{"title":"Cl, Br and I measurements in rock samples by ICP-MS/MS using reaction gases","authors":"Benoît Villemant , Julie Noël , Benoît Caron","doi":"10.1016/j.chemgeo.2025.122681","DOIUrl":null,"url":null,"abstract":"<div><div>Analysis of chlorine (Cl), bromine (Br) and iodine (I) in poorly concentrated geological materials remains a major analytical challenge. Analysis of halogens extracted in solution using single quadrupole ICP-MS is highly sensitive but suffers from numerous mass interferences. Experimental determination of species potentially interfering with halogens when analyzing silicates shows that mass interferences with <sup>35</sup>Cl are low (<1 % of the <sup>35</sup>Cl signal) but that <sup>37</sup>Cl signal is completely hidden by <sup>19</sup>F- oxides and <sup>1</sup>H<img><sup>36</sup>Ar signals. Mass interferences with Br isotopes signals may be up to 20 times higher in Br-poor, K-rich or REE-rich samples: they are mainly due to [<sup>40</sup>Ar<sup>39</sup>K]<sup>+</sup> and [<sup>158</sup>Gd]<sup>++</sup> for <sup>79</sup>Br and to [<sup>162</sup>Dy]<sup>++</sup> for <sup>81</sup>Br. Due to the low abundance of <sup>127</sup>I, mass interferences are always significant and mainly due to argides and chlorides: [<sup>36</sup>Ar<sup>91</sup>Zr]<sup>+</sup>, [<sup>38</sup>Ar<sup>89</sup>Y]<sup>+</sup>, [<sup>40</sup>Ar<sup>87</sup>Rb]<sup>+</sup>, [<sup>40</sup>Ar<sup>87</sup>Sr]<sup>+</sup>, [<sup>35</sup>Cl<sup>92</sup>Zr]<sup>+</sup>, [<sup>37</sup>Cl<sup>90</sup>Zr]<sup>+</sup>. In addition, matrix effects combined to solvent molarity (NH<sub>4</sub>OH or HNO<sub>3</sub>) may significantly affect halogens ionisation leading to possible systematic bias in halogens analysis. The use of a triple quadrupole mass spectrometer (ICP-MS/MS) with H<sub>2</sub> and N<sub>2</sub>O reactions/collision gases allows the reduction of all interferences and matrix effects to values lower than analytical errors. <sup>35</sup>Cl and <sup>37</sup>Cl are measured through the reactant species ClH<sub>2</sub><sup>+</sup> in H<sub>2</sub> reaction mode, and <sup>79</sup>Br rand <sup>81</sup>Br are measured through BrO<sup>+</sup> species in N<sub>2</sub>O reaction mode. <sup>127</sup>I is measured in N<sub>2</sub>O collision mode that slightly reduces argides and chlorides species and significantly increases the <sup>127</sup>I signal by collision focusing.</div><div>Sample digestion in NH<sub>4</sub>HF<sub>2</sub> and dissolution of the residue in NH<sub>4</sub>OH (He et al., 2019) allow a simple and complete recovery of all halogens. Combined with ICP-MS/MS and gas reactions, the technique improves the precision and detection limits of halogen measurements by an order-of-magnitude compared to the currently reported performances of single quadrupole ICP-MS measurements. A set of international standard reference materials (ISRM) that cover a large range of halogen compositions are analysed: basalts BIR-1, BCR-1, BHVO-2, andesites AGV-1 and AGV-2, rhyolites RGM-1, ATHO and JR-1, minerals, marine sediment, soil, copper deposit and NIST-610 and -612 glass standards.</div></div>","PeriodicalId":9847,"journal":{"name":"Chemical Geology","volume":"681 ","pages":"Article 122681"},"PeriodicalIF":3.6000,"publicationDate":"2025-02-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemical Geology","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0009254125000713","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
Analysis of chlorine (Cl), bromine (Br) and iodine (I) in poorly concentrated geological materials remains a major analytical challenge. Analysis of halogens extracted in solution using single quadrupole ICP-MS is highly sensitive but suffers from numerous mass interferences. Experimental determination of species potentially interfering with halogens when analyzing silicates shows that mass interferences with 35Cl are low (<1 % of the 35Cl signal) but that 37Cl signal is completely hidden by 19F- oxides and 1H36Ar signals. Mass interferences with Br isotopes signals may be up to 20 times higher in Br-poor, K-rich or REE-rich samples: they are mainly due to [40Ar39K]+ and [158Gd]++ for 79Br and to [162Dy]++ for 81Br. Due to the low abundance of 127I, mass interferences are always significant and mainly due to argides and chlorides: [36Ar91Zr]+, [38Ar89Y]+, [40Ar87Rb]+, [40Ar87Sr]+, [35Cl92Zr]+, [37Cl90Zr]+. In addition, matrix effects combined to solvent molarity (NH4OH or HNO3) may significantly affect halogens ionisation leading to possible systematic bias in halogens analysis. The use of a triple quadrupole mass spectrometer (ICP-MS/MS) with H2 and N2O reactions/collision gases allows the reduction of all interferences and matrix effects to values lower than analytical errors. 35Cl and 37Cl are measured through the reactant species ClH2+ in H2 reaction mode, and 79Br rand 81Br are measured through BrO+ species in N2O reaction mode. 127I is measured in N2O collision mode that slightly reduces argides and chlorides species and significantly increases the 127I signal by collision focusing.
Sample digestion in NH4HF2 and dissolution of the residue in NH4OH (He et al., 2019) allow a simple and complete recovery of all halogens. Combined with ICP-MS/MS and gas reactions, the technique improves the precision and detection limits of halogen measurements by an order-of-magnitude compared to the currently reported performances of single quadrupole ICP-MS measurements. A set of international standard reference materials (ISRM) that cover a large range of halogen compositions are analysed: basalts BIR-1, BCR-1, BHVO-2, andesites AGV-1 and AGV-2, rhyolites RGM-1, ATHO and JR-1, minerals, marine sediment, soil, copper deposit and NIST-610 and -612 glass standards.
期刊介绍:
Chemical Geology is an international journal that publishes original research papers on isotopic and elemental geochemistry, geochronology and cosmochemistry.
The Journal focuses on chemical processes in igneous, metamorphic, and sedimentary petrology, low- and high-temperature aqueous solutions, biogeochemistry, the environment and cosmochemistry.
Papers that are field, experimentally, or computationally based are appropriate if they are of broad international interest. The Journal generally does not publish papers that are primarily of regional or local interest, or which are primarily focused on remediation and applied geochemistry.
The Journal also welcomes innovative papers dealing with significant analytical advances that are of wide interest in the community and extend significantly beyond the scope of what would be included in the methods section of a standard research paper.