固体进样一直接测汞仪法测定金精矿粉中微量汞

将金精矿粉样品直接置于石英舟中,在高纯氧气氛中燃烧,释放出汞,与齐化管中的金形成金汞齐,于900℃热释放出汞蒸汽,用直接测汞仪法测定汞的含量。测定结果的相对标准偏差为0．28％～1．57％（n=6）,方法检出限为1．0pg／kg,加标回收率为95．7％～117．4％。用该法对4种土壤标准样品进行了测定,测定结果与标准值相符。该方法适合于金精矿粉中微量汞的测定。     

石墨炉原子吸收法测定鱼中的铅

用硝酸和双氧水对鱼肉样品进行微波消解,然后用石墨炉原子吸收分光光度法测定鱼肉样品中铅的含量,测定结果的相对标准偏差为0．023％～0.137％（n=6）,加标回收率为83％～105％。     

石墨炉原子吸收分光光度法测定大气颗粒物中的镉

将大气颗粒物样品采集在有机滤膜上(或滤筒中)，用硝酸、高氯酸消解，以石墨炉原子吸收分光光度法测定其中镉的含量。在0．00～8．00μg/L范围内对镉的质量浓度与吸光度数据进行回归，得线性方程为A：0．016 0．041X，相关系数r=0．9991，回收率为90％～94％，测定结果的相对标准偏差为2．1％～7．5％，检出限为0．366μg/L，该方法适用于大气和固定污染源排气中镉的测定。     

石墨炉原子吸收光谱法测定铅钙锡铝合金中铝

铅钙锡铝合金广泛应用于全密封免维护铅蓄电池极板的生产。铅合金中铝的测定国标法采用络天青S比色法。试样用硝酸溶解,加入硫酸沉淀分离基体铅后进行比色测定。铅钙锡铝合金中含钙0．05％～0．12％,含锡0．1％～1．5％,含铝0．01％～0．04％,余量为铅。本文用石墨炉原子吸收光谱法测定铝,试样经硝酸溶解后,不加任何基体改进剂,直接测定,分析结果与国标法结果基本一致。     

铁盐增敏-石墨炉原子吸收法测定岩石样品中超痕量金

在解脱测定液中引入三价铁盐,并在其增敏下,使用石墨炉原子吸收法测定岩石样品中的超痕量金．方法检出限为0．02ng／g,精密度（RSD,n=12）为5％～8％．方法准确可靠．进行国家一级标样物质的测试,结果符合质量要求,与标准值吻合．     

β修正光度法测定食品中的微量锰

在pH=8．6的硼砂-磷酸二氢钾缓冲溶液中,锰(Ⅱ)-铬黑T-吐温80显色体系的最大吸收波长为550nm,利用此显色体系,用卢修正光度法测定食品中的微量锰,Mn(Ⅱ)含量在0．45～35μg／(25mL)内服从比耳定律,线性方程为A。=0．0281X-0．0026,相关系数r=0．9997,用该方法测定调味料八角和奶粉中的微量锰。测定结果的相对标准偏差为0．52％～2．86％,回收率为96．21％～102．2％。     

石墨炉原子吸收分光光度法测定空气中的铍

对300余个样品进行监测,选择灵敏度高的石墨管和最佳基体,提高灰化、原子化的温度,确立了石墨炉原子吸收法测定空气中铍含量的实验条件。样品采用干灰化消解法,最佳溶剂为质量分数l％的硝酸溶液,利用仪器内置的样品浓度计算程序,绘制工作曲线直接获得样品中铍的含量。方法检出限为0．021μg／L,测定结果的相对标准偏差小于2％（n=6）,线性范围为0～6．5μg／L,加标回收率为91．6％～107％。     

石墨炉原子吸收光谱法快速测定天然矿泉水中铬镍和银

研究了快速程序升温石墨炉原子吸收光谱法用于测定天然矿泉水中铬、镍和银。为提高分析速度,该法在升温程序中删去了灰化步骤,缩短了灰化时间,整个升温程序只需22～23s,远快于常规石墨炉原子吸收光谱法(80-90s)。铬、镍和银的回收率分别为94．0％～103．0％、98．5％-104．0％和95．0%-104．0％,符合测定要求。     

石墨炉原子吸收光谱法测定涂料中的铅

采用干灰法消化涂料样品，建立了测定涂料中铅含量的石墨炉原子吸收光谱法。讨论了灰化温度、原子化温度对测定铅的影响。铅的浓度在0．6～3．0μg／L范围内符合比尔定律，相关系数r=0．9996，涂料样品测定结果的RSD为1．3％，加标回收率为99．2％～102．1％。     

火焰原子吸收法测定钴基合金喷粉中铁的含量

建立了一种用空气-乙炔火焰原子吸收法测定钴基合金喷粉中铁含量的分析方法,探讨了硅对铁测定的干扰机理,对用氯化钙作为硅干扰铁测定的释放剂进行了试验。该方法测定铁含量的线性范围为O～10mg/L,线性相关系数为0．9980。对含铁2.29％的钴基合金喷粉标准样品进行测定,测定结果的相对标准偏差为2．28％(n=6)．加标回收率为95．0％～104.0％。     

一次溶矿、两种方法联用测定地质样品中的金

主要研究了将氢醌容量法和原子吸收光谱法结合起来,实现一次溶矿,两种方法联用测定金含量。即在氢醌滴定基础上,王水氧化零价金,甲基异丁基酮(MIBK)萃取,火焰原子吸收法测定,准确检测出0.50g/t以下的低含量金。结果表明,方法简便、快速,不需二次溶矿。分析有证标准物质的结果与推荐值一致,样品加标回收率可达到96%以上,符合国家地质勘查管理规范的要求,精密度和准确度均能满足分析要求。适用于地质找矿中批量样品金的测定,已应用于实际样品分析,结果令人满意。     

Single granular activated carbon microextraction and graphite furnace atomic absorption spectrometry determination for trace amount of gold in aqueous and geological samples

A new and simple method was developed for preconcentration trace amount of gold in aqueous and mineral samples. The method was based on the sorption of gold on granular activated carbon (AC) in acidic medium (hydrochloric acid) and subsequently direct determination by graphite furnace atomic absorption spectrometry (GFAAS). A small particle of adsorbent was delivered to small volume of sample. After extraction, AC removed and analyzed directly by GFAAS. Several factors influencing the extraction efficiency, such as the hydrochloric acid concentration, sample volume and extraction time were studied as well as effect of potential interfering ions. The preconcentration factor 50 was obtained. The limit of detection (LOD) of gold in water and soil samples was 0.007 μg L^− 1 and 0.9 ng g^− 1, respectively. The proposed method was applied successfully to the determination of trace amount of gold in environmental and geological samples. In order to validate the developed method, two certified reference materials: Platinum Ore (SARM-7B) and Copper Ore Mill Heads (No. 330) were analyzed and the determined values obtained were in good agreement with the certified values and recovery was obtained in the range of 80-118%. The relative standard deviations (RSD) for the spiking levels of 0.5 μg L^− 1 in the real samples was 4%, (n = 15).     

Interference-free determination of trace levels of gold and palladium in geological and metallurgical samples by flame atomic absorption spectrometry coupled with a flow injection on-line microcolumn preconcentration and separation system

A simple and highly selective method was developed for the routine determination of trace or ultratrace amounts of gold and palladium in geological and metallurgical samples. The method uses flow injection on-line preconcentration and separation with determination by flame atomic absorption spectrometry. Au and Pd in the sample are adsorbed on a 2-mercaptopyrimidine chemically modified silica gel (MPMSG) packed microcolumn in a 0.50M HCl medium and then eluted with 0.5 or 1.0% thiourea solution. The eluates are introduced into the flame atomic absorption spectrometer directly. With the use of a 0.85 mL microcolumn (about 0.14 g MPMSG packed), the present system tolerated concentrations of common base metal ions up to 25.0 mg/mL and concentrations of anions up to 100.0 mg/mL when Au(III) at 0.100 microg/mL and Pd(II) at 0.200 microg/mL were preconcentrated for 60 s with a sample flow rate of 5.0 mL/min. The limits of detection were 3.1 ng/mL for Au(III) and 6.1 ng/mL for Pd(II) with relative standard deviations of < or = 2.5%. The analytical results obtained by the proposed method for geological and metallurgical samples were in good agreement with the certified values.     

泡沫塑料吸附-电感耦合等离子体发射光谱法测定地质样品中的金

建立了泡沫塑料吸附-电感耦合等离子体原子发射光谱法测定地质样品中的金的方法,采用王水溶解地质样品中痕量的金,经泡沫塑料吸附富集,结合电感耦合等离子体原子发射光谱法进行测定。实验表明,方法的加标回收率为94.4%~111.0%,对国家一级标准物质进行测定,结果与认定值一致,方法的相对标准偏差RSD为3.2%~12.8%。     

Electrothermal vaporization inductively coupled plasma atomic emission spectrometry determination of gold, palladium, and platinum using chelating resin YPA(4) as both extractant and chemical modifier

A new method for determination of trace gold (Au), palladium (Pd), and platinum (Pt) in environmental and geological samples by electrothermal vaporization (ETV)-inductively coupled plasma atomic emission spectrometry (ICP-AES) with the use of chelating resin YPA₄ as both solid phase extractant and chemical modifier has been developed. The resin loaded with analytes was prepared to slurry and directly introduced into the graphite furnace without any pretreatment. The factors affecting the vaporization behaviors of Au, Pd, and Pt were investigated in detail. It was found that, in the presence of YPA₄, Au and Pd could be quantitatively vaporized at lower vaporization temperature of 1900 °C. Compared with the conventional electrothermal vaporization, the vaporization temperature was decreased by 700 °C, and the detection limits for Au and Pd was decreased by a three-fold. However, a little effect of YPA₄ on the ETV-ICP-AES determination of Pt was found. Under the optimized conditions, the detection limits (3σ) of Au, Pd, and Pt for this method are 75, 60, and 217 pg, respectively; and their relative standard deviations (R.S.D.) are 4.4, 5.6, and 3.7%, respectively (n=9, C=0.2 μg ml⁻¹). The proposed method has been applied to the determination of trace Pd and Pt in sewage sludge, and the results well agreed with the recommended values. In order to further verify the accuracy of the developed method, a GBW07293 certified geological reference material and an auto catalyst NIST SRM 2557 reference material were analyzed, and the determined values coincided with the certified values very well.     

Rapid determination of gold in geological samples using flow injection solid-phase chemiluminescence.

The solid-phase chemiluminescence analysis of gold on the surface of an anion-exchange resin was studied. A method for the fast determination of gold using flow injection was established. The anion-exchange resin was used as an adsorbent of gold ion in the form of AuCl4-. The cation-exchange resin was used for the on-line separation of cations in the matrix. To obtain the best results, the preconcentration and separation conditions, chemiluminescence conditions, interfering ions and their elimination conditions were optimized. The linear range of the calibration curve of AuCl4- is from 0 microg ml(-1) to 5.00 microg ml(-1). The detection limit of AuCl4- is 0.012 microg ml(-1). The method has been used for the determination of gold in geological samples (standard ores). The results are in agreement with certified value of gold standard samples with relative standard deviation from 2.22% to 8.97%. Through the use of flow injection, the preconcentration and separation can be performed automatically.     

氧化石墨烯/壳聚糖微球吸附-电感耦合等离子体质谱法测定地质样品中痕量钽EI北大核心CSCD

建立了氧化石墨烯/壳聚糖微球吸附-电感耦合等离子体质谱法测定地质样品中痕量Ta的方法。合成了氧化石墨烯/壳聚糖微球,将其应用于地质样品中痕量Ta的分离富集,采用电感耦合等离子体质谱对富集后的试液进行测定。对氧化石墨烯含量、配体种类和浓度、pH、吸附时间、吸附剂用量等吸附条件和洗脱剂类型、体积、洗脱时间等洗脱条件进行了优化,在优化的条件下,对地质样品标准物质进行测定,Ta的方法检出限为2.0 ng/g,富集倍数为26.7倍。     

Gold and silver determination in Waters by SPHERON® Thiol 1000 preconcentration and ETAAS

A reliable procedure for the electrothermal atomic absorption spectrometry (ETAAS) determination of gold and silver in waters at trace level is described. The method is based on prior separation and preconcentration of the metals using a chelating sorbent SPHERON® Thiol 1000 after acidification of water samples (pH < 3) with nitric acid. Optimization of analytical variables during enrichment and ETAAS determination of the metals are discussed. The accuracy of the method is verified by analysis of certified reference materials. The limits of determinations based on 10 σ definition were 0.005 ng cm^?3 for Au and 0.02 ng cm^?3 for Ag. Precision of studied elements determination expressed by relative standard deviation varied in the range from 2.9 % to 16.4 %.     

电感耦合等离子体质谱(ICP-MS)法测定地球化学样品中的痕量金

采用王水体系对地球化学样品进行水浴消解,聚氨酯泡塑吸附富集,硫脲解脱,电感耦合等离子体质谱(ICP-MS)法测定地球化学样品中的金元素。采用调谐液调节ICP-MS仪器至最佳化,以GAu-11b为标准,单点校正直接测定。对痕量金标准物质(GAu-12、GAu-13、GAu-11b、GAu-10a、GAu-2b、GAu-7b、GAu-8a)的分析结果与标准值相一致,方法相对标准偏差(RSD,n=12)为4.8%~6.7%。方法检出限为0.015ng/g,加标回收率为85.5%~100%。与常规石墨炉原子吸收光谱法测定方法相比较,ICP-MS法操作简单快捷、试剂用量少、信背比高,有利于大批量地球化学样品快速测定。