微波消解-ICP-MS测定土壤和底泥中的12种金属元素

以20.0μg/L铟作内标,采用硝酸-氢氟酸-过氧化氢体系微波消解,ICP-MS(电感耦合等离子体质谱法)同时测定土壤和底泥中的12种金属元素,各元素方法检出限为0.003～0.2μg/g,相对标准偏差小于6.1%,土壤标准样品的测定值与标准值吻合。方法简便快捷,灵敏度高,重现性好,是分析大批量土壤和底泥样品中多元素的可靠、高效方法。     

微波消解ICP-MS法测定宣威和富源土壤中的微量元素

建立了微波消解-ICP-MS法测定土壤中32种微量元素的方法。采用氢氟酸-硝酸-过氧化氢体系微波消解,稀释定容后用ICP-MS对溶液进行元素的测定,在优化仪器工作参数后,以双内标铑(Rh)和铼(Re)进行校正。元素检出限为0.01～0.45ng/ml,测定国家标准物质西藏土壤成分分析标准物质GBW 08302中的元素,测定值与标准值或参考值基本一致,用该法测定云南宣威和富源两地24份土壤样品结果表明,该方法快速、简便、准确,适于土壤中多种微量元素的测定。     

土壤中总铬测定方法改进

采用《土壤质量总铬的测定火焰原子吸收分光光度法》(GB/T 17137-1997)测定土壤中总铬时,需用硫酸、硝酸、氢氟酸消解,再用盐酸溶液定容.由于硫酸的共沸最高温度为317 ℃[1],在熔样时要将硫酸产生的SO3完全赶尽较困难,现用硝酸-氢氟酸-高氯酸消解土壤的标准样品和实际样品,同时消解并绘制工作曲线(简称工作曲线法),再通过标准加入法测定样品,可取得较为满意的结果.     

密闭微波消解电感耦合等离子体发射光谱(ICP-AES)法同时测定大气颗粒物PM10中的18种无机元素

建立了测定大气颗粒物PM10中18种无机元素的密闭微波消解电感耦合等离子体发射光谱法。考察了微波消解体系和消解条件,选取了适宜的仪器工作条件和最佳的分析谱线,合理地进行了背景扣除,并对共存元素的干扰情况进行了研究。样品采用硝酸-盐酸-过氧化氢-氢氟酸体系进行消解并经饱和硼酸溶液络合后上机测定,测定值与参考样品标准值相符,主量元素的方法精密度(RSD%)小于3%,次量、微量元素的方法精密度小于10%。各元素的检出限在0.0001~0.0141mg/L之间,回收率在90%~110%之间,应用建立的方法对北京市的颗粒物膜样品进行了分析。     

火焰原子吸收法测定河流沉积物中微量铜,铅,锌,镉,镍

河流沉积物中微量金属元素的原子吸收测定法已有报道,通常采用的分解方法是用高氯酸—氢氟酸—硝酸混合酸体系消解.但此法的分解效果不是很好,分解液中往往有油脂状物质残留,分解后期会出现溅暴现象,影响测定结果的重现性和准确性.本文研究了用氯酸—氢氟酸—硝酸混合酸体系分解河流沉积物样品.与上述方法比较,此方法分解效果好,分解液澄清,没有油脂状物质残留;操作方便,避免了溅暴现象.     

高压密闭消解土壤砷、汞、铅、镉酸体系比较

采用高压密闭消解系统消解土壤,氢化物发生-原子荧光光谱法(HG-AFS)测定As和Hg,石墨炉原子吸收光度法(GF-AAS)测定Pb和Cd,对比了不同消解酸体系对国家土壤标准参考样中As、Hg、Pb、Cd的消解效果。结果表明,盐酸-硝酸体系对As、Hg、Pb和Cd的消解平均回收率分别为26.1%、100.6%、69.7%、87.3%;硝酸-高氯酸-氢氟酸体系中As、Hg、Pb和Cd消解平均回收率分别为109.9%、84.7%、87.5%、90.1%;硝酸-双氧水体系对Hg、Pb、Cd消解平均回收率分别为104.8%、95.1%、93.3%,对As的回收率虽只有69.2%,但数据精密度最好。此外,从简化试验步骤,减少误差,提高检测效率及减少试验危险性等方面综合评价,认为硝酸-双氧水消解体系是采用高压密闭系统消解土壤重金属的最理想酸体系。     

微波消解-氢化物发生原子荧光光度法 测定土壤中的砷

建立了微波消解一氢化物发生原子荧光光度法测定土壤中砷的方法。对微波消解条件进行了优化，用5mL硝酸和2mL过氧化氢的混合酸作消解溶剂，在设定的微波条件下砷提取完全。用5％的盐酸作为反应载流，12g／L硼氢化钾与0．5％氢氧化钠的混合液为还原剂，直接定容后应用HG．AFS测定，并通过测定国家标准参考物质和加标回收实验，对方法进行了验证。实际土壤加标同收率97％～103％。     

不同酸消解体系测定大气颗粒物中的镉

采用微波消解-石墨炉原子吸收分光光度法测定北方某市环境空气PM10及PM2.5样品中的镉,并比较了硝酸-盐酸体系与硝酸-过氧化氢体系的消解效果。结果表明,硝酸-盐酸体系与硝酸-过氧化氢体系的方法检出限分别为0.006、0.008μg/L,相对偏差分别为5.4%、7.9%,加标回收率为85%~110%,其检出限、精密度与加标回收率均满足要求。2种消解体系均能较好地提取颗粒物中的镉,测定结果无显著差异(P0.05),但硝酸-过氧化氢体系更适合作为多种分析仪器测试通用的前处理体系。     

全自动消解-石墨炉原子吸收法测定土壤中镉的探讨

探讨全自动消解-石墨炉原子吸收法测定土壤中镉的方法。选用硝酸-氢氟酸-高氯酸作为消解体系,采用全自动消解仪对土壤样品进行消解,通过研究干燥、灰化和原子化温度对吸光度的影响,优化出最佳的石墨炉升温程序,依据国标方法 (GB/T17141-1997)石墨炉原子吸收分光光度法测定土壤样品中的镉元素含量。该方法检测土壤国家标准物质GSS-8、 GSS-22、GSS-24等,所得结果与标准值相吻合。方法简便、快速、重现性好、灵敏度高,适用于批量土壤样品中Cd的测定。     

一次微波消解测定土壤中铬铜锌铅镉

测定土壤中铬、铜、锌、铅、镉多采用传统电热板加热消解方式进行样品处理，但不能同时一次消解．笔者尝试使用微波一次消解测定五种元素，试验结果令人满意．     

石墨炉原子吸收法测定环境空气中的锡

研究了硝酸-双氧水体系消解、石墨炉原子吸收法测定环境空气中锡的方法.采用抗坏血酸和磷酸二氢铵作混合基体改进剂,热解涂层石墨管,塞曼扣背景.方法的检测限为3.56 μg/L,实际样品回收率为90.6％～102％.     

微波消解-ICP/MS法同时测定水产品中13种元素

用硝酸-双氧水体系微波消解，以In、Sc为内标，采用电感耦合等离子体质谱法（ICP／MS）同时测定水产品中V、Cr、C0、Ni、Cu、Zn、As、Se、Cd、Sb、Ba、T1、Pb等13种元素。各元素的检出限在0．05ng／g～0．064μg／g之间，样品平行测定4次的RSD〈5％，鲢鱼样品的加标回收率在81％～117％之间。     

Soil Lead and Other Metal Levels in Industrial, Residential and Nature Reserve Areas in Singapore

The use of pressure feedback microwave digestion technique has permitted rapid and efficient digestion of soil and sediment samples. The evaluation of different acid mixtures to digest soil samples were studied by mixed-level orthogonal array design. The selected acid mixture of HCl-HNO3-HF was employed in the survey of Pb, Zn, Cu, Cr and Mn in soil samples. Surface soil samples were collected from industrial, residential and nature reserve areas in Singapore. The five metal concentrations were determined by flame atomic absorption spectrometry and graphite furnace atomic absorption spectrometry. The lead and other metal contents in NBS SRM 1645, NIES CRM No. 2 and NRCC BCSS-1 sediment standard references were determined concurrently with the survey samples. Five measured metal loading on the surface soils was in the order: industrial area > residential area > nature reserve area. The trace metal concentrations in surface soil from areas of heavy traffic are higher than those from residential areas. The main sources of trace metal pollution are vehicular exhaust and industrial activities.     

土壤和底泥中砷、铬、锰测定的前处理技术

试验了土壤和底泥中砷的前处理技术，其目的是能对土壤、底泥中砷、铬、锰在一次前处理中制备成试液，比色法分析。试验表明，用Ｈ２ＳＯ４－Ｈ３ＰＯ４－Ｈ２Ｏ２进行前处理是可行的。方法简单、挥发酸雾少，用标准参考物质检验证明，分解完全，数据准确，有粒较好一致性。     

底质样品微波消解总磷测定研究

使用硫酸_高氯酸在微波消解系统消解 ,以钼锑抗比色法测定底质中的总磷 ,通过实验确定最佳消解及分析条件。结果表明 ,该方法快速简便并有较高准确度、精密度和较低的检测限 ,值得推广和应用。     

增压溶样－冷原子荧光法测定煤样中的汞

采用增压溶样器加７：３：５的ＨＮＯ３－Ｈ２ＳＯ４－ＨＣｌＯ４混合酸处理煤样．用冷原子荧光法测定煤样中的总汞含量。该法的加标回收率为９２．７～１１２．５％，结果令人满意。     

Antimony speciation in terrestrial plants. Comparative studies on extraction methods

A suitable method for the extraction of antimony species from plant materials prior to IC-HG-AFS analysis is presented. The extraction efficiency with different extraction systems using various aqueous and aqueous/solvent mixtures was initially evaluated by analysing the Virginia Tobacco Leaves Certified Reference Material. The concentration of antimony extracted was compared with the total antimony content in the plant material measured by HG-AFS after focused microwave-acidic digestion using HNO3 and H2O2. The proposed extraction procedures were applied to antimony speciation in several plants from a natural terrestrial environment impacted by mining activities. End-over-end agitation (4 h) followed by sonication (1 h) extraction using 0.1 mol l(-1) citric acid was found to provide the best extraction efficiency while also giving reliable speciation information. Both inorganic and methylantimony species were found in the extractable portion of some terrestrial plants.     

Synthesis of HNO3 from Organic Matter and its Influence on Nutrient Replenishment in Forest Soils

Chemical analyses during a decade of bulk precipitation, throughfall, humus water and soil water in forest plots ranging from sand to silt of Pleistocene origin in Flanders (N-Belgium) prove that previous and present weathering is predominantly due to synthesis of HNO3 from soil organic matter. The HNO3 reacts with silicates and possibly PO4(3-) species, releasing Al, Fe, nutrient base cations and H2PO4-, and is transformed into NO3-. In all soils solubilized Al3+ is predominantly associated with NO3- and with some organic bases in the coarse-textured soils with undisturbed or previously plowed spodic B horizon. The amounts of ions leached, especially Al3+ and NO3-, are much higher in the sandy than in the silty soils as a result of a stronger neutralization of acidity in the silty soils. Nutrients, leached from the soil, have to be replenished in some way for a sustained forest growth. N- and S-species must come from the atmosphere. Basic cations and P-species have to be supplied out of the solid phase. The concentrations of NO3- in the soil water show that the liberation of these elements from the solid phase is performed by HNO3. Especially in the coarse-textured soils the need for NO3- is high. Therefore, instead of being a real hazard for the forest ecological system, supplementary addition of HNO3 or NH3 can be beneficial.     

微波消解-电感耦合等离子体质谱法同时测定废水中20种元素

采用微波消解-电感耦合等离子体质谱法,同时测定了废水中Be、V、Cr、Mn、Co、Ni、Cu、Zn、As、Se、Mo、Ag、Cd、Sb、Ba、Hg、Tl、Pb、Th、U等20种元素,比较了5种不同消解体系对废水样品的加标回收结果,确定采用硝酸+过氧化氢消解体系。Hg在0.050μg/L～2.00μg/L、其他元素在5.00μg/L～500μg/L范围内线性良好,检出限为0.01μg/L～0.2μg/L,国家有证标准物质的测定结果符合要求,废水样品平行测定的RSD为2.6%～6.5%,加标回收率为84%～110%。     

火焰原子吸收法测定土壤中的铅

建立了一种以 HNO3-HCl-HCl O4 -HF对土壤样品进行消化 ,火焰原子吸收测定铅的方法。该法用于实际样品的测定时 ,相对标准偏差小于 2 .3 % ,加标回收率为 98%～ 1 0 2 %。