ICP-AES detection of silicon carbide impurities volatilized in a graphite furnace with the use of carbon tetrachloride vapour

The analytical capability of high-temperature halogenation with carbon tetrachloride vapour in a graphite furnace was investigated for silicon carbide powder with known chemical composition and particle size. Intensity vs heating time curves were determined for analytical lines of Al, B, Ba, Ca, Cr, Cu, Fe, Mg, Mn, Ti, V and Si constituents, volatilized with and without the presence of CCl₄ vapour in the furnace atmosphere. Igniting 10 mg SiC at 2100 °C for 60 s in chlorinating atmosphere, the evaporated fraction of most of the constituents was higher than 90% (for Al about 50%). The line intensity vs sample mass (4–26 mg) relationships were linear for all impurities studied, while the intensity of silicon line showed a relatively small change with the sample mass. BEC (background equivalent concentration) values for this solid sampling technique (10 mg loaded sample) were 2–20 fold lower than those calculated for the conventional solution sample introduction method.     

An Interlaboratory Comparison of a Standardised EDTA Extraction Procedure for the Analysis of Available Trace Elements in Two Quality Control Soils

Abstract

A standardised EDTA extraction procedure was tested collaboratively by six laboratories using two in-house reference soils identified as soil A and soil B. The extracts were analysed for Zn, Cu, Pb and Mn by Inductively Coupled Plasma Spectrometry. Concentrations of extractable elements in soil A were generally much lower than those found in soil B. All laboratories produced some extreme outlying results, most of these were produced in soil B. Results for Mn were the most variable, with a range of 63.4–100.3 μg g^?1 in soil A and 226.4–415.3 μg g^?1 in soil B. In both soils, one laboratory reported high values for Zn and Mn and, one laboratory, for soil B, produced values for all four elements which were consistently low.

If outlying results are ignored, the results from most laboratories were in reasonable agreement for all elements except Mn.     

流动注射在线萃取-有机相ICP-AES法测定矿石中的痕量金

提出了一种流动注射在线萃取－有机相ＩＣＰ－ＡＥＳ法测定矿石中痕量金的分析方法,研究了流动注射在线萃取与ＩＣＰ－ＡＥＳ法的联用技术,设计了在线萃取流路,优化了各项化学条件及流路参数。该方法操作简便,快速,检出限为０．００１μｇ／ｍＬ,相对标准偏差（ＲＳＤ）为３．４％,应用于矿石中痕量金的分析,获得满意的结果。     

ICP-AES 法测定 RZnAl5RE 合金中的镧、铈、铁、铝、铅、镉

采用ＩＣＰ－ＡＥＳ测定了ＲＺｎＡｌ５ＲＥ合金中的Ｌａ、Ｃｅ、Ｆ３、Ａｌ、Ｐｂ、ＣＤ元素含量。考察了基体及无机酸浓度对６种元素线强度的影响。选择了仪器工作条件,检出限在０．０３～１．００μｇ／Ｌ之间,加标回收率为９３％～１０８％,相对标准偏差小于１２．６８％（ｎ＝１０）。     

碱溶ICP—AES法同时测定AISi／SiC复合材料中的高含量硅和低含量？…

本文采用碱溶ＩＣＰ－ＡＥＳ法对ＡＩＳｉ／ＳｉＣ复合材料中的高含量硅和低含量镁、钛、铁的测定进行研究,着重进行基体元素铝及特测定元素硅、镁、钛、铁之间的干扰试验,进行了碱度试验和酸度试验,测定和ＡＩＳｉ／ＳｉＣ复合材料中的硅、镁、钛、铁含量,得到了较好的精密度和准确度。方法简便可靠,可获得满意的分析结果。     

微晶萘固液萃取分离和ICP-AES测定痕量金的研究

在一定酸度的盐酸介质中,络阴离子ＡｕＣｌ－４与孔雀绿（ＭＧ）形成稳定的离子缔合物,可被析出的微晶萘定量吸附,实现痕量金的分离与富集。分离了基体富集物中的Ａｕ,并用ＩＣＰ－ＡＥＳ测定。详细考察了影响金的分离与测定的各种因素。在优化的实验条件下,方法的检出限为６．０ｎｇ／ｍＬ,ＲＳＤ为１．３４％（ｎ＝９）。本法已用于矿石浸取液和标准矿样中痕量金的测定,分析结果满意。     

微波消解-ICP-AES同时测定不同产地红枣中的微量元素

采用HNO3-H2O2作消解剂进行微波消解,利用ICP-AES同时测定不同产地红枣中Fe、Mg、Mn、Cu、Al、Zn等元素,对样品的前处理条件进行了探讨,通过加标回收实验,验证了分析数据的可靠性,在最佳测定条件下,方法检出限为0.0005—0.0100μg.mL-1,加标回收率为90.0%—103.6%,相对标准偏差≤4.2%。结果表明,该方法快速、简便、数据准确可靠,结果令人满意,适合常规分析。     

植物样品消解后残留颗粒物元素组成研究

分别采用干灰化法和湿消化法处理植物标准参考物质灌木枝叶组合样(杨树叶和茶叶),用扫描电镜(SEM)对消解液中残留的不溶性颗粒物微观形貌进行了观察,并用SEM附属的X能谱仪研究了颗粒物的主要元素组成。另外,还用BCR法对茶叶残留颗粒物进行了分级萃取, 相关元素在四种存在形态中的含量分布状况由AAS和ICP-AES给出。研究结果表明：不同消解方法对颗粒物微观形貌有较大影响,其中植物样品经干灰化法处理后残留的颗粒物多呈灰黑色,表面疏松多孔;经湿消化法处理后残留的颗粒物均呈白色,多数结构紧密,数量也相对较少。不同植物样品残留的颗粒物元素组成均大同小异,主要为Si和Al,此外还有少量的Ca, Fe, K, Ti等。这些元素在颗粒物中存在形态不一,致使在进行植物样品分析时某些元素含量测定结果大为偏低。     

基于离子交换分离的ICP发射光地测定地质样品中的微量锆,铪研究

在 2 %酒石酸介质中 ,用阳离子交换树脂吸附干扰元素 ,富集的锆和铪直接以 ICP- AES法定 ,锆的检出限为 0 .3× 1 0 - 6,铪为 0 .4× 1 0 - 6。本方法简便、快速 ,应用于分析地球化学标准物质中微量的锆和铪 ,结果满意。     

模拟增温与氮沉降对蒙药阿给12种必需元素分配的影响

联合国政府间气候变化专门委员会(IPCC,2007)指出,伴随着全球变暖,氮沉降的现象也日益加剧。通过野外控制实验,使用红外辐射器增温(+2℃)和人工添加NH4NO3(+10g N·m-2.a-1),模拟未来气候变暖与氮沉降状态,设计对照(CK)、增温(IR)、施氮(N)、增温施氮(IRN)四种处理,结合ICP-AES法研究气候变暖与氮沉降对传统蒙药材——阿给12种必需元素在生殖(营养)部位中分配的影响。结果表明:增温与施氮处理改变阿给对必需元素的吸收与分配。增温条件下12种元素含量虽有波动,但基本上呈现出负效应大于正效应的趋势。施氮处理明显改善磷、锰的吸收。同时,增温与施氮处理之间的交互作用不显著。生殖枝与营养枝之间,只有氮、钾、钙、镁四种元素表现出显著性差异。