电感耦合等离子体质谱法(ICP-MS)测定高纯氧化铒中稀土杂质

从同位素的选择、基体效应,内标元素的选择及仪器工作条件等方面对实验参数进行了优化,重点研究了等离子体功率及仪器分辨率的改变对铒基体所形成的氢化物多原子离子干扰的影响。通过提高等离子体功率、改变仪器分辨率及数学方程校正等方法,减少和剔除了ErH对Ho和Tm测定的干扰。实验中选取Cs为内标元素,测定了不同含量的高纯氧化铒样品。分析结果与标准加入法结果进行了比较,之间无显著性差异。     

电感耦合等离子体发射光谱(ICP-OES)在地质样品中的研究进展

电感耦合等离子体发射光谱仪在地质样品无机元素分析测试中常用,具有灵敏度高,干扰小,测定线性范围广、稳定性好等优点。本文就电感耦合等离子体发射光谱法测定地质土壤,岩石样品时,综述了酸溶法、碱熔法、烧结法三种消解体系各自特点及消解剂的特性;详细分析了样品测定时外标法、内标法、标准加入法的选择及应用;探讨了样品测试时仪器条件的优化措施,同时对电感耦合等离子体发射光谱的干扰及校正做了分析。最后,对电感耦合等离子体发射光谱测定技术在地质样品中非金属元素分析物测定的应用及未来发展进行了展望。     

电感耦合等离子体质谱法测定氧化钕中砷含量

建立草酸沉淀分离氧化钕,用校正方程消除残余钕离子产生的双电荷离子干扰,电感耦合等离子体质谱法测定砷含量的方法。选择了溶解样品条件,硝酸溶解样品即能满足检测要求;优化了仪器条件,功率1500W,雾化器流量0.86L/min;进行了内标元素的选择,确定Rh为最佳校正内标元素;确定用草酸分离基体并结合干扰校正方程消除钕的双电荷离子干扰;方法检出限为0.029 ng/mL,定量限为0.097 ng/mL。采用方法对实际样品进行测定,回收率(n=11)为94%～104%,相对标准偏差(RSD,n=11)为0.56%～5.82%。     

电感耦合等离子体质谱(ICP-MS)法测定氧化钕中砷含量

建立了草酸沉淀分离氧化钕,用校正方程消除残余钕离子产生的双电荷离子干扰,电感耦合等离子体质谱(ICP-MS)法测定砷含量的方法。选择了溶解样品条件,硝酸溶解样品即能满足检测要求;优化了仪器条件,射频功率1 500 W,雾化器流量0.86L/min;进行了内标元素的选择,确定Rh为最佳校正内标元素;确定用草酸分离基体并结合干扰校正方程消除钕的双电荷离子干扰;方法检出限为0.029ng/mL,定量限为0.097ng/mL。对实际样品进行测定,加标回收率为94%~104%,相对标准偏差(RSD,n=11)为0.56%~5.8%。方法操作简单,快速、准确,加标回收率及相对标准偏差满足日常检测要求。     

均匀实验设计-电感耦合等离子体发射光谱(ICP-OES)法测定N36锆合金中微量钠元素含量

建立了电感耦合等离子体发射光谱(ICP-OES)法测定N36锆合金中微量钠元素含量的分析方法。对样品溶解方法、观测方式、谱线选择、基体效应干扰等对实验的影响进行了讨论。采用均匀试验设计法确定了最佳的等离子体发生器功率、等离子气流量、辅助气流量、雾化气流量。实验结果表明,锆基体对测定结果有较大影响。采用基体匹配消除干扰,在均匀实验设计优化的仪器测定参数下,实验证明,方法的相对标准偏差(RSD,n=11)5%,加标回收率在95%～105%。所建立的方法快捷、简便、准确,满足核用N36锆合金中微量钠元素的分析要求。     

均匀试验设计电感耦合等离子体发射光谱(ICP-OES)法测定N36锆合金中微量钠元素含量

建立了电感耦合等离子体发射光谱法测定N36锆合金中微量钠元素含量的分析方法。对样品溶解方法、观测方式、谱线选择、基体效应干扰等对实验的影响进行了讨论。采用均匀试验设计法确定了最佳的等离子体发生器功率、等离子气流量、辅助气流量、雾化气流量。实验结果表明,锆基体对测定结果有较大影响。在本实验中,采用基体匹配消除干扰,在均匀试验设计优化的仪器测定参数下,使用N36锆合金样品对本方法的精密度与准确度进行验证,相对标准偏差(RSD,n=11)＜5%,加标回收率在95%~105%之间。所建立的方法快捷、简便、准确,满足核用N36锆合金中微量钠元素的分析要求。     

电感耦合等离子体质谱(ICP-MS)法测定高纯砷中痕量磷和硒

通过对样品前处理方式、内标元素及质量数的选择、仪器检测模式等方面进行优化,采用串联四级杆电感耦合等离子体质谱仪直接测定高纯砷中痕量的磷和硒.实验室使用电子级盐酸、硝酸配制王水直接溶解样品,在不除基体的情况下,以铑作为内标补偿校正砷基体的抑制效应,在调试好的仪器上进行测定磷、硒含量.磷、硒的测定结果相对标准偏差(RSD)...     

电感耦合等离子体质谱法测定高纯铼中26种痕量杂质元素

以电感耦合等离子体质谱法(ICP-MS)测定了高纯铼中26种杂质元素含量。应用反应池技术消除了复合离子对K、Ca、Fe等元素的干扰,采用干扰方程校正技术消除了Re氧化物对Tl的质谱重叠干扰,未受干扰的其它杂质元素采用内标校正法直接测定。考察了溶液酸度、基体效应等条件对测定的影响,优化选择了测定同位素和内标元素。方法测定下限介于0.12～5.0μg/g,加标回收率在90%～110%之间,相对标准偏差小于10%。方法可以满足4N5高纯铼的测定。     

端视ICP-AES中用铟内标校正钠基体干扰的研究

端视电感耦合等离子体原子发射光谱中易电离元素引起的非光谱干扰,常使分析结果产生偏差。本文就不同浓度钠基体对分析谱线产生的干扰进行了试验和研究,并用铟作为内标元素来补偿钠基体的干扰。得出选择用几个内标元素和多条内标谱线时可以校正钠基体的干扰。     

电感耦合等离子体质谱法(ICP-MS)测定镍钴锰三元素氢氧化物中铅

研究了用电感耦合等离子体质谱法(ICP-MS)测定镍钴锰三元素氢氧化物中铅含量的测定方法。选择了仪器的最佳测量条件、元素测定的质量数,进行了基体元素的干扰等实验。方法测定结果准确、可靠,测定下限小于0.00005%,样品加标回收率在99.2%~101.0%。方法的建立为控制镍钴锰三元素氢氧化物中铅提供了检测依据。     

Direct determination of rare earth impurities in high purity erbium oxide dissolved in nitric acid by inductively coupled plasma mass spectrometry

A novel method was developed for the direct determination of trace quantities of rare earth elements (REEs) in high purity erbium oxide dissolved in nitric acid by inductively coupled plasma mass spectrometry (ICP-MS) in this work. The mass spectra overlap interferences arose from Er matrix on the neighbouring and monoisotopic analytes of ¹⁶⁵Ho(100) and ¹⁶⁹Tm(100) were eliminated by adjusting instrumental peak resolution value from 0.7 to 0.3 amu. The matrix suppression effect of Er on the ion peak signals of REEs impurities was effectively compensated with spiking In as internal standard element. The limit of quantitation (LOQ) of REEs impurities was from 0.0090 to 0.025 μg g⁻¹, the recoveries of spiked sample for REEs were found to be in the range of 90.3-107% through using the proposed method and relative standard deviation (R.S.D.) varied between 2.5% and 6.7%. The novel methodology had been found to be suitable for the direct determination of trace REEs impurities in 99.999-99.9999% high purity Er₂O₃ and the results obtained from this method keep in good agreement with that acquired from high resolution ICP-MS.     

三重四极杆电感耦合等离子体质谱(ICP-MS)法测定氧化铕中13种稀土杂质元素

稀土杂质元素直接影响高纯单金属稀土材料的整体性能,是高科技领域许多材料的重要组成部分。通过考察最佳的消解酸量、温度、时间、氧气反应气流量、稀释气流量,建立了基于三重四极杆电感耦合等离子体质谱仪(ICP-MS/MS)直接测定氧化铕中13种稀土杂质元素分析方法。该方法采用0.1%基体直接进样,可以很大程度提高前处理分析效率。利用碰撞模式测定氧化铕稀土中的Y、La、Pr、Nd、Sm、Gd、Tb、Dy、Ho、Er、Yb、Lu元素,氧气质量转移模式测定氧化铕中的Tm,两种模式结合可以有效去除多原子干扰,实现氧化铕的稳定测试分析。通过对氧化铕标准物质（GBW02902）直接测定分析,结果表明,在碰撞和氧气质量转移模式下,各元素线性相关系数（r）均大于 0.9999,方法检出限为0.001~0.023 mg/kg,测试精密度优于1.99%,13种元素的测试值都在认定值的不确定度范围之内。该分析方法操作简单,测试稳定,效率高,为实验室进行氧化铕材料中REE杂质的准确测试分析提供思路和借鉴。     

An ICP-AES method for the determination of heavy rare earth elements (Eu-Lu) in high purity yttrium oxide

Traces of heavy rare earth elements (Eu-Lu) were determined in high purity yttrium oxide by inductively coupled plasma atomic emission spectrometry. The yttrium oxide samples were dissolved in nitric acid and the solutions analyzed with a plasma produced by a 56 MHz RF generator at an output power of 1.5 kW. Using a high resolution sequential monochromator, interference-free spectral lines for Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb and Lu could be found for calibration. The detection limits for the above elements have been found to be slightly higher in the presence of yttrium matrix, than in aqueous solution. This could be attributed to background enhancements due to the presence of yttrium. The mean RSD of the method varied between 2.3% and 6.3% in the concentration range 0.01 and 0.5 g/ml. The percentage recovery ranged from 84 to 106 for the different rare earth elements.     

Determination of rare earth impurities in high purity europium oxide by inductively coupled plasma-mass spectrometry and evaluation of concentration values for europium oxide standard material

Direct determinations of 13 rare earth elements (La, Ce, Pr, Nd, Sm, Gd, Tb, Dy, Ho, Er, Yb, Lu and Y) in high purity europium oxide by inductively coupled plasma mass spectrometry (ICP-MS) have been reported. The operating parameters of the instrument were optimized and the spectral interferences and the matrix effects were investigated. Using Ga or Rh as the internal standard can eliminate most of the matrix effects. The detection limits (3 sigma, n=10, integral time=1s) are 0.013-0.085 ng mL(-1) and the reproducibility (n=11) is 0.9-3%. The recoveries of spiking samples are 80-108%. Europium oxide standard material was made and its concentration values were evaluated by various techniques from 10 collaborating laboratories. By comparison of the results of ICP-MS with the results of other techniques, we have validated that ICP-MS is an accurate and reliable technique for analysis of ultratrace impurities in high purity rare earth matrix.     

DIRECT DETERMINATION OF NEODYMIUM AND ERBIUM IN RARE EARTH MIXTURE BY DERIVATIVE SPECTROPHOTOMETRY

The absorption spectra of 4f electron transitions of the complexes of neodymium and erbium with 8-hydroxyquinoline-5-sulphonic acid in the presence of diethylamine and ethanol have been measured by normal and third-derivative spectrophotometry. Their molar absorptivities are 70.7 l.mol~(-1).cm~(-1) for Nd and 62.5 l.mol~(-1).cm~(-1) for Er. They are 7.6 times and 14.9 times greater than those of corresponding chlorides, respectively. Use of the third-derivative spectra both eliminates the interference of Ce(Ⅳ) and increases the sensitivity for Nd and Er. Beer,s Law was obeyed from 0-10 ug/ml of Nd and Er. The method has been applied to the determination of neodymium and erbium in rare earth mixtures.     

微波消解-电感耦合等离子体质谱(ICP-MS)法测定板栗中的矿物元素及稀土元素

为了准确测定板栗中矿物元素和稀土元素的含量水平,采用冷冻干燥方式预处理样品,选用硝酸和过氧化氢体系微波消解样品,结合电感耦合等离子体质谱技术,建立了板栗中钠(Na)、钾(K)、镁(Mg)、锰(Mn)、铁(Fe)、钒(V)、钴(Co)等19种矿物元素及镧(La)、铈(Ce)、镨(Pr)、钕(Nd)、钐(Sm)、铕(Eu)、钆(Gd)、铽(Tb)、镝(Dy)、钬(Ho)、铒(Er)、铥(Tm)、镱(Yb)、镥(Lu)、钇(Y)等15种稀土元素的同时分析测定方法。方法检出限为0.0027~0.78μg/L,相对标准偏差为1.4%~6.3%。通过国家标准物质GBW10019苹果的准确度实验验证,测定结果均在标准证书值范围内。实验结果表明,方法适用于板栗中矿物元素及稀土元素的同时测定。     

高纯氧化铕中微量稀土杂质的化学光谱测定

将高纯Ｅｕ２Ｏ２通过Ｐ５０７萃淋树脂分离富集，分离掉大量基体Ｅｕ２Ｏ３剩下微量稀土杂质用碳粉吸附，加ＫＢＨ４作载体进行光谱测定，本方法可测定９９．９９９９％，纯度的Ｅｕ２Ｏ３中微量稀土杂质。     

标准溶液配制用碳酸锂纯物质中杂质含量的测定

从高纯碳酸锂中杂质含量测定出发,研讨了标准溶液配制用原料的杂质测定方法,首先利用电感耦合等离子体质谱(ICP-MS)法对高纯碳酸锂进行半定量分析,再依据半定量分析结果选择ICP-MS、电感耦合等离子体原子发射光谱(ICP-AES)法、原子吸收光谱(AAS)法等方法对相应元素(杂质含量0.001%)进行定量分析,通过扣除杂质含量得出高纯碳酸锂纯度大于99.991%。从而建立了一个准确、高效,覆盖元素种类多的高纯物质中杂质含量的分析方法     

Determination of the rare earth elements in natural waters by isotope-dilution mass spectrometry

A method is described for the determination of ten rare earth elements (La, Ce, Nd, Sm, Eu, Gd, Dy, Er, Yb, Lu) in natural waters by isotope-dilution mass spectrometry. A 1-l sample is used for sea water, and proportionately less for other natural waters. The rare earth elements are extracted by co-precipitation with hydrated iron (III) oxide and purified on a single cation-exchange column, with hydrochloric and nitric acids as eluents. Final measurements are from a triple Re/ Ta filament in the mass spectrometer, run automatically under computer control. Relative standard deviations are better than 4% for the analysis of standard solutions, with accuracy in the same range. The analytical blank is low ( <0.03 pmol, 4 pg, for Nd) producing a sample/blank concentration ratio greater than 100 for all ten rare earth elements when determined in a 1-l seawater sample. Concentration depth profiles are given for an ocean water and normalised abundance patterns for three natural waters.