分光光度法测定合金钢中的钼

建立了采用氯化亚锡还原-分光光度法测定合金钢中钼的方法,研究了实验条件对检测结果的影响,用测定已知钼含量的合金钢标准样品,选定最佳检测条件,在选定的实验条件下对样品中钼含量进行检测,其结果与传统的测钼方法得到的结果吻合,方法省时省试剂,能快速准确测得合金钢中的钼。     

微波消解–电感耦合等离子体质谱法测定铀合金中铌、钼、锆

建立微波消解–电感耦合等离子体质谱法测定铀合金中铌、钼、锆。铀铌钼锆合金样品经8 mL HNO_3 (1+1)和2 mL HF微波消解并稀释处理后,利用电感耦合等离子体质谱法测定合金样品中铌、钼、锆含量,研究了铀浓度在0～30 μg/L时对铌、钼、锆元素直接测定的影响。铌、钼、锆的质量浓度在各自的范围内与其质谱响应值线性关系良好,相关系数大于0.999。铌、钼、锆的加标回收率为96.10%～105.00%,测定结果的标准偏差为0.74%～2.71%(n=6)。该方法流程简单,无需分离基体元素,可实现铀合金中铌、钼、锆元素的快速测定。     

封闭溶样-电感耦合等离子体质谱法测定地质样品中痕量金

建立了聚乙烯塑料瓶封闭水浴加热,王水溶解,以铼作内标,电感耦合等离子体质谱法测定地质样品中痕量金。结果表明,样品中的金可分解完全,节约了成本、减少了环境污染。方法经国家一级标准物质验证,结果与标准值相符。对实际样品测定的方法相对标准偏差(RSD,n=9)为4.1%～6.7%。方法检出限为0.12ng/g,方法简便快速,适用于地质样品的批量分析。     

电感耦合等离子体原子发射光谱法测定钼镧合金中镧元素

采用盐酸-硝酸溶解钼镧合金样品,建立电感耦合等离子体原子发射光谱法（ICP-AES）测定钼镧合金中镧元素的分析方法,给出影响测量结果的不确定度分量。选择379.478nm为镧的分析谱线,通过基体匹配法消除基体钼的干扰。在优化条件下对钼镧合金样品进行测定,线性相关系数在0.999以上,定量下限为0.048%,测定结果的相对标准偏差（RSD,n=11）小于3%,回收率为93.00%~105.00%。该方法快速、准确,可以满足实际生产中钼镧合金样品的测定要求。     

电感耦合等离子体原子发射光谱（ICP-AES）法测定钼镧合金中镧含量

采用盐酸-硝酸溶解钼镧合金样品,建立了电感耦合等离子体原子发射光谱(ICP-AES)法测定钼镧合金中镧含量的分析方法,给出影响测定结果的不确定度分量。选择379.478nm为镧的分析谱线,通过基体匹配法消除基体钼的干扰。在优化条件下对钼镧合金样品进行测定,线性相关系数达到0.999以上,定量下限为0.048%,测定结果的相对标准偏差(RSD,n=11)小于3%,加标回收率为93.0%～105%。方法快速、准确,可满足实际生产中钼镧合金样品的测定要求。     

X射线荧光光谱法同时测定矿石中钨钼锡

提出了X射线荧光光谱法同时测定钨钼锡矿石中钨、钼、锡元素含量的分析方法。方法选择四硼酸锂作熔剂,熔融制成样片,通过PW2403型X射线荧光光谱仪自带Super Q系统软件,以经验α系数法和Rh康普顿散射线内标法校正基体效应。以标准样品建立工作曲线,同时测量样品中钨、钼、锡元素含量。方法准确度和精密度能满足规范要求,钨、钼、锡的分析方法检出限分别为0.0042%、0.0026%、0.0072%。采用本法同时测定矿石中钨、钼、锡元素含量结果与传统分析方法测定结果相吻合,样品检测结果能满足矿区地质勘查的工作要求。     

直读光谱法测定合金工具钢中铬、锰和钼

建立了ARL-4460直读光谱仪对Cr12、Cr12MoV中铬、锰、钼元素的快速检测方法。使用基体铁作为内标元素,测定标准样品中铬、锰、钼元素的相对强度,减少了外界电压不稳对绝对强度稳定性的影响;由于标准样品中基体铁含量不同,为减少内标元素含量的变化对工作曲线相关系数和估计标准差的影响,使用相对含量校正工作曲线。在优化的实验条件下,试样中三种元素的相对标准偏差分别为0.68%、0.79%和1.7%(n=11)。测定结果与化学分析方法测定结果一致,可实现合金工具钢中铬、锰和钼的快速检测。     

电感耦合等离子体发射光谱测定钼铝合金中硅含量的方法研究

采用王水、氢氟酸在180℃加热条件下溶解试样,全面分析了硅元素的212.412、221.667、251.611、252.851、288.158 nm五条分析谱线的受干扰情况,最终选择了灵敏度和信噪比较高、受钼基体干扰程度较小的Si 288.158 nm为分析谱线。使用多谱线拟合(MSF)技术建立了Si 288.158 nm的光谱校正模型,通过校正模型对样品检测信号峰进行了校正,消除了基体钼(Mo 288.137 nm)的光谱干扰,建立了电感耦合等离子体发射光谱法(ICP-OES)测定钼铝合金中硅含量的方法。该方法在0.10～5.00 mg/L范围内(对应固体样品中硅的质量分数范围为0.010%～0.50%),硅的工作曲线线性关系良好,相关系数为0.9995;方法检出限和定量限分别为23μg/g和76μg/g;对3个不同含量的钼铝样品中的硅含量进行了测定,测定结果的相对标准偏差(RSD)在0.76%～1.36%之间,加标回收率在98.0%～106%范围,与标准(YS/T 1075.3-2015)中钼蓝分光光度法的测定结果一致。     

高压消解-电感耦合等离子体质谱(ICP-MS)法测定地质样品中的铌和钽

建立了运用硝酸-硫酸-氢氟酸体系高压消解样品,电感耦合等离子体质谱(ICP-MS)法测定地质样品中铌和钽含量的方法。研究了样品消解体系、样品消解时间、溶液的介质、内标元素等对测定的影响。Nb的方法检出限为0.027μg/g,Ta的方法检出限为0.015μg/g。Nb测定的相对标准偏差(RSD)为3.3%;Ta测定的相对标准偏差(RSD)为2.5%。经标准物质验证,分析结果令人满意,可适用于大批量地质样品中铌和钽的测定。     

流动注射-分光光度-火焰光度串联技术同时快速测定磷、钾、钠的研究

本文利用流动注射-分光光度-火焰光度串联技术,使磷生成磷钼兰以721型分光光度计检测,钾、钠以6400型火焰光度计检测,从而建立了磷、钾和钠三元素同时快速测定的新方法,该方法操作简单、方便、快速,每小时可进行60次测定,磷、钾、钠兰元素的线性范围分别为1.0～4.0μg/ml、3.0～60μg/ml和6.0～40μg/ml。利用该方法测定了植物样品中的磷、钾和钠,获得了良好的结果。     

石墨炉原子吸收光谱法测定地质样品中的痕量金

用活性炭吸附,于5％盐酸溶液中用甲基异丁基酮(MIBK)萃取金,采用斜坡升温和热解涂层石墨管技术进行地质样品中痕量金的石墨炉原子吸收光谱法测定,检出限为0．1ng/g。用该方法对标准物质进行测定,结果与标准值相符,测定结果的相对标准偏差为2．0％～6、9％(n=6)。     

Fast simultaneous determination of niobium and tantalum by Kalman Filter analysis with flow injection chemiluminescence method.

A fast and highly efficient Kalman Filter analysis-flow injection chemiluminescence (FI-CL) method was developed to simultaneously determine trace amounts of niobium and tantalum in geological samples. The method, without the boring process of separation and dear instruments, is suitable for field scene analysis. The mixed chemiluminescence kinetic curve was analyzed by a Kalman Filter (KF) in this method to realize the simultaneous determination of niobium and tantalum. Possible interference elements in the determination were investigated. Under the selected conditions, the detection limits (3sigma, n = 11) of niobium(V) and tantalum(V) were 2.1 x 10(-3) microg g(-1) and 4.0 x 10(-3) microg g(-1), respectively, and the relative standard deviations were 4.9% and 3.3% (n = 9). The method was applied to the determination of niobium and tantalum in geological samples with satisfactory results.     

电热鼓风干燥箱解脱–火焰原子吸收光谱法测定地质样品中金的含量

建立高海拔地区电热鼓风干燥箱解脱–火焰原子吸收光谱法测定地质样品中的金的方法。高海拔地区由于大气压低,水的沸点低,使得泡塑吸附金的解脱率不高。为了得到准确的分析结果,采用电热鼓风干燥箱代替水浴锅来解脱泡塑吸附金,优化后的解脱条件:解脱温度为105℃,解脱时间为30 min,在此条件下金的解脱率为91.19%。金的质量浓度在0.00~10.00μg/mL范围内与其吸光度呈良好的线性关系,相关系数r=0.999 6,方法检出限为0.012μg/mL。测定结果的相对标准偏差为2.15%(n=7),加标回收率为96.0%~102.5%。用该方法测定国家一级标准物质,测定结果与参考值相符。该方法准确、可靠,适用于高海拔地区地质样品中金的测定。     

A new strategy of solution calibration in laser ablation inductively coupled plasma mass spectrometry for multielement trace analysis of geological samples

Because multielement trace analysis by laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) is often limited by the lack of suitable reference materials with a similar matrix composition, a novel quantification strategy using solution calibration was developed. For mass spectrometric multielement determination in geological samples a quadrupole-based LA-ICP-MS is coupled with an ultrasonic nebulizer (USN). In order to arrange matrix matching the standard solutions are nebulized with a USN during solution calibration and simultaneously a blank target (e.g. lithium borate) is ablated with a focused laser beam. The homogeneous geological samples were measured using the same experimental arrangement where a 2% nitric acid is simultaneously nebulized with the USN. Homogeneous targets were prepared from inhomogeneous geological samples by powdering, homogenizing and fusing with a lithium borate mixture in a muffle furnace at 1050 degrees C. Furthermore, a homogeneous geological glass was also investigated. The quantification of analytical results was performed by external calibration using calibration curves measured on standard solutions. In order to compare two different approaches for the quantification of analytical results in LA-ICP-MS, measured concentrations in homogeneous geological targets were also corrected with relative sensitivity coefficients (RSCs) determined using one standard solution only. The analytical results of LA-ICP-MS on various geological samples are in good agreement with the reference values and the results of other trace analytical methods. The relative standard deviation (RSD) for trace element determination (N = 6) is between 2 and 10%.     

A new strategy of solution calibration in laser ablation inductively coupled plasma mass spectrometry for multielement trace analysis of geological samples

Because multielement trace analysis by laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) is often limited by the lack of suitable reference materials with a similar matrix composition, a novel quantification strategy using solution calibration was developed. For mass spectrometric multielement determination in geological samples a quadrupole-based LA-ICP-MS is coupled with an ultrasonic nebulizer (USN). In order to arrange matrix matching the standard solutions are nebulized with a USN during solution calibration and simultaneously a blank target (e.g. lithium borate) is ablated with a focused laser beam. The homogeneous geological samples were measured using the same experimental arrangement where a 2% nitric acid is simultaneously nebulized with the USN. Homogeneous targets were prepared from inhomogeneous geological samples by powdering, homogenizing and fusing with a lithium borate mixture in a muffle furnace at 1050?°C. Furthermore, a homogeneous geological glass was also investigated. The quantification of analytical results was performed by external calibration using calibration curves measured on standard solutions. In order to compare two different approaches for the quantification of analytical results in LA-ICP-MS, measured concentrations in homogeneous geological targets were also corrected with relative sensitivity coefficients (RSCs) determined using one standard solution only. The analytical results of LA-ICP-MS on various geological samples are in good agreement with the reference values and the results of other trace analytical methods. The relative standard deviation (RSD) for trace element determination (N = 6) is between 2 and 10%.     

氢化物发生-原子荧光光谱法测定1：5万区域地质调查样品中的As、Sb、Bi、Hg等4种元素

建立了氢化物发生-原子荧光光谱法测定1∶5万区域地质调查样品中的As、Sb、Bi、Hg等4种元素的分析方法,通过采用王水(1+1)分解样品,在盐酸(5%)介质中用硼氢化钾作为还原剂对As、Sb、Bi、Hg等4种元素进行氢化物发生-原子荧光光谱法测定。方法检出限为0.008 9(As)、0.008 1(Sb)、0.008 1(Bi)、0.001 7(Hg)μg/g,测定结果的相对标准偏差(RSD,n=12)为0.82%～7.6%,准确度△lgC=-0.01～0.02。方法简便、成本低,检测结果准确,检出限、准确度及精密度均能达到行业规范要求,适用于1∶5万区域地质调查样品水系沉积物、土壤中As、Sb、Bi、Hg等4种元素的测定。     

泡沫塑料动态快速分离富集金方法的研究

本文系统研究了泡沫塑料动态快速分离富集金的方法。对泡沫塑料柱的处理方法,再生及主要共存离子干扰的消除等均做了较详细的研究。提出了一种简便,不控速的金分离富集的方法。该法用于分析0.051～3.59g/t四种不同含量的金标样,结果与推荐值吻合,5次分析结果,相对标准偏差<5％,同时,可用泡沫塑料柱当天连续使用分析拿标样,回收率为93％—109％。     

A direct method for the determination of carbonate and non-carbonate carbon in geological materials by infrared spectrometry

A simple and direct infrared method for determining carbonate and non-carbonate carbon in geological samples is described. To determine carbonate carbon, hydrochloric acid is added directly to the heated samples; non-carbonate carbon is determined by combustion after digesting the samples with hydrochloric acid. The limit of detection is 2 ppm for carbonate carbon and 10 ppm for non-carbonate carbon; the relative standard deviations are 4% or less for 100–1000 μg of carbonate and non-carbonate carbon. The method has been applied to standard rocks, NBS minerals and geological exploration reference samples.     

岩石样品中43种元素的高分辨等离子质谱测定

以ＨＮＯ３和ＨＦ高压密封溶样,选择各元素浓度分布高低兼顾的国标ＷＢＧ０７１０３和ＷＢＧ０７１０５作参考标准,以高分辨ＩＣＰ－ＭＳ仪器测定岩石样品中４０余种元素,方法检出限在０．１～１８８ｎｇ／ｇ之间,各元素相对标准偏差（ＲＳＤ,ｎ＝６）多在５％以下,方法已用于批缇岩石样品分析。