn in a single unit offers definite advantages. Hoegg et al.61 have coupled a liquid-sampling, atmospheric pressure GD to a commercial ion trap instrument with the specific purpose of evaluating it for IRMS measurements of U isotopes. An IR precision of ∼0.1% RSD was achieved, but this was degraded to 1–3% RSD for low-abundance species. However, as the intention was also to use this as a field deployable instrument, this was deemed satisfactory. Jiang et al.62 coupled an MPT with a commercial linear ion trap MS instrument, for the determination of Cd and Zn as both positive M(NO3)·nOH·mH2O and negative M(NO3) ions. The MPT was operated at 50 W with a total gas flow of ∼1300 mL min−1 argon. Spectra obtained in positive ion mode were too complex to be used for quantitative analysis, but negative ion spectra were simpler and allowed quantitation, with LODs of 10 μg L−1.
Diagnostic studies require a ready source of fundamental data. New measurements of the oscillator strengths of Mo(II)65,66 and V(II)67 lines were additions to this database. de Podesta et al.68 have revised an earlier estimate (2013) of the Boltzmann constant made by measuring the speed of sound in argon. They partly based this on a separate measurement of the molar mass of argon, by making precision comparison measurements of the IRs found in gravimetrically prepared argon against the ratios of Ar isotopes found in atmospheric air. A revised estimate of the Boltzmann constant of kB = 1.38064753(125) × 10−23 J K−1, with an uncertainty (k = 1) of 0.91 parts in 106, was computed.
While computational models are all very well, it is important to obtain confirmatory evidence by empirical study. Chan and Hieftje72 used time-resolved, 2D imaging of the load-coil region of an ICP to study the behaviour of single 50 μm diameter droplets as they passed through that region. Three wavelengths were observed in order to elucidate the effects on plasma conditions: 309.0 nm OH molecular band; 656.3 nm H(I) emission; and 696.5 nm Ar(I) emission. In the region of the droplet they observed plasma shrinkage due to a thermal pinch effect and heating upstream for up to 4 ms after passage of a vaporising droplet. They speculated that hydrogen from the droplet played a role in these effects due to its higher thermal conductivity compared with argon. They also observed significant plasma cooling up to 6 mm downstream from the droplet location, and a significant change in plasma impedance which lasted for 10 ms. As a consequence, if the droplet introduction rate is higher than 100 Hz, the perturbation in plasma impendence is unlikely to return to a steady-state level before arrival of the next droplet.
Further downstream of the ICP-MS sampling interface, single particle analysis requires fast detection of the transient signals, which might only last between 200 and 400 μs. Most instrument electronics have minimum dwell times of between 50 and 100 μs which limits the counting time and hence sensitivity for the analysis of particles less than 10 nm in diameter. A further problem is that the linear dynamic range is limited to ca. 150 counts per 50 μs dwell time, thus making the detection of fast transient signals something of a challenge. Shaw and Donard73 have overcome this problem by using a magnetic sector ICP-MS instrument with GHz ppm−1 sensitivity, using dwell times of a low as 10 μs. They achieved this by incorporating a physical attenuation grid, after the MS but before the detector, to reduce the intensity of the ion beam. Hence, it was possible to use a discrete dynode electron multiplier in pulse counting mode even for large ion counts. They used this system to monitor solutions of gold NPs of between 5 and 60 nm in diameter, with fast data acquisition up to 105 Hz and capable of measuring signals in excess of 3 × 107 cps. In a related study, Strenge and Engelhard74 developed a home-built data acquisition (DAQ) unit to address some of these problems in single-particle ICP-MS. The unit was capable of 5 μs dwell times during continuous data acquisition for virtually unlimited measurement time. Samples containing gold NPs with nominal sizes of 10 nm and 30 nm at different particle number concentrations were analysed using this system and compared with a standard DAQ. They found that the increased time resolution almost eliminated errors in monitoring single particle ion clouds, such as particle coincidence and split-particle events.
Temperature measurements and spatial diagnostics have long been favoured techniques for plasma characterisation, so inevitably some of the new miniaturised plasmas have now received this treatment. Krahling et al.75 determined Te and ne in a liquid electrode DBD using Stark broadening of Sr(II) 407.771 nm, Sr(II) 421.552 nm and Sr(I) 460.733 nm lines. They determined ne to be between 0.8 and 1.6 × 1016 cm−3 and Te > 1.1 eV. Unsurprisingly, Boltzmann plots of the OH rotational distribution deviated from thermal equilibrium. Kuklya et al.76 studied a low temperature He/N2 DBD used for ambient ionisation. They mapped the spatial distribution of various species in the plasma, but made particular mention of the decrease in N2+, thought to be an important intermediate for the formation of H3O+ and also proton transfer ionisation of analyte species. However, there was an excess of NO in a 0.6% nitrogen plasma, suggesting that charge transfer reactions involving NO+ formed by Penning ionisation might be significant in this type of plasma, though no empirical evidence was presented in the paper.
Burger and Hermann77 presented a method for the measurement of Stark broadening of atomic and ionic lines in a plasma produced by UV nanosecond laser ablation of calcium sulfate in argon at near atmospheric pressure. Spectral lines from Ca, O2 and several impurity elements were observed, simultaneously with the Hα transition, over a 6000 to 14000 K temperature range. The uniform nature of the ablated plasma aided the reproducible measurement of Stark broadening and the use of an echelle spectrometer of large resolving power allowed the recording of a large number of spectral lines. Borggren et al.78 have used diode lasers to excite fluorescence in a pre-mixed, low pressure, methane–air flame, thereby facilitating a two-line ratio method of temperature measurement using In as the thermometric species. The stated advantage was that it afforded 2D planar imaging with a spatial resolution of 210 μm, normally only possible with high power, pulsed lasers.
Sometimes, direct visual observation confirms the intuitive. Yu et al.79 used a high-speed camera to study an argon MPT source at various power and flow rates. This design mimics that of the more traditional ICP, so the observation that the cone shaped plasma has a rotational motion of ca. 100 Hz follows; as does the conclusion that this helps stabilise it in the presence of a central sample introduction gas flow.
Hattendorf et al.83 have studied interferences caused by doubly-charged, polyatomic Ar interferences in ICP-MS. They focused on the unexpected interference at m/z 63 and 64 caused by ArSr2+ and its effect on Zn and Cu IRA. They found that the same mass concentration of Sr altered the measured 63Cu:65Cu and 64Zn:66Zn isotope ratios by between −0.036‰ and −0.95‰. In addition, they also observed effects on IRs caused by: BaAr2+ on Sr+; MgAr2+ on S+; and CaAr2+ on Ca+. Wet sample introduction and lower carrier gas flow rate was found to reduce the interferences, but the authors noted that matrix removal prior to analysis may be a requirement to ensure accurate IRs.
Cheung et al.84 continued a recent theme which focused on prediction of matrix interferences in ICP-OES. However, in the paper they used the temporal nature of ICP-TOF-MS to monitor the time-dependent ratio of two ion signals, and used it to indicate and correct for mass-dependent matrix interferences. By injecting a discrete sample solution they were able to monitor the time-dependent dispersion of the aerosol. In the absence of matrix interference all species yielded the same concentration profiles, with matching signal profiles. However, in the presence of a matrix this was not the case, and signal ratios could be monitored to detect this. They studied the 51V+:55Mn+, 59Co+:107Ag+, 55Mn+:208Pb+, and 52Cr+:208Pb+ ratios and found that the ion pairs having the largest mass difference were best to flag up matrix interferences caused by heavy matrices such as Ba and U. In addition, the dilution factor necessary to minimise the interference could be identified by the point at which the ratio became constant.
In a somewhat philosophical paper, Andersen86 commented on the origin of uncertainty in analytical measurements. He examined the question of why some laboratories produce excellent results while others do not; and whether is it down to human error or inherent failings in the system. He suggests that lack of compliance can be explained largely by the latter rather than the former, and concluded that a consensus value should include any outliers. While this reviewer does not agree entirely with this analysis, it does hold out hope for the ‘ordinary’ practising analyst.
Several workers investigated plasma shielding effects and ablation processes at different operating conditions, such as underwater, ambient gas, pressure and temperatures. In particular, Pishdast et al.96 investigated, experimentally and numerically, the influence of plasma shielding induced by Nd:YAG laser irradiance at various pressures (ranging from 5 to 1000 mbar) and different atmospheres (e.g. Ar, He, Ne, and air), on the behavior of radiation intensity, SBR, and expansion of the plasma. Strong enhancement of Cu atomic emission lines due to increasing plasma temperature and density was observed at increasing laser irradiance, but saturation was observed at values above 5 GW cm−2. Simulation and experimental values of plasma plume expansion velocity, obtained using the absorption and scattering of a continuous He–Ne probe laser beam, showed that plume velocity was enhanced at increasing laser irradiance until it saturated due to plasma shielding and a reduction in effective laser target interaction. Temporal evolution of pressure, density, Te, Tion and velocity of different layers of plasma, were numerically calculated using hydrodynamic equations to confirm the experimental results.
El-Saeid et al.97 studied the effect of very low sample temperature (77 K) on LIBS spectral behavior and plasma parameters, under both atmospheric pressure and vacuum conditions. From the analysis of bronze alloy samples, it was observed that analyte emission and ablation rates were reduced when the samples were at low temperature. Plasma ne and Te were lower at low temperature and increased under vacuum conditions. LIBS analysis under extreme temperature conditions might be of interest for applications in planetary exploration. Laser ablation under vacuum conditions was also studied by Oderji et al.,98 who developed a model to describe the laser ablation of W, based on the non-equilibrium mechanism of explosive partial sublimation in the superheated zone of the sample surface. Vacuum conditions simulated the situation within a fusion reactor. During the irradiation of W only a portion of the lattice bonds were thought to be broken so a mixture of atoms and particles was generated. The mass of ablated particles was measured using two quartz crystal deposition monitor sensors located at different angles to the normal of the target surface, and compared with a theoretical estimate obtained using a heat conduction equation. The results suggested that ablated particles were free to disperse whereas atoms formed vapour plume which produced rarefaction waves on expansion on a vacuum.
Underwater LIBS has become a hot topic. Gavrilovic et al.99 investigated the spatial and temporal evolution of an underwater LIBS plasma, formed on an aluminium target, using fast photography, Schlieren imaging, shadowgraphy, and optical emission spectroscopy. Observation revealed that the plasma rapidly expanded and decayed immediately after the single laser pulse. The optical emission was characterised by an intense continuum component and large line-widths. However, at longer delays (>5 μs) another plasma phase, starting from the backward reheated target and lasting over tens of microseconds from the laser pulse, was observed. This secondary plasma, confined inside the expanded vapour cavity, was found to have significantly lower electron densities, resulting in emission spectra with an almost continuum-free component. Goueguel et al.100 reported the use of underwater LIBS for direct in situ measurements of CaCO3 dissolution at elevated pCO2 (e.g. up to 350 bar, which equates to depths of about 3500 m). Dissolution of CaCO3 was observed at increasing pCO2 (from 50 to 150 bar) but then remained nearly constant at higher pressures, which may be related to changes in pH. The authors thought that this method might provide a practical way to perform real-time measurements of elements released during carbonate dissolution resulting from the degradation of cement seals in geologic CO2 storage.
LIBS methods have been developed for the analysis of aerosols. Boudhib et al.101 demonstrated that calibration-free LIBS measurements provided accurate results for the compositional analyses of aerosols in a helium flux. The LIBS plasma was considered to be in partial LTE, in which the population number densities of plasma species, except He atoms and ions, followed Boltzmann equilibrium distributions. The authors claimed that this method could be applied to all types of low density aerosols, where reabsorption of spectral lines from vaporised atoms is negligible in the cold plasma peripheral zone.
Tandem-LIBS has been investigated as a way to improve analytical figures of merit. Viljanen et al.104 developed microwave assisted LIBS (MW-LIBS) working at atmospheric pressure conditions without employing an enclosed cavity. Signal enhancement was achieved by using integration times of hundreds of microseconds. The external microwave field was coupled into the plasma using a novel and simple near-field applicator. The experimental set-up was developed to avoid the complex process of sample loading and to provide improved temporal and spatial resolution. Jarvinen et al.105 employed electrodynamic balance trap (EDB)-LIBS to investigate the analysis of single water droplets, containing known amounts of Al, Mn and Pb. The dependence of signal on the level of analyte preconcentration was evaluated by varying the water content and the exact position of the particles. Emission signals became saturated after 6 s (i.e. after total evaporation) because even a small amount of water in the particle resulted in a significant reduction in the LIBS signal. Emission signals were also reduced when the trapped particle was out of the focal position. The authors scanned the particles across the focal spot of the laser beam, with a resolution of a few micrometers. This was claimed to provide means to improve the sensitivity and reproducibility of single particle LIBS analysis.
Determination of trace amounts of halogens in solid samples by LIBS is a challenging task due to the low excitation efficiency of these elements. Alvarez-Llamas et al.107 developed an atmospheric-air LIBS method, based on the detection of CaF molecular emission bands, for the determination of trace amounts of F in solid samples. Samples of copper, containing F concentrations between 50 and 600 μg g−1 and variable amounts of Ca, were used to demonstrate the linear relationships between CaF emission signal and F concentration. LODs for F determination in atmospheric-air LIBS were improved by more than 1 order of magnitude.
Several approaches for direct LIBS liquid analysis were published during the review period, highlighting the increased interest in this research field. Zhong et al.108 developed an ultrasonic nebuliser to improve LIBS capabilities for direct liquid quantitative analysis. An operational procedure was designed to enhance LIBS stability and repeatability for the analysis of Pb-containing solutions. A linear calibration curve, up to a Pb concentration of about 4000 μg g−1, for the background normalised Pb(II) emission line at 220.35 nm was obtained. De Giacomo et al.109 demonstrated the use of NELIBS for microdrop analysis at the sub-ppm level using single shot mode. The emission intensity of Ag(I) 328.1 nm, Li(I) 670.8 nm, and Pb(I) 405.7 nm increased when a microdrop (e.g. aqueous, protein and human serum solutions) was deposited on a glass substrate covered with gold NPs. The authors thought that the enhancement was due to field enhancement caused by coupling of the electromagnetic field of the laser with that induced on the NP surface plasmon. Other effects such as adsorption of analytes on the NP surface and increase of particle number density in the plasma phase might also have had an influence. These promising results highlight the potential capability of NELIBS on future medical and forensic science applications. The wavelength dependency of NELIBS was investigated by Sherbini et al.110 Three wavelengths from a Nd:YAG laser, at 1064 nm, 532 nm and 355 nm, were employed for the LIBS analysis of ZnO nanomaterial and bulk material. Enhanced emission signals and lower laser fluence thresholds were observed for the nanomaterial. The authors considered that lower laser fluence thresholds were due to a reduction in the bulk thermal conduction length to the size of the nanoparticles. Moreover, laser radiation dependent threshold fluence was found to vary with wavelength as 1/λ2.
This year Goderis et al.115 provided a significant review of isotopes in cosmochemistry. It covered the range of radiogenic, mass-dependent and mass-independent IR variation and provided very useful tables of information on the key isotopes of interest. Of particular interest was a schematic figure that depicted the key processes responsible for each stable isotope deviation and a comprehensive reference list across the subject area.
Horsky et al.116 evaluated the uncertainty of Sr isotope measurements by calculating the combined uncertainties inherent in three different instrumental mass fractionation strategies: internal normalisation to 86Sr:88Sr; sample-standard bracketing; and using Zr as a fractionation proxy. A conclusion from comprehensive propagation modelling was that natural variation in normalisation parameters expands relative uncertainties by a factor of two, meaning that instrumental fractionation corrections become the major contributor to overall uncertainty. Correction for mass fractionation and application of double spike protocols requires complex mathematical calculations. To assist with this, Zhang et al.117 produced a Matlab-based program named “IsotopeMaker”. This software provided a solution to all double spike systems, both radiogenic and stable, with four or more isotopes. It was also aimed at users of laser ablation MC-ICP-MS for whom it will perform data reduction and correct for interferences in Sr, Nd and Hf isotope determinations.
Laser ablation produces transient signals that often result in an IR drift through the course of measurements. Claverie et al.123 examined the relationship between detector response times on MC-ICP-MS and drift in IR. Detector response times were noticeably different between Faraday–Faraday combinations, in particular when signals changed rapidly at the start of ablation. By minimising the regression coefficient between coincident detector signals through an acquisition they were able to calculate the time lag between the detectors (or the order of 150 ms between ion counting and Faraday detectors). This produced a consistent 235U:238U ratio during the course of ablation of uranium particles. The method could be applied routinely to any LA IR analysis.
The effect of LA transient signals on IR was also investigated by Kimura et al.124 These workers examined the effect of changes in the intensity of Pb signal on the Pb IR generated by differences in the response of Faraday amplifiers. The study utilised the recently introduced 1013 Ω resistors and made comparisons with 1012 Ω and multiple ion counting detector combinations. After detector–amplifier response time correction, data generated using 1013 Ω resistors for 208Pb:206Pb in the 1.7 ppm Pb BHVO-2G reference glass achieved precisions of ±0.2% (2 sd). This was demonstrated to be a 2–3 fold improvement in precision relative to the 1012 Ω amplifiers. Zircon U:Pb geochronology by TIMS was the subject of a study by von Quadt et al.125 The study used 1013 Ω resistors to measure all isotopes except 204Pb which was assigned to an axial electron multiplier detector. Collector gains were completed using an Nd isotope standard. Results indicated that the high-impedance equipped Faraday collectors were capable of reproducibility at the 0.01% level.
Lead IR measurement by both 265 nm femtosecond and 213 nm nanosecond LA was investigated by Ohata et al.127 Instrumental mass fractionation on the MC-ICP-MS was corrected by introducing the SRM 981 reference solution via desolvation and a dual-sample introduction system. Both laser systems produced consistent results and demonstrated that application of a fractionation determined from the coincident solution measurement gave accurate Pb IR.
Calibration schemes for determination of Pb:U during zircon geochronology by SIMS were evaluated by Jeon et al.128 Of the various Pb/UO calibration schemes tested with reference zircon 91500, Pb/UO–UO2/UO showed the smallest mean uncertainty. The use of this scheme demonstrated that precision was much improved, but the age determined was not changed significantly. Sharpe and Fayek et al.129 investigated the mass bias corrections used in the U–Pb dating of uraninite by SIMS. They found that the level of mass bias varied as a function of Pb content of the mineral analysed, and developed a three-point calibration protocol based on different reference materials to correct bias in unknown materials. Errors in age determination were found to be as much as 130 Ma in uraninite of ∼500 Ma.
Thallium isotope measurement was the focus of a study by Nielsen et al.130 They examined the Tl-isotope variation across the chain of Aleutian volcanoes and found that ε205Tl changed to heavier ratios toward the west. This was taken to reflect the nature of the sedimentary material being subducted – more continental or mantle derived to the east and more pelagic or MnO-bearing to the west.
In order to remove the matrix prior to MC-ICP-MS analysis, Van Hoecke et al.132 devised a cation exchange scheme with 0.28 M HCl loading of <100 ng Li and elution of 0.5 mL fractions. This resulted in an external precision of ±0.2‰ for both carbonate and clay fractions of sedimentary material.
Magnesium is an abundant element in many geological materials, so Mg IR variation is a potential target for LA. Dai et al.133 coupled a femtosecond laser to MC-ICP-MS and investigated Mg isotope variation in geological reference materials in glass form. They concluded that reproducible δ25Mg and δ26Mg could be achieved by referencing to a solution standard providing the concentration ratio of the sample:standard was in the range 0.4–3.0 δ26Mg. The reproducibility was reported to be within ∼±0.2 for BCR-2G and BIR-1G. Vogl et al.134 characterised the absolute Mg isotope composition and atomic weights of European Reference Materials and related these to NIST SRM 980. Fractionation laws used to correct Mg isotope ratios were found to produce systematic bias, with the exponential law found to induce the smallest.
Sulfur isotopes have been traditionally measured by electron-ionisation gas source mass spectrometers. Typically these achieve δ34S reproducibility of ±0.2‰ but require mg levels of analyte. Because of the lower amount of sulfur required, Albalat et al.135 have investigated using MC-ICP-MS for δ34S on medical samples. Their study demonstrated that subtle variations in δ34S (±0.1‰) can be achieved with concentrations of approximately 300 ng mL−1. The medical application showed that there are detectable differences in sulfur IR between patients with and without liver cancer. Fu et al.136 also used MC-ICP-MS to measure sulfur isotopes, but via LA. The study examined a range of solid sulphide reference materials with the aim of enhancing sensitivity by optimising operational conditions and improving precision of sulfur IR. Their instrument was tested with standard cones as well as ‘X’ skimmer and ‘Jet’ sampling cones in combination with varied addition of Ar make-up gas and N2. Laser ablation is known to produce fewer hydride interferences compared with solution-based sample introduction, but these were still present in mass scans across the sulfur peaks in their study. Addition of 4 mL min−1 N2 was found to suppress hydride formation and, combined with measurement at medium resolution (∼5000), resulted in stable δ33S and δ34S with precision of ∼±0.4 (2 SD). A useful assessment was made of the relationship between signal intensity and measurement precision for each of the cone combinations, which provided a good guide to what can be achieved with different sulfur concentrations. Hauri et al.137 demonstrated the potential for sulfur isotope measurement by nano-SIMS. These workers were able to demonstrate long-term reproducibility of metal sulphide analysis of ±0.4 for δ33S. The technique was then used to demonstrate that measurements by nano-SIMS were capable of distinguishing mass-independent fractionation of sulfur isotopes generated by microbial sulfate reduction in the neoarchaean (∼2.7 Ga).
The potential for high precision K IR measurements was examined by Li et al.138 They used single-focusing ICP-MS with a collision cell that removed ArH+ at m/z 41 by reaction with He and D2 gas. Following cation chromatographic purification, the measurements resulted in precision of ±0.02% (2 sd) for 41K:39K on samples including rock reference materials and plant samples.
Measurement procedure and fractionation correction of Ca isotopes was the subject of a study by Naumenko-Dezes et al.139 They used TIMS to measure Ca SRM 915 and found that a modified exponential law fractionation correction produced internally consistent Ca IR across the mass range. It resulted in valid results across the range of fractionation conditions, including when the filament was strongly depleted following extensive ionisation.
Vanadium IR were investigated by Nielsen et al.140 using MC-ICP-MS. At medium resolution (∼4000) and with a combination of 1010 Ω and 1012 Ω resistors they achieved an external reproducibility of ±0.15‰ δ51V. This is similar performance to previous low resolution methods, but they used as little as 200 ng V per analysis.
Larsen et al.141 studied Cr IR measurements to quantify mass-dependent and mass independent fractionation from a chemical separation viewpoint. They identified the magnitude of stable isotope fractionation generated by the elution characteristics of CrIII species (Cr3+, CrCl2+, CrCl2+, CrCl3) and devised a chromatographic procedure that resulted in Cr recoveries in excess of 95%.
A study by Finlayson et al.142 set out to improve the precision of Fe IR in geological measured by MC-ICP-MS. Like many Fe isotope studies, these workers used a 57Fe–58Fe double spike to correct for instrumental mass fractionation. However, a novel aspect was the use of ion counting to measure 60Ni, to enable a more accurate determination of the isobaric 58Ni. This improved the reproducibility of 56Fe threefold. Further improvement was also made by the detection of transient NeAr polyatomic interference by the ion counting detector.
A method for Cu isotope measurement in geological materials was investigated by Hou et al.143 These authors deployed NIST SRM 944 gallium as an internal mass fractionation standard. Fractionation of 65Cu:63Cu in bracketed standards was quantified using 69Ga:71Ga and their average value corrected the Cu fractionation in the samples.
In order to understand the biogeochemical processes operating on Zn in seawater Samanta et al.144 developed an MC-ICP-MS protocol using a 67Zn–68Zn double spike added to the seawater prior to processing. Results indicated that there is a systematic change in Zr isotopes with ocean depth which were attributed to variation in biological activity.
Louvat et al.145 have examined the systematics of Br isotope measurement by MC-ICP-MS using high- and low-resolution mode, and made a comparison between three different introduction systems: spray chamber, direct injection and desolvation. Results in low resolution mode were found to produce higher precision than high resolution providing the 40Ar2H+ isobaric interference was minimised by tuning the mass spectrometer. Br solutions and salts gave reproducible δ81Br to better than ±0.25‰. Alternatively, Ma et al.146 used positive ionisation TIMS to determine Br isotopes from Cs2Br+ ions and reported an external reproducibility of <0.18‰ δ81Br.
Molybdenum isotopic measurements of geological samples were investigated by Liu et al.147 using MC-ICP-MS. The accuracy of Mo isotopes was compared following fractionation correction by double spiking and sample-standard bracketing. Both methods were found to give comparable results, but the double spike method produced better results for samples with less than 500 ng g−1 Mo. External precision for samples with between 10 and 100 ng g−1 Mo was found to be better than ±0.04% for δ98:95Mo. Nagai et al.148 investigated the potential for negative ionisation TIMS to measure Mo isotopes, by generating MoO3− ions from a rhenium filament loaded with La(NO3)3. Following a correction for oxygen isotope interferences they claimed that this method resulted in a 1.3 to 2.7 fold improvement in reproducibility, of ±10 μ95Mo, where μMoi = [(iMo/96Mo)sample/(iMo/96Mo)std − 1] × 106: normalized to 98Mo/96Moi = 1.413173 by using the exponential law. Worsham et al.149 also measured Mo isotopes by negative TIMS and found that careful oxide correction resulted in ∼2.4 times improvement in the precision of μ97Mo.
A technique for measuring Ru stable IR was developed by Hopp et al.150 This utilised a 98Ru–101Ru double spike added prior to sample digestion to accommodate instrumental mass fractionation and chromatographic fractionation. An effective separation method was performed by cation exchange followed by distillation of volatile Ru oxides. Analysed rock standards demonstrated that an external precision of ±0.05‰ for δ102:99Ru could be measured using MC-ICP-MS, and that this level of precision was sufficient to confirm that variations of approximately 1‰ δ102:99Ru existed between Ru standard solutions and natural chromite crystals.
Saji et al.151 reported Nd isotope measurements using MC-ICP-MS that examined mass-dependent isotope compositions of geological, meteoritic and reference materials. The high precision achieved (<3.5 ppm on all Nd isotope pairs) and high chemical recovery allowed a comparison of mass-dependent effects and potentially revealed the effects of a 146Nd nucleosynthetic anomaly.
Tungsten IR in reference materials were the analytical focus of Abraham et al.152 Following three-step anion chromatography, W isotopes were measured in high resolution by MC-ICP-MS, in a 0.2 M HNO3 to 0.1 M HF solution. Mass fractionation was accounted for using a 180W–183W double spike. External reproducibility of rock reference materials was determined to be ±0.05‰ of the δ186W parameter. Trinquier et al.153 used negative ionisation TIMS to measure W isotopes as WO3−. A problem was a mass-dependent oxygen isotope variation on the oxide ions at 182W and 184W. Corrections could be made on the 183W:184W ratio, but this assumed the tungsten ratio is itself constant. A method was employed to simultaneously monitor the 18O:16O and the W IR on an individual integration basis.
Mercury isotope analysis by MC-ICP-MS was the subject of a study by Rua-Ibarz et al.154 They investigated the effect of sample introduction using both pneumatic nebulisation and CV generation. Using combined sample-standard bracketing and Tl as mass fractionation correction, they were able to provide a long-term precision of better than 0.006%. Cold vapour generation was found to enhance Hg signal intensity by a factor of 20 compared to pneumatic nebulisation.
Esaka et al.156 used ICP-MS to measure individually dissolved U and Pu particles. They demonstrated that 240Pu:239Pu, 241Pu:239Pu and 242Pu:239Pu can be determined accurately in particles with U:Pu ranging from 1 to 70, provided a correction is made for 238UH. It was not possible to measure 238Pu:239Pu with good precision due to the high blank on m/z 238. Konegger-Kappel et al.157 measured Pu isotopes of particle samples by LA-MC-ICP-MS. They targeted material originating from the Chernobyl reactor and determined average values for 240Pu:239Pu and 242Pu:239Pu that were comparable with previously published data for the contamination incident. Hedberg et al.158 also evaluated nuclear forensic measurements of U particles but used multi-ion counting SIMS. They achieved precision for 235U:238U of 0.1% (1 sd) on reference materials with 10% 235U and ∼1.5% on ratios with the minor isotopes 234U and 236U in the U010 reference material.
Plutonium IR were determined by Isselhardt et al.159 using RIMS. This technique has the potential to allow isobar-free analysis of heavy elements without chemical purification. Tests with Pu deposited on metal surfaces yielded overall precision of 240Pu:239Pu better than 1.5% (2 sd).
High-resolution ICP-OES has been used to examine U and Pu isotopes by Krachler et al.160 They demonstrated the potential for this technique to quantify 238Pu, 239Pu and 242Pu. In addition161 this was shown to be an alternative to MC-ICP-MS for 234U:238Pu age dating. Buompane et al.162 examined the potential for measuring 236U–238U by AMS using uranium carbide relative to uranium oxide as molecular ions. Results indicated that when UC− ions are injected 238U backgrounds were significantly reduced relative to UO− or UC2−.
Paul et al.163 investigated new ionisation techniques for TIMS analysis of U and Pu. They used a polymeric material as sorbent to concentrate the actinides. These polymer sorbents were grafted to rhenium filaments by melting before measurement to determine U and Pu concentration. The advantage of this method was seen as providing a single-step preparation with reduced exposure of analytical personnel to radiation.
3D | Three dimensional |
AA | Atomic absorption |
AAS | Atomic absorption spectrometry |
ADI | Ambient desorption ionisation |
AES | Atomic emission spectrometry |
AF | Atomic fluorescence |
AF4 | Asymmetric flow field-flow fractionation |
AFM | Atomic force microscopy |
AFS | Atomic fluorescence spectrometry |
APDC | Ammonium pyrrolidine dithiocarbamate |
APGD | Atmospheric pressure glow discharge |
CCD | Charge coupled detector |
CCP | Capacitively coupled plasma |
CRM | Certified reference material |
CRS | Cavity ringdown spectroscopy |
CS | Continuum source |
CV | Cold vapour |
CVG | Chemical vapour generation |
DBD | Dielectric barrier discharge |
DC | Direct current |
DDW | Distilled deionised water |
DL | Diode laser |
DLTV | Diode laser thermal vaporisation |
DMA | Dimethylarsenic |
DOF-MS | Distance of flight mass spectrometry |
DOTA | 1,4,7,10-Tetraazacyclo-dodecane n,n′,n′′,n′′′-tetra acetic acid |
EDB-LIBS | Electrodynamic balance trap laser induced breakdown spectroscopy |
ES-MS | Electrospray mass spectrometry |
ETV | Electrothermal vaporisation |
ETV-AAS | Electrothermal vaporisation atomic absorption spectrometry |
ETV-ICP-MS | Electrothermal vaporisation inductively coupled plasma mass spectrometry |
EVG | Electrochemical vapour generation |
FAPA | Flowing atmospheric pressure afterglow |
FF | Flame furnace |
FI | Flow injection |
FWHM | Full width at half maximum |
GD | Glow discharge |
GD-MS | Glow discharge mass spectrometry |
GD-OES | Glow discharge optical emission spectrometry |
GF-AAS | Graphite furnace atomic absorption spectrometry |
HG-AAS | Hydride generation atomic absorption spectrometry |
HG-AFS | Hydride generation atomic fluorescence spectrometry |
HPLC-ICP-MS | High performance liquid chromatography inductively coupled plasma mass spectrometry |
HR | High resolution |
hTISIS | Heated torch integrated sample introduction system |
HV | High voltage |
ICP-AES | Inductively coupled plasma atomic emission spectrometry |
ICP-DOF-MS | Inductively coupled plasma distance of flight mass spectrometry |
ICP-MS-MS | Inductively coupled plasma multicollector mass spectrometry |
ICP-MS | Inductively coupled plasma mass spectrometry |
ICP-MS/MS | Triple quadrupole inductively coupled plasma mass spectrometry |
ICP-OES | Inductively coupled plasma optical emission spectrometry |
ICP-QMS | Inductively coupled plasma quadrupole mass spectrometry |
ICP-QQQ-MS | Inductively coupled plasma triple quadrupole mass spectrometry |
ICP-TOF-MS | Inductively coupled plasma time-of-flight mass spectrometry |
ID | Isotope dilution |
IDA | Isotope dilution analysis |
ID-ICP-MS | Isotope dilution inductively coupled plasma mass spectrometry |
ID-MRM-MS | Isotope dilution multiple reaction monitoring mass spectrometry |
ID-MS | Isotope dilution mass spectrometry |
IL | Ionic liquid |
IRMS | Isotope ratio mass spectrometry |
LA | Laser ablation |
LA-ICP-MS | Laser ablation inductively coupled plasma mass spectrometry |
LA-MC-ICP-MS | Laser ablation multicollector inductively coupled plasma mass spectrometry |
LAMIS | Laser ablation molecular isotopic spectrometry |
LC | Liquid chromatography |
LEP | Liquid electrode microplasma |
LIBS | Laser induced breakdown spectroscopy |
LIF | Laser induced fluorescence |
LOD | Limit of detection |
LPME | Liquid phase microextraction |
LTP | Low temperature plasma |
MALDI | Matrix-assisted laser desorption ionisation |
MC-ICP-MS | Multicollector inductively coupled plasma mass spectrometry |
MIP | Microwave induced plasma |
MMA | Monomethylarsenic |
MNP | Magnetic nanoparticle |
MPT | Microwave plasma torch |
MW-LIBS | Microwave assisted LIBS |
Nd:YAG | Neodymium doped:yttrium aluminum garnet |
n e | Electron number density |
NELIBS | Nanoparticle enhanced LIBS |
NP | Nanoparticles |
od | Outer diameter |
OPO | Optical parametric oscillator |
PDMS | Polydimethylsiloxane |
PFH | Perfluorohexane |
PLS | Partial least squares |
PN | Pneumatic nebuliser |
ppb | Parts per billion (10−9) |
ppm | Parts per million (10−6) |
ppq | Parts per quadrillion (10−15) |
ppt | Parts per trillion (10−12) |
PVG | Photochemical vapour generation |
Q | Quadrupole |
QTF | Quartz tube furnace |
RF | Radiofrequency |
RIMS | Resonance ionisation mass spectrometry |
RSD | Relative standard deviation |
RVM | Relevance vector machine |
SALD | Substrate assisted laser desorption |
Sat-CRDS | Saturated-absorption CRDS |
SBR | Signal-to-background ratio |
SCGD | Solution cathode glow discharge |
SNR | Signal-to-noise ratio |
SP | Single particle |
SPME | Solid phase microextraction |
TDLAAS | Tunable diode laser atomic absorption spectroscopy |
T e | Electron temperature |
T gas | Gas temperature |
TIMS | Thermal ionization mass spectrometry |
T ion | Ionization temperature |
TOF | Time-of-flight |
T rot | Rotational temperature |
UV | Ultraviolet |
VG | Vapour generation |
This journal is © The Royal Society of Chemistry 2017 |