离子色谱法测定镍钴锰氢氧化物中硫酸根离子含量

建立了离子色谱法测定镍钴锰氢氧化物中硫酸根含量的方法。试样以盐酸溶解,挥发除去过量盐酸,经阳离子树脂柱去除金属离子,离子色谱法测定其中硫酸根离子的含量。方法操作简便快速,检出限低,样品测定具有较好的精密度,加标回收率为97%~103%。     

氧瓶燃烧离子色谱法测定氯化聚乙烯中氯含量

元素分析仪法是测定有机元素含量的现代分析技术,一次进样可以同时测定化合物中的C、H、N等元素的含量,在元素含量分析中发挥了重要作用,但该方法对卤族元素无法测定.氧瓶燃烧分解样品后用电位滴定法或称(容)量法测定有机卤素的含量,是有机卤素分析的经典方法.国家标准测定聚氯乙烯样品中的氯含量采用氧瓶燃烧分解电位滴定法[1].电位滴定法一次只能测定样品中一种卤离子,若多种离子同时存在会产生干扰,影响测定结果,且需要配制多种试剂,费时费力.有机样品或聚合物经氧瓶燃烧法分解后采用离子色谱法一次进样可以同时测定多种元素的含量而互不干扰[2],分析速度和灵敏度都优于传统方法.许多有机化合物或聚合物都含有卤素,离子色谱对卤素离子测定的灵敏度很高,氧瓶燃烧离子色谱法弥补了元素分析仪法的不足,是有机化合物或聚合物卤素含量分析较理想的方法.本实验以间氯苯甲酸元素分析标准样品为对照品,测定了氯化聚乙烯中的氯含量,取得满意结果.     

蔬菜中金属元素测定方法研究

采用微波消解处理样品,应用离子色谱UV-Vis检测和火焰原子吸收法分别测定了蔬菜样品中的金属元素Fe、Cu、Zn、Ni、Ca、Mn和Mg的含量。结果显示,离子色谱UV-Vis检测法测定结果准确,方便快捷。     

铅-锌-硼玻璃中氧化硼含量的测定方法探讨

由于铅、锌两元素均具有两性性质,铅锌硼玻璃样品中大量的铅离子和锌离子的存在会影响其B2O3含量的分析结果。本文通过实验验证,提出准确测定铅锌硼玻璃中B2O3含量的主要思路:在石墨坩埚中用氢氧化钾将玻璃样品熔融后用盐酸脱出,所得溶液逐步通过硫酸盐沉淀、碳酸盐沉淀和氢氧化物沉淀的方法去除大多数的铅锌离子,随后用0.1 mol·L-1EDTA(乙二胺四乙酸二钠)溶液络合的方法去除残余铅锌离子的存在对B2O3含量测定的影响,最后用酸碱滴定法测定样品中B2O3的含量。通过硼硅酸盐玻璃标准物质和铅锌硼玻璃样品对该方法进行B2O3含量测定的验证试验结果显示,该方法具有较好的准确性。     

碱融浸取–离子选择电极法测定固体废物中的总氟

采用氢氧化钠熔融浸取固体废物中的氟,用离子选择电极法测定其中的总氟含量。固体废物样品经氢氧化钠高温熔融后,以热纯水浸取并加入适量的盐酸使溶液呈弱碱性,去除主要干扰离子。测定氟的线性范围为5.00~500μg,线性相关系数r=0.999 6,检出限为12.5 mg/kg。6种类型固体废物样品的加标回收率在90.4%~110.0%之间,测定结果的相对标准偏差为2.3%~4.6%(n=6)。该方法样品预处理简单、重现性好、检出限低,适用于多种固体废物中总氟的测定。     

离子色谱法测定气体中痕量二氧化硫

建立了测定气体中痕量二氧化硫的离子色谱法。采用氢氧化钠–过氧化氢溶液为吸收液,将气体样品中痕量二氧化硫转化为硫酸根离子,以离子色谱法测定硫酸根离子,从而得到气体中二氧化硫含量。二氧化硫气体含量在1~100μL/L范围内与色谱峰面积线性关系良好,相关系数为0.999 9。二氧化硫的检出限为0.1μg/L,测量结果的重复性小于2%(n=6),测定标准样品的回收率在98.1%~99.6%之间,准确度优于对照方法。     

几种样品中溴与碘的离子色谱安培法测定

1 引言 许多样品通常要求测定溴和碘的含量,往往含量甚微,电导检测的离子色谱法达不到要求。本文研究了离子色谱安培法连续测定溴和碘的可行性,拟定了一个快速、简便,无干扰的、可同时测定各种样品中痕量溴和碘的方法。本法以艾斯卡半熔,抗坏血酸为还原剂,使样品中的碘全部转变成适合于离子色谱安培法检测     

土壤易溶盐浸提液中硫酸根和硝酸根的测定

对不同地区不同深度的土壤进行前期预处理,在最佳试验条件下,应用离子色谱法测定土壤浸提液中硫酸根和硝酸根的含量,测定的相对标准偏差分别为1.9%和3.0%,加标回收率SO42-90.0%~100.0%、NO3-93.0%~101.0%.样品预处理操作简单,方法灵敏度和准确性高,结果稳定性好,检出限低,能满足土壤环境样品检验的要求.     

离子色谱法测定PM_(2.5)中可溶性阴离子含量不确定度评议

准确测定大气颗粒物中水溶性组分对分析污染物来源及身体健康具有重要意义。本文采用离子色谱法测定PM2.5中水溶性阴离子(氯离子、硝酸根离子、硫酸根离子)含量,并对测定的不确定度进行分析。分析过程不确定度来源是样品重复性测量引入不确定度,样品测量准确性引入不确定度和标准曲线的不确定度。应用不确定度评定理论,分别计算氯离子、硝酸根离子和硫酸根离子的合成不确定度。结果表明,滤膜质量与取样环节是不确定度的主要来源。为了提高分析准确性,建议使用本底低的滤膜,取全样分析。     

热解-电位滴定(或酸碱滴定)快速测定萤石中氟化钙

萤石中氟化钙的测定,多是通过测定钙换算成样品中氟化钙含量。这些测定方法操作繁琐,准确度低。近年来有人试图用氟离子选择性电极测定氟矿中的氟含量,只是应用上的报导还不多。本文研究了热解-电位滴定及酸碱滴定测定萤石中氟化钙的适宜条件,并提出了简单快速、切实可行的分析方法。     

腐植酸作用下γ-六氯环己烷在冰相中的光转化

研究了腐植酸(HA)存在下冰相体系中γ-六氯环己烷(γ-HCH)的光转化规律.结果表明,HA浓度对γ-HCH的光转化率呈现低浓度促进而高浓度抑制的现象;盐离子浓度、NO_2~-及NO_3~-对γ-HCH的光转化率均有促进作用;低浓度Fe~(3+)对γ-HCH的光转化率有促进作用,当Fe~(3+)的浓度增大到50μmol/L时,呈现抑制效应;γ-HCH在不同p H值条件下光转化速率的大小顺序为碱性中性酸性.冰相中HA通过产生单线态氧(~1O_2)、羟基自由基(·OH)及三重激发态(HA*)加速γ-HCH的光转化.HA存在下γ-HCH的光转化产物主要是五氯环己烯、邻二氯苯和对二氯苯、一氯苯,光转化过程中~1O_2通过消耗中间产物间接加速了γ-HCH的光转化过程.     

Ion chromatographic determination of common ions at ultratrace levels in Antarctic snow and ice

The simultaneous determination of major impurities present in Antarctic snow and ice at ng g^? (ppb) concentrations by ion chromatography is described. Calibration data are presented for ammonium, sodium, potassium, chloride, nitrate and sulphate ions. Special attention is paid to the different ways of removing field contamination from ice and snow cores and suitable equipment is described. The results provide evidence against the validity of published sets of concentration data for nitrogen-containing compounds (NO^?₃ and NH⁺₄ in Antarctic snow, and demonstrate a crucial contamination problem in the determination of ammonium ions.     

青藏高原雪冰样品中低含量水溶金属离子分析方法对比研究

从采自青藏高原阿汝和古里雅冰川的两支冰芯中选取31个样品,分别用三种仪器对比分析K^+、Na^+、Ca^2+、Mg^2+四种水溶金属离子,寻求最佳分析方案。分析结果对比发现,电感耦合等离子体发射光谱(ICP-OES)法在K+测量中存在困难,而离子色谱(IC)法和电感耦合等离子体质谱(ICP-MS)法均能够满足要求,且分析结果具有高度的一致性,四种离子的相关系数(R2)均在0.97以上,且并未出现ICP-MS法比IC法测量值明显偏高的现象。因此,除IC法外,ICP-MS法也是检测青藏高原雪冰样品中水溶金属离子的有效手段,其测定速度更快,且可以同时进行微、痕量元素检测,适用于大批量冰芯样品的快速分析。     

Thirty years of snow deposition at Talos Dome (Northern Victoria Land, East Antarctica): Chemical profiles and climatic implications

The aim of this study was to use ion chromatographic methods to measure trace species under clean conditions in Antarctic snow samples. Both anionic and cationic contents of the snow samples were measured using preconcentration columns for both the ion chromatographic systems due to the low concentrations typical of Antarctic snow and ice samples. Samples were collected from a snow-pit dug in Talos Dome (East Antarctica) during the 2003-2004 Italian Antarctic Campaign to perform a preliminary survey of the site chosen for deep drilling in the framework of the TALos Dome ICE core (TALDICE) international project. Stratigraphic dating was attempted for the entire snow-pit, covering about 30 years, in order to achieve climatic information from the chemical profiles of the measured species. In particular, ions coming mainly from biogenic sources were investigated as potential markers for historical reconstruction of parameters expressing atmospheric and oceanic circulation, such as Southern Oscillation Index (SOI). For the studied period, a good correlation between biogenic species and SOI and sea-ice extent in the Ross Sea sector was observed, suggesting that these ions, as recorded in Talos Dome, can be used as markers for the reconstruction of the oceanic and atmospheric conditions in the past.     

四氢叶酸辅酶模型1, 2, 3-三取代咪唑啉盐的质谱裂解行为

讨论了１ ,２ ,３不对称取代咪唑啉盐各种离子的生成途径以及取代基对裂解方式的影响并分析了该类化合物的主要裂解方式。在所有实验中均有 ｍ／ｚ ＝ １２７（ Ｉ＋ ） 的离子峰和有机正离子 Ａ 峰存在,表明化合物１ 和２ 均为有机正离子和碘离子形成的盐。化合物１ 和２ 的质谱有相似的裂解方式：有机正离子发生失掉氮原子上的一个取代基而保留咪唑啉环产生 Ｄ, Ｅ, Ｆ 离子的裂解方式。更重要的是咪唑啉环有相同的裂解方式： Ｃ２ Ｎ３ 键和 Ｃ５ Ｎ１ 键同时断裂产生 Ｇ 离子碎片,以及 Ｃ２ Ｎ３ 键和 Ｃ４ Ｃ５ 键同时断裂产生 Ｈ 离子碎片。由于化合物１ 和２ 环上所连接的取代基不同而导致了其质谱裂解方式和程度的差异。化合物２ 的有机正离子 Ａ部分较稳定,质谱中表现为基峰,其 Ｅ, Ｆ 离子峰很弱;化合物１ 的有机正离子 Ａ 稳定性差,其相对丰度很小,其 Ｅ, Ｆ 离子峰较强。化合物１ｃ ,１ｄ ,１ｅ 的质谱中出现了比 Ａ 离子少三个单位的 Ｃ 离子峰,这是一种较特殊的裂解方式。     

Clean conditions for the determination of ultra-low levels of mercury in ice and snow samples

Laboratory facilities and methods are presented for the determination of ultra-low levels of mercury (Hg) in ice and snow samples originating from polar ice caps or temperate regions. Special emphasis will be given to the presentation of the clean laboratory and the cleaning procedures. The laboratory is pressurized with air filtered through high efficiency particle filters. This first filtration is not enough to get rid of contamination by Hg in air. Experiments are conducted in a clean bench, especially built for Hg analysis, equipped with both particle filter and activated charcoal filter. It allows to obtain very low levels of atmospheric Hg contamination. Ultrapure water is produced for cleaning all the plastic containers that will be used for ice and snow samples and also for the dilution of the standards. Hg content in laboratory water is about 0.08+/-0.02 pg/g. A Teflon system has been developed for the determination of Hg in ice and snow samples based on Hg(II) reduction to Hg(0) with a SnCl2/HNO3 solution followed by the measurement of gaseous Hg(0) with a Hg analyzer GARDIS 1A+ based on the Cold Vapor Atomic Absorption Spectroscopy method. Blank determination is discussed.     

Interaction between sulfonephthalein dyes and chitosan in aqueous solution and its application to the determination of surfactants.

A spectrophotometric method for the determination of ionic surfactants with Bromophenol Blue (BPB) based on incorporation into a precipitated chitosan was studied. Cationic surfactants (CS+), such as a quaternary ammonium ion containing a long-chain alkyl group, associate with BPB2- buffered at about pH 9 to form the ion associate (CS+)2 x BPB2-. CS+ associates with anionic surfactants (AS-). In the presence of a definite amount of CS+, an increase in the amount of AS- leads to a decrease in the amount of excess CS+, and therefore to a decrease in the amount of the ion associate of CS+ with BPB2-. The addition of a chitosan dissolved in acetic acid to a solution containing these ion associates leads immediately to precipitation of the chitosan and the incorporation of the ion associates (CS+)2 x BPB2- or CS+ x AS- into the precipitated chitosan. After centrifuging, ionic surfactants can be determined by the following two methods: (1) the absorbance of the supernatant solution is measured at 590 nm. (2) After the supernatant solution is separated, the precipitate is dissolved in an acetic acid solution and the absorbance is measured at 625 nm. Because the color of the precipitate is judged by the naked eye, this can be applied to the visual method. This is a simple and rapid method for the determination of a 10(-6) M order of ionic surfactants.     

Electronic sputtering produced by fission fragments on condensed CO and CO2

Condensed CO and CO2 are bombarded by approximately 65 MeV 252Cf fission fragments and the desorbed ions are analyzed by time-of-flight mass spectrometry as a function of target temperature, in the ranges 25-33 K and 75-91 K, respectively. Absolute desorption yields are measured up to complete ice sublimation. The mass spectra of both ice targets reveal the emission of: (1) low mass ions, produced by direct Coulomb interaction of the highly charged projectiles and delta-electrons with CO and CO2, and (2) pronounced series of cluster ions. The basic ice cluster structures (CO)n and (CO2)n are present in the emitted cluster series such as (CO)nCO+, (CO2)nCO2+, or (CO2)nCO3-. In the case of CO ice, however, the intense production of the series Cn+, Cn-, and (CO)mCn+ shows that Cn is the main cluster structure, consequence of a higher concentration of free carbon atoms in the nuclear track plasma of CO ice than in that of CO2 ice. Ion cluster abundance is observed to decrease exponentially with cluster mass. The decay constant is k(n) congruent with 0.13, about the same for series based on (CO)n and (CO2)n, but a factor 3.3 higher for the Cn series. The Cn clusters are formed by gas-phase condensation, but the (CO)n and (CO2)n clusters are produced by fracturing of the highly excited solid around the nuclear track. A dramatic reduction of the ion desorption yield is observed near T = 29 K for CO and near T = 85 K for CO2, when fast sublimation occurs and ice thickness vanishes. Close to sublimation temperature, the decay constant of the (CO)2Cn+ series increases due to a decreasing formation probability of large Cn clusters.     

Clean conditions for the determination of ultra-low levels of mercury in ice and snow samples

Laboratory facilities and methods are presented for the determination of ultra-low levels of mercury (Hg) in ice and snow samples originating from polar ice caps or temperate regions. Special emphasis will be given to the presentation of the clean laboratory and the cleaning procedures. The laboratory is pressurized with air filtered through high efficiency particle filters. This first filtration is not enough to get rid of contamination by Hg in air. Experiments are conducted in a clean bench, especially built for Hg analysis, equipped with both particle filter and activated charcoal filter. It allows to obtain very low levels of atmospheric Hg contamination. Ultrapure water is produced for cleaning all the plastic containers that will be used for ice and snow samples and also for the dilution of the standards. Hg content in laboratory water is about ¶0.08 ± 0.02 pg/g. A Teflon system has been developed for the determination of Hg in ice and snow samples based on Hg(II) reduction to Hg(0) with a SnCl₂/HNO₃ solution followed by the measurement of gaseous Hg(0) with a Hg analyzer GARDIS 1A+ based on the Cold Vapor Atomic Absorption Spectroscopy method. Blank determination is discussed.     

DX-300离子色谱测定山地冰川雪冰中的有机酸与无机酸阴离子

 利用AS4A SC分离柱 ,AG4A SC保护柱 ,ASRS Ⅱ抑制器 ,TAC 2阴离子富集柱和ATC 1阴离子捕集柱 ,以四硼酸钠 (Na2 B4O7)为淋洗液试剂 ,2 5mmol/LH2 SO4为化学抑制的再生液 ,采用梯度淋洗方式 ,对中国天山乌鲁木齐河源一号冰川雪冰中的生物有机酸和无机酸阴离子进行了测试分析。 2mL雪冰融水样品可在 16min内通过一次进样检测出氟离子、乙酸根离子、甲酸根离子、丙酮酸根离子、一氯乙酸根离子、氯离子、亚硝酸根离子、溴离子、硝酸根离子、磷酸根离子、硫酸根离子和草酸根离子共 10多种有机酸和无机酸阴离子。