红酒中的~(87)Sr/~(86)Sr同位素比测定

研究了多接收电感耦合等离子体质谱(MC-ICP-MS)测定红酒样品中87Sr/86Sr同位素比的分析方法,并用建立的分离测定方法参加了欧洲参考物质与测量研究所(IRMM)组织的CCQM-P105国际比对,即红酒中87Sr/86Sr同位素比的分析比对.红酒样品经微波消解后,采用Dowex 50W×8树脂分离纯化锶,用MC-ICP-MS精确测定锶组分中的87Sr/86Sr同位素比,同时对测量结果的不确定度进行了分析和评定.     

人牙齿中锶的特效树脂分离及其同位素测定

采用锶特效树脂(Sr-Spec)建立了快速分离富集人牙齿中微量元素锶,并测定87Sr/86Sr的有效方法。采用HNO3-HClO4体系消解牙齿样品,以8mol/L HNO3为介质上柱,8mol/L HNO3淋洗,0.05mol/LHNO3洗脱,收集淋洗液,蒸干;采用正热电离质谱法进行87Sr/86Sr的测定。结果表明,利用Sr-Spec树脂,不仅能将锶与基质中大量钙分离,并能有效分离同位素测定中干扰元素铷。本方法可以缩短分离时间,提高分离效率,减少试剂用量,降低实验空白。采用本方法对陕南地区人牙齿牙釉质中锶进行分离,测得的87Sr/86Sr值在0.710948～0.711037之间。     

肉类制品中微量锶的分离及^87Sr/^86Sr同位素比值测定

利用87Sr/86Sr同位素比值进行生物和古人类源区与迁徙的示踪是Sr同位素技术应用的新领域,也是考古研究和肉类食品溯源研究的新尝试。本研究对牛肉干粉采用酸溶、微波消解和灰化后硝酸提取等不同方法进行消解,比较了它们的离子交换分离效果和Sr同位素测定结果;用石英、石墨和瓷坩埚3种器皿对牛肉干粉进行灰化,检测了灰化器皿对87Sr/86Sr同位素比值的影响,从而确定了石英坩埚灰化的消解方法,建立了适合于肉类制品微量Sr的化学分离方法与87Sr/86Sr同位素比值测定方法。本方法包括肉类制品的石英坩埚灰化、离子交换分离和87Sr/86Sr比值的热离子化质谱测定。所建方法对肉类食品溯源和考古研究等领域富含有机质样品的Sr同位素比值测定具有普适性。     

贝类体内麻痹性贝类毒素的提取方法研究

采用浓度系列为0.04、0.07、0.10、0.15、0.20、0.25、0.30、0.40、0.50、0.70、1.0 mol/L的HCl和HAc溶液作为提取液,分别取10 mL提取液与10 g栉孔扇贝性腺混合,在沸水浴中加热5 min提取麻痹性贝类毒素(PSP);同时采用0.3 mol/L HAc和0.2 mol/L HCl,于冰水浴中进行超声波提取麻痹性贝类毒素5~30 min。提取完成后将混合物于4℃冷冻离心机内离心5 min(3500 r/min),取上清液并以0.1 mol/L NaOH或5 mol/L HCl调整至pH为2.0~4.0。经超滤膜过滤后的提取液以高效液相色谱柱后衍生荧光检测法进行毒素分析,研究毒素组分间的转化关系和提取效率,并与超声波提取法进行了比较。结果表明,采用0.04~0.25 mol/L HCl和0.04~1.0 mol/L HAc从贝肉中提取PSP毒素,各毒素组分浓度差异不大,当HCl浓度大于0.25 mol/L时,N-磺酰氨甲酰基类毒素C1浓度急剧降低,HCl浓度大于0.5 mol/L时,N-磺酰氨甲酰基类毒素C2和GTX5浓度急剧降低,三者在酸度过大的情况下分解或转化为膝沟藻毒素-2(GTX2),膝沟藻毒素-3(GTX3)和石房蛤毒素(STX)。在相同浓度酸的情况下,超声波提取液中C1毒素的浓度显著低于沸水浴提取法,但C2的浓度略高于沸水浴提取液。     

锶特效树脂萃取色谱耦合热电离同位素质谱法测定海水中锶同位素研究

采用锶特效树脂,以萃取色谱法将锶离子自基体中分离,详细介绍了锶特效树脂萃取原理,进行了实验条件优化。采用HNO3消解海水样品,以HNO3(8.0mol/L)为介质上柱,用HNO3(8.0mol/L)淋洗,样品中的锶离子被强烈吸附在树脂柱上,再以HNO3(0.05mol/L)洗脱,Sr被解吸。收集淋洗液,蒸干,采用热电离同位素质谱仪测定海水样品中的87Sr/86Sr比值。结果表明,利用锶特效树脂,可将锶与基体元素(K,Na,Mg,Ba)分离,并能有效分离同位素测定中干扰元素Ca和Rb。消除了基体干扰,提高了分离效率,达到灵敏测定。     

利用锶特效树脂分离富集岩石样品中的锶及测定~(87)Sr/~(86)Sr

本研究以Sr-Spec树脂作为分离锶的特效树脂,以HNO3为淋洗液,通过改变HNO3的浓度,将地质岩石样品中的锶分离富集.实验结果表明,Sr与基质元素和Rb能很好地分离.利用Sr-Spec树脂分离国际标准物质SRM607、日本岩石标样JA-2、JB-2、JF-2和国家标准物质GBW04111后, 测得同位素比值87Sr/86Sr结果及误差(2σ)分别为1.200660±22, 0.706350±17, 0.703640±16, 0.709692±22和0.700008±23.相对于常规的阳离子树脂分离方法,此方法所用淋洗试剂量少,分离流程短,可以降低实验空白并提高工作效率.因此,Sr-Spec树脂分离法是快速分离富集不同岩性地质样品的Sr并测定87Sr/86Sr的有效方法.     

电感耦合等离子体质谱(ICP-MS)法测定水产品中锶同位素比值

为推动锶同位素在水产品溯源中的应用,本文建立了基于电感耦合等离子体质谱法（ICP-MS）测定水产品中锶同位素比值的分析方法。水产品组织经冻干研磨和微波消解后,用ICP-MS测定样品溶液中的锶同位素比值,并采用标准品-样品-标准品交叉测量方法降低质量歧视效应的影响。结果表明,通过稀释样品消解溶液,将总锶浓度控制在70-100 μg/L,并与80 μg/L的锶同位素标准品溶液进行交叉测量,可准确校正质量歧视效应;84Sr/86Sr、87Sr/86Sr和88Sr/86Sr的日内精密度分别为0.06%、0.03%和0.03%,日间精密度分别为0.08%、0.04%和0.03%;按照所建立的方法测定大虾和扇贝生物成分分析标准物质的锶同位素比值,84Sr/86Sr、87Sr/86Sr和88Sr/86Sr的相对标准偏差均低于0.1%。该方法前处理简单快捷并且测量精密度高,可为锶同位素比值测定并进一步应用于水产品溯源研究提供技术支撑。     

微波消解-电感耦合等离子体原子发射光谱法同时测定碳酸盐岩中Ca、Mg、Sr、Ba等13种元素

为了探索碳酸盐岩主量元素和部分微量元素的同时准确测定方法,选用微波消解法,考察了HNO₃-HF、HNO₃-H₂O₂、HNO₃-HCl、HNO₃-HF-H₂O₂和HNO₃-HCl-HF-H₂O₂5种不同的溶样体系对碳酸盐岩样品的消解情况,通过选择各元素合适的分析谱线,进行标准溶液的高钙基体匹配,建立了电感耦合等离子体原子发射光谱(ICP-AES)法同时测定其中的主量元素Ca、Mg、Al、Fe、K和微量元素Mn、Sr、Ba、V、Cu、Cr、Ni、Li含量的方法。结果表明,HNO₃-HF-H₂O₂三酸溶样体系消解更彻底,方法的标准曲线线性相关系数均不小于0.999,方法检出限为0.000 2～1.10μg/mL,测定值的相对标准偏差为0.10%～9.6%,测定值与标准值基本一致。方法用于古...     

锶稳定同位素比质谱在进口大麦原产地溯源中的应用研究

利用热电离质谱检测了进口自加拿大、法国、澳大利亚和美国的大麦样本的⁸⁷Sr/⁸⁶Sr同位素比值。研究了TIMS测定进口大麦⁸⁷Sr/⁸⁶Sr同位素比值的精密度，利用SPSS 25.0对不同进口国大麦样本的⁸⁷Sr/⁸⁶Sr同位素比值进行了正态性验证、置信区间分析、方差分析和事后多重比较。结果表明：TIMS技术测定进口大麦⁸⁷Sr/⁸⁶Sr同位素比值日内精密度和日间精密度分别达到0.003 59%和0.010 20%;不同进口国的大麦样本⁸⁷Sr/⁸⁶Sr同位素比值成正态分布，置信区间分析、方差分析以及事后多重比较都显示不同进口国大麦⁸⁷Sr/⁸⁶Sr同位素比值间具有显著性差异，可以利用TIMS测定大麦中的⁸⁷Sr/⁸⁶Sr同位素比值并进行进口国溯源。     

用萃取-氢化物发生-原子荧光光谱法测定海带中的无机砷

利用无机砷在强酸性下能溶于氯仿,在弱酸性下能溶于水的特点,将其与其他干扰物质分离,采用氢化物发生-原子荧光光谱法测定海带中的无机砷.利用9mol/L HCl溶解海带样品后用三氯甲烷萃取其中的无机砷,再反萃取于1 mol/L HCl溶液中,干燥-消化后,用氢化物发生-原子荧光光谱法测定其中无机砷的含量.重要干扰物-二甲基亚砷酸不会被同时萃取,方法的回收率在80%以上.     

The determination and application of 87Sr/86Sr ratio in verifying geographical origin of wheat

As ⁸⁷Sr/⁸⁶Sr ratio plays a significant role in authenticating the geographical origin of foodstuff, it is important to identify where the ⁸⁷Sr/⁸⁶Sr signature in food comes from, and the methods of ⁸⁷Sr/⁸⁶Sr ratio analysis in food and environmental samples. Wheat with three genotypes, soil and groundwater samples were collected from three regions of China during harvest time of 2014. The ⁸⁷Sr/⁸⁶Sr ratios in the samples were determined by thermal ionization mass spectrometer in order to investigate the possible source of ⁸⁷Sr/⁸⁶Sr in wheat, and the concentrations of Rb and Sr in wheat and soils were also detected by inductively coupled plasma mass spectrometry and combined with ⁸⁷Sr/⁸⁶Sr ratio in order to trace the geographical origin of wheat. The ⁸⁷Sr/⁸⁶Sr ratio, the contents Rb and Sr, and Rb/Sr ratio of wheat and soil samples showed significant differences among three regions. The ⁸⁷Sr/⁸⁶Sr ratios and the concentrations of Rb and Sr in soils were higher than those in corresponding wheat. The ⁸⁷Sr/⁸⁶Sr ratio in wheat was identical to that corresponding soil NH₄NO₃ extracts (labile fraction of soil) and groundwater. Wheat uptake more Rb than Sr. 3D distribution of ⁸⁷Sr/⁸⁶Sr, Rb and Sr could identify wheat samples from different regions clearly. The ⁸⁷Sr/⁸⁶Sr ratio of wheat reflects the ⁸⁷Sr/⁸⁶Sr ratio of the associated environment including soil and groundwater. It is expected that the use the parameters of ⁸⁷Sr/⁸⁶Sr ratio, the contents of Rb and Sr will allow to trace geographical origin of wheat. Copyright © 2017 John Wiley & Sons, Ltd.     

Specificity and Origin of the Stability of the Sr Isotopic Ratio in Champagne Wines

The ⁸⁷Sr/⁸⁶Sr ratio of 39 Champagnes from six different brands, originating from the whole “Appellation d’Origine Contrôlée” (AOC) Champagne was analyzed to establish a possible relation with the geographical origin. Musts (i.e., grape juice) and base wines were also analyzed to study the evolution of the Sr isotopic ratio during the elaboration process of sparkling wine. The results demonstrate that there is a very homogeneous Sr isotopic ratio (⁸⁷Sr/⁸⁶Sr = 0.70812, n = 37) and a narrow span of variability (2σ = 0.00007, n = 37). Moreover, the Sr concentrations in Champagnes have also low variability, which can be in part explained by the homogeneity of the bedrock in the AOC Champagne. Measurements of the ⁸⁷Sr/⁸⁶Sr ratio from musts and base wines show that blending during Champagne production plays a major role in the limited variability observed. Further, the ⁸⁷Sr/⁸⁶Sr of the musts were closely linked to the ⁸⁷Sr/⁸⁶Sr ratio of the vineyard soil. It appears that the ⁸⁷Sr/⁸⁶Sr of the product does not change during the elaboration process, but its variability decreases throughout the process due to blending. Both the homogeneity of the soil composition in the Champagne AOC and the blending process during the wine making process with several blending steps at different stages account for the unique and stable Sr isotopic signature of the Champagne wines.     

Isotope analysis of strontium by multicollector inductively-coupled plasma mass spectrometry: High-precision combined measurement of 88Sr/86Sr and 87Sr/86Sr isotope ratios

The paper describes a new high-precision method for the simultaneous precise determination of ⁸⁸Sr/⁸⁶Sr and ⁸⁷Sr/⁸⁶Sr ratios in a single portion of a geological sample by multicollector inductively coupled mass spectrometry (MC-ICP-MS). The isotope analysis is carried out with mass bias effect correction by a combination of internal normalization to the standard Zr-isotope ratio and bracketing standard method (external normalization). Our results for geochemical IAPSO and BCR-1 standard samples are in a good agreement with the published data. The reproducibility of the ⁸⁸Sr/⁸⁶Sr ratio varies from ±0.015 to ±0.05?? (depending on the sample features) and, together with the analysis accuracy, is superior to the previously reported methods of MC-ICP-MS analysis. Still ahead is only double spike thermal ionization mass spectrometry with its ±0.02?? reproducibility. However, the new method allows the simultaneous determination of ⁸⁸Sr/⁸⁶Sr and ⁸⁷Sr/⁸⁶Sr ratios and its productivity is higher by 5 to 6 times. On the other hand, in sample preparation, it is necessary to strive for at least 95% Sr yield from the chromatographic column; otherwise the sorption-desorption process may lead to a 0.6?? ⁸⁸Sr/⁸⁶Sr ratio bias relative to the true value.     

Problems in obtaining precise and accurate Sr isotope analysis from geological materials using laser ablation MC-ICPMS

This paper reviews the problems encountered in eleven studies of Sr isotope analysis using laser ablation multicollector inductively coupled plasma mass spectrometry (LA-MC-ICPMS) in the period 1995–2006. This technique has been shown to have great potential, but the accuracy and precision are limited by: (1) large instrumental mass discrimination, (2) laser-induced isotopic and elemental fractionations and (3) molecular interferences. The most important isobaric interferences are Kr and Rb, whereas Ca dimer/argides and doubly charged rare earth elements (REE) are limited to sample materials which contain substantial amounts of these elements. With modern laser (193 nm) and MC-ICPMS equipment, minerals with >500 ppm Sr content can be analysed with a precision of better than 100 ppm and a spatial resolution (spot size) of approximately 100 μm. The LA MC-ICPMS analysis of ⁸⁷Sr/⁸⁶Sr of both carbonate material and plagioclase is successful in all reported studies, although the higher ⁸⁴Sr/⁸⁶Sr ratios do suggest in some cases an influence of Ca dimer and/or argides. High Rb/Sr (>0.01) materials have been successfully analysed by carefully measuring the ⁸⁵Rb/⁸⁷Rb in standard material and by applying the standard-sample bracketing method for accurate Rb corrections. However, published LA-MC-ICPMS data on clinopyroxene, apatite and sphene records differences when compared with ⁸⁷Sr/⁸⁶Sr measured by thermal ionisation mass spectrometry (TIMS) and solution MC-ICPMS. This suggests that further studies are required to ensure that the most optimal correction methods are applied for all isobaric interferences.     

High-precision direct determination of the Sr/Sr isotope ratio of bottled Sr-rich natural mineral drinking water using multiple collector inductively coupled plasma mass spectrometry

We describe a precise and accurate method for the direct determination of the ⁸⁷Sr/⁸⁶Sr isotope ratio of bottled Sr-rich natural mineral drinking water using multiple collector inductively coupled plasma mass spectrometry (MC-ICP-MS). The method is validated by the comparative analysis of the same water with and without cation-exchange resin purification. The work indicates that isobarically interfering elements can be corrected for when ⁸⁷Rb/⁸⁶Sr < 0.05 (Rb/Sr < 0.015), and that the matrix elements (Ca, Mg, K and Na) have no significant effect on the accuracy of the Sr isotope data. The method is simple, rapid, eliminates sample preparation time, and avoids potential contamination during complicated sample-preparation procedures. Therefore, the high sample throughput inherent to the MC-ICP-MS can be fully exploited.     

Simultaneous determination of mass-dependent isotopic fractionation and radiogenic isotope variation of strontium in geochemical samples by multiple collector-ICP-mass spectrometry.

We present a method to determine (88)Sr/(86)Sr and (87)Sr/(86)Sr simultaneously. The former variation reflects the mass-dependent isotopic fractionation through the physico-chemical processes, and the latter originates from beta(-)-decay of the parent nuclide (87)Rb as well as the mass-dependent isotopic fractionation. In order to determine the mass-dependent isotopic fractionation, the mass-discrimination effect on (88)Sr/(86)Sr was externally corrected by an exponential law using Zr. For the radiogenic growth of (87)Sr/(86)Sr, the mass-dependent isotopic fractionation effect on (87)Sr/(86)Sr was corrected by a conventional correction technique using the (88)Sr/(86)Sr ratio. The reproducibility of the (88)Sr/(86)Sr and (87)Sr/(86)Sr measurements for a high-purity Sr chemical reagent was 0.06 per thousand (2SD, n = 20) and 0.07 per thousand (2SD, n = 20), respectively. Strontium isotopic ratios ((88)Sr/(86)Sr and (87)Sr/(86)Sr) were measured on six geochemical reference materials (igneous rock: JB-1a and JA-2; carbonate mineral: JLs-1, JDo-1, JCp-1 and JCt-1) and one seawater sample. The resulting (87)Sr/(86)Sr ratios obtained here were consistent with previously published data within the analytical uncertainties. The resulting (88)Sr/(86)Sr ratios for igneous rock samples did not vary significantly within the samples, whereas the carbonate samples showed enrichments of the lighter Sr isotopes over the seawater sample. The (88)Sr/(86)Sr ratio of geochemical samples could reflect the physico-chemical processes for the sample formation. Also, a combined discussion of (88)Sr/(86)Sr and (87)Sr/(86)Sr of samples will render multi-dimensional information on geochemical processes.     

Rapid and precise determination of Sr and Nd isotopic ratios in geological samples from the same filament loading by thermal ionization mass spectrometry employing a single-step separation scheme

Thermal ionization mass spectrometry (TIMS) offers the excellent precision and accuracy of the Sr and Nd isotopic ratio analysis for geological samples, but this method is labour intensive, expensive and time-consuming. In this study, a new analytical protocol by TIMS is presented that aims at improving analytical efficiency and cutting down experimental cost. Using the single-step cation exchange resin technique, mixed Sr and rare earth elements (REEs) fractions were separated from matrix and evaporated to dryness. Afterwards, mixed Sr + REEs fractions were dissolved and loaded onto the same Re filament using 1 μL of 2 M HCl. Then, Sr and Nd were sequentially measured without venting using TIMS. In contrast to conventional TIMS methods, the merits of this analytical protocol are its cost- and time-saving adaptations. The applicability of our method is evaluated by replicated measurements of ⁸⁷Sr/⁸⁶Sr and ¹⁴³Nd/¹⁴⁴Nd for nine international silicate rock reference materials, spanning a wide range of bulk compositions. The typical internal precision in this study is ca. 0.001% (RSE) for ⁸⁷Sr/⁸⁶Sr and ¹⁴³Nd/¹⁴⁴Nd; the analytical results obtained for these standard rocks show a good agreement with reported values, indicating the effectiveness of the proposed method.     

Strontium isotope ratios (87Sr/86Sr) of tooth enamel: a comparison of solution and laser ablation multicollector inductively coupled plasma mass spectrometry methods

Strontium isotope ratios (87Sr/86Sr) in tooth enamel provide a means to investigate migration and landscape use in humans and other animals. Established methods for measuring (87)Sr/(86)Sr in teeth use bulk sampling (5-20 mg) and labor-intensive elemental purification procedures before analysis by either thermal ionization mass spectrometry (TIMS) or multicollector inductively coupled plasma mass spectrometry (MC-ICP-MS). Another method for measuring 87Sr/86Sr is laser ablation MC-ICP-MS, but concerns have been expressed about its accuracy for measuring tooth enamel. In this study we test the precision and accuracy of the technique by analyzing 30 modern rodent teeth from the Sterkfontein Valley, South Africa by laser ablation MC-ICP-MS and solution MC-ICP-MS. The results show a mean difference in 87Sr/86Sr measured by laser ablation and by solution of 0.0003 +/- 0.0002. This degree of precision is well within the margin necessary for investigating the potential geographic origins of humans or animals in many areas of the world. Because laser ablation is faster, less expensive, and less destructive than bulk sampling solution methods, it opens the possibility for conducting 87Sr/86Sr analyses of intra-tooth samples and small and/or rare specimens such as micromammal and fossil teeth.