电感耦合等离子体质谱法测定水泥样品中的铅同位素比值

研究和讨论了用电感耦合等离子体质谱仪(ICP—MS)测定铅的同位素比值测定时，影响测试结果的准确度和精密度的主要因素及其优化过程。在优化后的仪器分析条件下，测定5μg/L的NIST SRM981自然丰度铅同位素标准溶液的各对铅同位素比值，获得的^207Pb／^206Pb分析精度可优于0．1％。在该条件下测定了14个不同的水泥粉样品中的铅同位素比值，结果显示：铅的同位素比值分析技术可以用来示踪环境监测样品的铅污染源。     

同位素稀释电感耦合等离子体质谱法测量鱼样中的总汞

发展了一种条件温和的提取鱼样中总汞的前处理方法,并建立了同位素稀释电感耦合等离子体质谱(ID-ICP-MS)分析鱼样中总汞的方法。对ID-ICP-MS测量过程中的主要误差来源进行了讨论,使用铅同位素标准参考物NIST SRM 981对测量汞同位素过程中的死时间和质量歧视效应进行了校正。对两种标准参考物(金枪鱼肉IAEA436和角鲨鱼肝NRCC DOLT-3)中的总汞用ID-ICP-MS进行了测定。IAEA436和DOLT-3总汞的测定结果分别为4.23±0.06mg/kg和3.33±0.05mg/kg,与标准值相符。此外,建立的前处理方法可以有效地降低测量过程中汞在系统中产生的“记忆效应”,有利于ID-ICP-MS的应用。     

电感耦合等离子体质谱法测定硼同位素丰度

以硼同位素标准物质NIST SRM 951配制标准溶液,在优化的仪器操作条件下对电感耦合等离子体质谱(ICP-MS)测定的硼同位素质量进行校正,求出校正因子,确定了样品的线性浓度范围,选定样品浓度为1.1 mg/L。在同样的仪器条件下首先测定了硼标准物质的硼同位素丰度比,测量误差为0.2%,然后测定了硼同位素浓缩过程中硼样品的硼同位素丰度比,测定结果的相对标准偏差为1.1%。此外考察了仪器的稳定性。实验结果表明本方法“记忆效应”小,结果可靠,测量精度高。     

电感耦合等离子体质谱法测定土壤中痕量铀

建立电感耦合等离子体质谱法测定土壤样品中痕量铀含量的方法。采用硝酸、氢氟酸、高氯酸混合酸消解样品后,以铼为内标溶液校正基体干扰,用电感耦合等离子体质谱仪测定土壤中的痕量铀含量。实验结果表明,铀的质量浓度在0~20 ng/m L范围内与信号强度呈线性关系,相关系数r=0.999 9,方法检出限为0.006μg/g,测定结果的相对标准偏差小于5%(n=6),加标回收率在96%~103%之间。用该方法与标准方法对同一样品进行测定,两种方法测定结果一致。该方法准确可靠,满足土壤样品中痕量铀含量的测定要求。     

电感耦合等离子体质谱法测定铜精矿中痕量铀

铜精矿样品经盐酸和硝酸溶解,用电感耦合等离子体质谱法测定样品溶液中痕量铀的含量。优化了仪器工作参数及酸的用量。铀的质量浓度在40.0μg.L-1范围以内与其信号值呈线性关系,方法的检出限(3S/N)为0.012 ng.g-1。此法用于铜精矿中铀含量的测定,加标回收率在98.6%～99.4%之间。     

应用多接收器电感耦合等离子体质谱法测定海洋碳酸盐中稳定铅同位素组成

研究了多接收器电感耦合等离子体质谱仪(MC-ICP MS)测定铅同位素比值时,影响测试结果准确度和精密度的主要因素及其优化过程。在优化条件下,10 h内连续30次测定4 ng/mL NIST SRM 981同位素标准溶液铅同位素比值,获得208Pb/206Pb、207Pb/206Pb和206Pb/204Pb相对标准偏差(RSDs)分别为0.005%、0.004%和0.054%。长期监测208Pb/206Pb、207Pb/206Pb和206Pb/204Pb,标准偏差(2SDs)分别为0.000 06、0.000 05和0.006 7。采用NEPTUNE MC-ICP MS法测定了低铅海洋碳酸盐样品中稳定铅的同位素比值,并对南海橙黄滨珊瑚(Porites lutea)和库氏砗磲(Tridacna gigas)进行了分析,得到全流程空白为8～10 pg,重复样误差优于0.1%。经0.50 mol/L HNO3洗脱之后,得到海南珊瑚样品中208Pb/206Pb、207Pb/206Pb的比值分别为2.086 2±0.001 5、0.849 90±0.001 47(n=16);海南砗磲样品中208Pb/206Pb、207Pb/206Pb的比值分别为2.116 9±0.004 2、0.864 81±0.001 62(n=9)。进一步考察了南海海洋碳酸盐中204Pb的同位素比值。分析结果表明,南海海洋碳酸盐中稳定铅同位素比值与中国气溶胶、珠江三角洲大气沉降、黄土及南海海底玄武岩等具有很好的相关性。方法适用于复杂基体高钙低铅的海洋碳酸盐样品中铅同位素比值的分析。     

激光烧蚀-多接收电感耦合等离子体质谱法测定铀颗粒物中铅杂质的同位素比值

为有效获取铀颗粒物中具有取证价值的铅杂质同位素信息,建立了激光烧蚀-多接收电感耦合等离子体质谱(LA-MC-ICP-MS)测定铀颗粒物中铅杂质同位素比值的方法.探究了诸多同位素分馏效应校正方法下铅本底对同位素测量的影响,选用的LA-MC-ICP-MS系统的本底对比值测量结果的影响小于0.001(208Pb的信号强度大于2.2× 103 cps),确定采用NIST SRM612为外标校正质量分馏,固定激光束斑直径30μm、脉冲重复率20 Hz、调节能量密度使LA-MC-ICP-MS分析NIST SRM612和铀颗粒物样品所得208Pb分别小于1.5×105 cps和3×104 cps,标准物质CRM124-4样品中206Pb/208Pb、206Pb/207Pb和207Pb/208Pb比值测量结果的相对实验标准不确定度小于0.48％、0.68％和0.40％.实际样品分析结果表明,本方法可有效区分铀颗粒物中的铅同位素比值差异,有助于鉴别其来源.     

气溶胶直接进样电感耦合等离子体-质谱法快速测定环境气溶胶中~(239)Pu

采用本实验室建立的气溶胶直接进样ICP-MS在线定量分析技术,对取样钢瓶取得的某环境气溶胶样品进行直接进样快速分析.结果表明: 对239Pu的检出限为1.4×10-3 Bq/m3;所测样品浓度在3.1×10-3～1.2×10-2 Bq/m3之间,比法规限值低一个量级以上.     

汽油中痕量铅的电感耦合等离子体质谱法同位素比值分析

为建立汽油中痕量铅的等离子体质谱的同位素比值分析方法,考察使用了不同的样品处理手段处理汽油样品。结果表明,V(HNO3) V(H2O)=1 10体系萃取汽油,为汽油中同位素比值分析的最佳方法,其操作安全简单,方便快速,且灵敏度高,从而有效保证同位素比值分析的精确度。利用等离子体质谱仪对汽油中痕量铅的实际含量进行了分析,为配合城市大气铅污染来源调查工作提供了一种极为快速简捷、安全有效的手段。     

在线稀释进样-电感耦合等离子体质谱法测定单个酵母细胞中痕量元素的研究

基于四通阀在线稀释装置和单通道雾化室,建立了在线稀释进样-电感耦合等离子体质谱(ICP-MS)测定单个酵母细胞中痕量元素的分析方法.结果表明,在线稀释装置与单通道雾化室联用的单细胞信号采集效率为31.3％,显著大于双通道雾化室的1.3％.所测富硒酵母细胞中元素信号呈现不同的分布情况,除Mg外,P、Cu、Zn、Se等都表...     

Accurate Determination of Lithium Isotopic Compositions in Geological Samples by Multi-collector Inductively Coupled Plasma-Mass Spectrometry

Accurate determination of lithium (Li)isotopic composition in natural geological samples is the basis for Li isotope geochemical studies. In this study, a method contained preparation of geological materials (water and rock) and accurate determination of Li isotopic composition was set up. The separation of Li from water and rock samples was implemented by a single column containing 1.5 mL of Bio-Rad AG 50W-X12 (200–400 mesh) resin, with 0.40 M HCl and 1.0 M HCl as eluents. Only 8.5 and 14 mL of eluents were used to separate Li from water and rock samples with this method, respectively. Blank signal of the operation procedure was (2.4 ± 0.1) mV, which was almost same as the 2.3 mV of the 2% HNO₃ signal used in this study. Experimental results showed that Li isotopic fractionation during leaching process was significant and deviation of δ⁷Li values in these samples with incompletely recovered Li reached up to 50‰. Lithium isotopic ratios were determined by multi-collector ICP-MS (Nu Plasma II) using the sample standard bracketing (SSB) method. L-SVEC standard with similar Li concentration to samples (about 80 ng mL^?1) was used in this study. The external precision (2σ) of this technique, determined by repeated measurement of pure Li standard solutions and seawater was < ±0.8‰. The measured δ⁷Li values of seawater and rock standards AGV-2, BCR-2 and GSP-2 were +31.4‰ ± 0.7‰ (n = 18), +7.23‰ ± 0.16‰ (n = 4), +3.7‰ ± 0.7‰ (n = 8) and ?0.10‰ ± 0.18‰ (n = 4), respectively, similar to previously published values. This method could be used to accurately determine Li isotopic composition of various types of geological samples such as waters and rocks. The advantage of this method was that the amount of resin and reagent was reduced to 50% or less of the previous studies, thereby significantly improving the work efficiency and reducing the operation procedure blank.     

电感耦合等离子体质谱间接法测定蛋白质含量

尺寸排阻色谱分离牛血清白蛋白(BSA),超氧化物歧化酶(SOD)和金属硫蛋白(MT)等3种标准蛋白的混合物后,在线使用电感耦合等离子体质谱测定这三种蛋白中的S,并根据每种蛋白质含有的S原子数,计算出3种蛋白质的相对含量。尺寸排阻色谱的流动相为0.1mol/LTris-HAc。向电感耦合等离子体质谱的六级杆加入反应气O2,使之与S反应生成SO ,间接测定32S16O 而避开直接测量32S时存在的严重干扰。测量结果与天平称量所得结果一致。方法的精密度好,每个蛋白质峰面积的RSD<3%(n=3)。BSA、SOD和MT的检出限分别为14、52和27pmol。     

电感耦合等离子体质谱法分析小鼠组织中以及和DNA结合的贫铀浓度与235U/238U

在DU染毒动物模型基础上,采用ICP-MS技术同时测定各组织中铀浓度和235U/238U比值,分析DU在体内的分布和代谢规律;提取纯化肝肾组织中的基因组DNA,ICP-MS检测与DNA结合的DU浓度和235U/238U。以Pt为内标元素,补偿基体效应,组织中铀的检出限为0.0019～0.0981μg/kg;精密度(RSD)为0.92%～2.13%,回收率在100%±10%内。ICP-MS对贫铀气溶胶中235U/238U检测结果与经典的α谱仪检测结果相吻合。DNA样品采用中性溶液稀释,DNA中铀元素检出限为0.0016μg/kg DNA,回收率为98.3%±7.3%。样本测定结果显示,肾脏和骨骼对贫铀的蓄积能力最强,脑组织几乎不受贫铀影响,其它组织的DU蓄积能力介于二者之间。在肾、肝组织中,DU可以与DNA发生结合,与肾DNA结合更持久。组织中235U/238U随染毒铀同位素组成和浓度发生规律性改变。铀浓度与235U/238U均可以作为衡量核素污染类型和程度的敏感指标。     

电感耦合等离子体质谱法测定高纯金中痕量杂质

建立了高纯金中40余种痕量杂质的电感耦合等离子体质谱测定方法。方法检出限为0．0006～0．21μg/L。考察了基体Au的谱干扰及基体效应,采用Cs内标补偿基体对待测信号的抑制作用。方法简单、快速、灵敏、准确。     

电感耦合等离子体发射质谱法测定钨矿石中的钨华

建立电感耦合等离子体发射质谱法测定钨矿石中钨华的含量。用氨水溶液对矿石样品进行浸取分离,将浸取液稀释10倍体积后测定,以3%盐酸溶液作为测定介质。WO3的质量浓度在0~100 ng/m L范围内与信号强度呈良好的线性关系,相关系数为0.999 9,方法检出限为0.5 ng/m L。用该方法对5个钨矿石样品和2个标准物质样品中的钨华进行测定,测定结果的相对标准偏差为2.15%~9.46%(n=12),且与经典方法极谱法测定结果的相对偏差小于10%。该方法快速、简便,精确度较高,可用于钨矿石中钨华的测定。     

Determination of Bromine in Human Serum by Inductively Coupled Plasma-Mass Spectrometry

Abstract

The determination of bromine in human serum by inductively coupled plasma-mass spectrometry (ICP-MS) is discussed. Sample preparation was kept as limited as possible: serum samples were only diluted with nitric acid (five- or ten-fold). Indium was added as internal standard. In order to avoid overlap of ⁴⁰Ar ⁴⁰Ar with     

电感耦合等离子体质谱法测定高纯氧化钇

报道了高纯氧化钇中３０种痕量稀土和非稀土杂质元素的电感耦合等离子体质谱测定方法。考察了谱干扰及基体效应，采用Ｇａ内标能较好地补偿基体钇的影响。方法检出限为０．０１３￣４．１μｇ／Ｌ。方法简便，快速，灵敏。     

Characterization of Geological Certified Reference Materials by Inductively Coupled Plasma-Mass Spectrometry

A rapid, safe, and efficient microwave-assisted acid digestion method is reported to determine thirty-six elements in three international geological reference materials and two in-house reference materials using high resolution inductively coupled plasma mass spectrometry. This method was also employed to determine the radiogenic isotopic composition of Sr and Nd in two geological reference materials by multicollector inductively coupled plasma mass spectrometry. In order to ascertain the most suitable preparation method, four microwave-assisted digestion procedures were compared. The presence of insoluble fluorides on the recoveries of Ba, Rb, Sr and rare earth elements was resolved through sequential evaporation at 80 degrees Celsius followed by microwave digestion. Digestion methods without using HClO₄ or H₃BO₃ and using only H₃BO₃ were unsuitable due to lower recoveries and higher procedural blanks, respectively. Digestion methods that involved the use of HCl-HNO₃-HF and HCl-HNO₃-HF-HClO₄ were most suitable, resulting in better recoveries of the elements. However, the HCl-HNO₃-HF method was preferred compared to HCl-HNO₃-HF-HClO₄ because the former avoids the use of HClO₄ and thus was used in measurements of the radiogenic isotopes of Sr and Nd. The optimized method was used to verify the reference values for the isotopic compositions of Sr and Nd in geological standard reference materials.