DMA-80测汞仪直接测定固体样品中的汞

利用DMA-80测汞仪直接测定固体样品中的汞,采用升温加热直接进行热分解、金汞齐反应,采用长、短双检测池,可直接测定固体、液体样品,汞含量在0.n~600.0ng/g范围内的样品都能准确地测定,每个样品测定时间约为5min。测定结果证明方法具有可靠性。     

DMA-80测汞仪的应用探讨

本文的主要实验目的是利用DMA-80测汞仪直接测定固体样品中的汞并证明其方法可靠。采用升温加热直接进行热分解、金汞齐反应,采用长、短双检测池,可直接测定固体、液体样品,汞含量在0.n×10-9～600.0×10-9范围内的样品都能被很准确地测定,每个样品测定时间约为5min。 测试结果证明其方法具可靠性。     

催化热解-冷原子吸收分光光度法测定大米中的汞含量

建立冷原子吸收分光光度法测定大米中汞含量的方法。采用DMA–80直接测汞仪,大米样品经干燥、分解灰化、还原等过程,直接进入冷原子吸收光谱仪进行测量。干燥温度为200℃,热解温度为650℃。该方法的检出限为0.001 ng/g,加标回收率为85.0%～99.2%,测定结果的相对标准偏差为0.25%～3.70%(n=6)。利用标准物质和原子荧光法进行比对试验,测定结果均在误差范围内。该方法测定结果准确,灵敏度高,重现性好,适用于大米中汞含量的测定。     

碳酸钙固硫固体进样测汞仪快速测定硫化铅精矿中汞

在使用固体进样测汞仪直接测定硫化铅精矿中汞时,由于试样中硫含量通常较高(高达30%以上),在测定过程中大量的硫被氧化会污染甚至腐蚀固体进样测汞仪的核心部件催化管,导致催化管寿命严重缩短。为解决该问题,建立碳酸钙固硫-固体进样测汞仪直接测定硫化铅精矿中汞的分析方法;并对Ca/S比,分解温度,分解时间,齐化时间等参数进行优化。在最优条件下,Hg的含量在2~20 ng和20~500ng线性范围内回归系数(R²)分别为0.9996和0.9998;方法检出限(LOD)为0.006 μg/g。用该法对3个典型样品进行测定,相对标准偏差RSD≤9%(n=7),加标回收率为96%~106%。该方法简单、快捷,准确度和精密度高,适合硫化铅精矿中汞的快速测定。     

固体进样直接测定法测定铜精矿中汞

建立了固体进样直接测定法测定铜精矿中汞含量的方法。铜精矿样品在测汞仪的分解炉中经300℃干燥和750℃高温热分解后,汞被催化分解为汞原子,于850℃齐化成金汞齐。汞蒸气被氧气流带入单波长光学吸收池,在波长253.7 nm处测量汞的吸光度,采用标准曲线法计算汞量。方法的线性范围分别为0~1.00,0~100μg/mL,线性相关系数为0.9999,检出限分别为0.10,0.04 ng/g。5个汞含量不同的铜精矿样品测定结果的相对标准偏差为2.14%~4.35%(n=11),样品加标回收率为92.00%~104.02%。采用该方法分别对2个铜精矿样品和铜精矿国际标准物质进行测定,测定结果与标准分析方法测定值和标准物质标示值基本一致。该方法简便、快速、准确,可以作为标准方法推广使用。     

测汞仪直接测定食品中总汞

建立了食品中总汞快速准确的测定方法。使用测汞仪,采用样品直接进样法,对芹菜、大葱、鸡肉等10种标准物质中的汞含量进行了测定,结果表明,在0.2~100ng范围内线性良好,10种标准物质的检测结果均在标示值范围内。使用测汞仪直接测定食品中总汞含量,具有灵敏度高、快捷、不受前处理影响等优点,便于推广,适用于各类食品中总汞的快速测定。     

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。     

催化裂解-金汞齐富集-冷原子吸收光谱仪测定土壤样品中总汞含量

为建立采用催化裂解-金汞齐富集-冷原子吸收光谱仪即直接测汞仪测定土壤样品中汞含量的方法,本研究配制汞总量为0~2 ng、0~15 ng和25~1023 ng的三种不同汞浓度系列的标准工作曲线,选取9个土壤样品,3种国家土壤有证标准物质,同一样品分别进行6组平行测定,并抽取3个土壤样品进行3种不同浓度加标回收试验,以对其方法精密度和准确度进行论证。 结果显示：仪器信号值与Hg总量之间均呈良好的线性关系。根据仪器多次测定空白数据结果,按照称样量0.1 g计算,方法最小检出量为0.09 ng/g;平行测定结果相对标准偏差均小于10%,土壤标准物质测定值与标准物质标准参考值均相符,不同浓度的加标回收率范围为78.4%～92.7%。结果表明催化裂解-金汞齐富集-冷原子吸收光谱仪,可用于批量土壤样品中汞含量的快速测定分析,方法的精密度和准确度可满足测定分析要求,且实验过程中无需前处理消煮,操作方便、快速高效。     

脉红螺中痕量汞分析方法的研究

为建立DMA-80直接测汞仪测定脉红螺中痕量汞的最优分析方法,通过正交实验优化了仪器分析程序,通过设置进样量梯度,确定了脉红螺样品的最佳进样量。结果表明:DMA-80最优分析程序为:干燥温度200℃,干燥时间150s,分解温度650℃,分解时间150s,齐化时间12s,氧气流量200mL/min,最佳进样量为0.1～0.2g(精确至0.000 1g),在0～20.0ng和20.0～1 400.0ng范围内均呈良好的二次拟合,相关系数为1.000,检出限为0.02ng。采用国际标准物质贻贝组织(NIST SRM2976)验证了方法的准确度和精密度,分析结果表明:加标回收率为95.1%～102%,相对标准偏差(RSD)为1.6%～2.2%,精密度和准确度优于海洋行业标准"HY/T147.3—2013"方法中的规定。方法简便快速,重现性好,准确度高,可用于脉红螺中痕量汞的实际检测工作。     

电热蒸发-直接进样-冷原子吸收光谱法测定土壤以及沉积物中汞

采用传统分析仪器测定汞元素,需要对样品进行化学消解,存在操作繁杂、效率低以及易交叉污染等问题。故建立了电热蒸发-直接进样-HGA-100测汞仪测定土壤以及沉积物中汞的方法,无需对样品进行化学前处理,降低环境污染。通过优化HGA-100测汞仪参数条件,汞质量浓度在0~20ng以及20~200ng,相关系数优于0.998,准确称量样品0.05g(精确至0.000 1g),方法检出限为0.5μg/kg,相对标准偏差1.6%~4.6%,加标回收率在90.1%~100%。方法用于对土壤和沉积物标准物质测定,结果与标准值相符。方法高效、准确,可用于测定土壤以及沉积物中的汞。     

微波萃取高效液相色谱-冷原子荧光光谱法测定沉积物中甲基汞和无机汞

建立了微波萃取高效液相色谱-冷原子荧光光谱法(MAE-HPLC-CVAFS)测定沉积物中甲基汞(MeHg+)和无机汞(Hg2+)的方法。以0.1%(V/V)2-巯基乙醇为萃取剂,用于沉积物样品中汞形态的萃取,在80℃下萃取8 min,萃取液直接注入HPLC-CVAFS系统分析。在优化条件下,MeHg+和Hg2+的检出限分别为0.58和0.48 ng/g;加标回收率分别为96.2%和95.8%;RSD(n=6)分别为5.7%和4.1%。对标准参考物质(IAEA-405和ERM-CC580)的分析结果与推荐值一致。本方法简单、快速、准确、检出限低,抗干扰能力强,具有很好的实用性和推广价值。     

Mercury determination with ICP-MS: signal suppression by acids

When mercury is quantified by ICP-MS under routine conditions (external calibration) in reference materials, which require mineralization with nitric acid, the experimental concentrations are almost always unacceptably low in comparison to certified values. Sorption of mercury on the Teflon surfaces of the digestion vessels, changes in the viscosity of the aspirated solutions, in the efficiency of the nebulization, in the aerosol transport, and memory effects cannot be responsible for the low results. The intensity of a mercury signal is strongly dependent on the concentration of nitric acid (and other mineral acids) in the measured solutions. Correct results for mercury in the SRM GBW-90101 (Chinese human hair; 2.16+/-0.21 mg Hg/kg certified) can only be obtained, when the solutions, with which the external calibration curves were established, have exactly the same nitric acid concentration as the aspirated digests (2.03+/-0.01 mg Hg/kg; n = 5), when mercury is determined by the standard addition method (2.10+/-0.01 mg Hg/kg; n = 5), or when the experimental mercury concentration obtained at a nitric acid concentration in the digest, different from the concentration in the external calibration solutions, is corrected mathematically based on a pre-established function [Hg2+] = f [HNO3]. The concentrations found by this mathematically based correction 2.04+/-0.01 mg Hg/kg (n = 5) is in good agreement with the values obtained by acid matched calibration or by the standard addition method. For practical work with large numbers of samples the mathematical correction appears to be the method of choice. For occasional mercury determinations, the standard addition method seems to be the most practicable.     

氧弹燃烧–原子荧光光谱法测定煤中汞含量

建立氧弹燃烧–原子荧光光谱法测定煤中汞含量的方法。用氧弹燃烧分解样品,汞释放后以硝酸溶液吸收,以0.5 g/L硼氢化钾溶液作为还原剂,体积分数5%的硝酸溶液为载流液,用原子荧光光谱法定量测定。方法检出限为0.02μg/kg,对标准物质GBW 11156(标准值0.32μg/g)进行平行测定,测定结果的平均值为0.318μg/g,相对标准偏差为7.3%(n=6),加标回收率为91.5%~106.5%。该方法简单、干扰少,准确度和精密度良好,可用于煤中汞的测定。     

环境样品的热解-溶液吸收预处理及其汞同位素组成的测定

利用多道接收电感耦合等离子体质谱仪(MC-ICP-MS)可实现汞同位素的高精度测定,但对样品预处理的要求很高。目前,液态、固态、气态环境样品的预处理方式不一,存在一定的系统误差。该研究旨在尽可能统一各状态样品的预处理步骤。先将各样品中的不同形态汞富集转化为固体可吸附态,令其吸附在固态载体上,包括:采用金柱富集气体样品中的气态单质汞;以吹扫-金柱捕集法富集液体样品中的溶解气态汞和总汞;用膜过滤法收集大气中的颗粒态汞。最后以管式炉热解定量固态样品,采用高氧化效率的酸性高锰酸钾混合溶液吸收热解产生的Hg~0并氧化为Hg~(2+),保存于溶液中供MC-ICP-MS测定。优化了气体流速、吸收液体积及高锰酸钾浓度等参数,考察了方法空白、回收率及精密度等指标,并将建立的方法应用于大气气态单质汞、大气颗粒态汞、溶解气态汞、雨水总汞和土壤总汞等样品中汞同位素的分析。     

Determination of Mercury in Urine and Seawater by Flow Injection Vapor Generation Isotope Dilution Inductively Coupled Plasma Mass Spectrometry

A simple and inexpensive laboratory-built vapor generator was used with inductively coupled plasma mass spectrometry (ICP-MS) for the determination of mercury in urine and seawater samples. The applications of vapor generation ICP-MS alleviated the non-spectroscopic interferences and the sensitivity problem of mercury determination encountered when the conventional pneumatic nebulizer was used for sample introduction. The concentration of mercury was determined by isotope dilution method. The isotope ratio of mercury was calculated from the peak areas of each injection peak. The repeatability of the peak areas and isotope ratio determinations of seven consecutive injections of 1 ng mL^?1 Hg solution were 2.3% and 2.2%, respectively. This method has a detection limit of 0.07 ng mL^?1 for mercury. This method was applied to determine mercury in a CASS-3 nearshore seawater reference sample, NASS-4 open ocean seawater reference sample, NIST SRM 2670 freeze-dried urine reference sample and several urine and seawater samples collected from National Sun Yat-Sen University. The results for the reference samples agreed satisfactorily with the reference values. Results for other samples analyzed by the isotope dilution method and the method of standard additions agreed satisfactorily. Precision was better than 10% for most of the determinations.     

Mercury characterisation in urban particulate matter

A five-step sequential extraction procedure was proposed in order to assess the distribution of mercury (Hg) forms in urban particulate matter (PM): exchangeable, HCl-soluble, organic-bound, elemental and other slightly soluble Hg species, mercury(II) sulphide (HgS), and residual Hg. This process was applied to the analysis of urban dust samples collected at locations in Prague (Czech Republic) with high traffic density. In addition to sequential extractions, thermal desorption analysis was performed. The differences in Hg concentrations between untreated and thermally treated samples were indicated as the thermally releasable amount of Hg. For the study of PM-adsorbing capacity, Hg vapours were passed through the samples as long as the enrichment of materials was observed. The retained elemental Hg was readily released by thermal desorption. All Hg analyses were based on the highly sensitive pyrolysis technique of atomic absorption spectrometry using the mercury analyser AMA-254.     

Determination of Mercury in Geological Materials by Continuous-Flow,Cold-Vapor,Atomic Absorption Spectrophotometry

Abstract

To determine mercury in geological materials, samples are digested with nitric acid and sodium dichromate in a closed teflon vessel. After bringing to a constant weight, the digest is mixed with air and a sodium chloride-hydroxylamine hydrochloride-sulfuric acid solution and then Hg(II) is reduced to Hg with stannous chloride in a continuous flow manifold. The mercury vapor is then separated and measured using cold vapor atomic absorption spectrophotometry (CV-AAS). For a 100 mg sample the limit of detection is 20 parts per billion (ppb) Hg in sample. To obtain a 1% absorption signal, the described method requires 0.21 ppb Hg solution (equal to 16 ppb in sample). Precision is acceptable at less than 1.2% RSD for a 10 ppb Hg aqueous standard. Accuracy is demonstrated by the results of the analysis of standard reference materials. Several elements do interfere but the effect is minimal because either the digestion procedure does not dissolve them (e.g., Au or Pt) or the; are normally of low abundance (e.g., Se or Te).