聚氧化乙烯絮凝-电感耦合等离子体原子发射光谱(ICP-AES)法测定土壤中水溶性钾、钠、钙、镁、硫酸根

建立了聚氧化乙烯絮凝-4000 r/min离心,电感耦合等离子体原子发射光谱(ICP-AES)法测定土壤水溶性钠、钾、钙、镁、硫酸根离子的方法.在常规方法浸提的基础上,加入聚氧化乙烯絮凝剂使溶液中的胶体形成絮凝物聚沉,制得澄清溶液,消除了胶体对钾、钠、钙、镁吸附的干扰;采用电感耦合等离子体原子发射光谱法测定钾、钠、钙、...     

电感耦合等离子体原子发射光谱法测定植物中钾、钠、钙和镁

采用硝酸–高氯酸湿法消解或硝酸–双氧水微波消解植物样品,以电感耦合等离子体原子发射光谱法同时测定样品溶液中钾、钠、钙和镁含量。用该法测定灌木枝叶和茶叶标准样品,测定值均在标准值范围内,测定结果的相对标准偏差为0.45%~4.05%(n=8)。钾、钠、钙、镁的加标回收率分别为94.4%~107.6%,92.6%~107.9%,93.7%~105.4%,92.9%~107.2%。该方法操作简便,测量精密度和准确度完全满足植物中钾、钠、钙和镁含量的测定要求。     

微波消解-电感耦合等离子体发射光谱法测定固体生物质燃料中8种元素

建立电感耦合等离子体发射光谱法同时测定固体生物质燃料中钾、钠、钙、镁、砷、铜、铁、锰8种元素的含量。样品采用5 mL硝酸溶液和2 mL过氧化氢溶液进行微波消解,在选定的仪器工作条件下进行测定。钠、钙、镁、砷、铜、铁、锰的质量浓度在0～5.0 mg/L,钾的质量浓度在0～50.0 mg/L范围内与光谱强度具有良好的线性关系,相关系数均大于0.999,方法检出限为0.002～0.022 mg/L。样品的加标回收率为91.9%～108.2%,测定结果的相对标准偏差为2.1%～6.8%(n=6)。该方法简便、快速、高效且准确,适用于固体生物质燃料中钾、钠、钙、镁、砷、铜、铁、锰的测定。     

电感耦合等离子体原子发射光谱法同时测定高强度玻璃纤维粉体中9种金属元素

建立电感耦合等离子体原子发射光谱法测定高强度玻璃纤维粉体中铝、镁、钙、铁、钛、锂、铈、钠、钾9种金属元素含量的方法。采用氢氟酸、高氯酸和盐酸分两段溶解样品,分别在选定的各元素分析谱线下,采用电感耦合等离子体原子发射光谱仪测定各元素含量。9种金属元素在各自的质量浓度范围内与光谱强度成良好的线性关系,相关系数均大于0.999,检出限为8.0~17.4 μg/g。测定结果的相对标准偏差小于1.8%(n=6),加标回收率为97.6%~103.7%。该方法准确,简便,快速,适用于高强度玻璃纤维中多金属元素的同时测定。     

电感耦合等离子体原子发射光谱法测定地热水中钾、钠、钙、镁的含量

地热水样品经0.45μm水系微孔滤膜过滤,弃去初始的50~100 mL滤液,收集500mL地热水样品,然后加入适量50%(体积分数)硝酸溶液,使pH不大于2,采用电感耦合等离子体原子发射光谱法测定其中钾、钠、钙、镁的含量。选择钾、钠、钙、镁的分析谱线依次为766.490,589.592,317.933,285.213nm。采用背景扣除及样品稀释的方法校正背景和减小基体效应。4种元素的质量浓度在一定范围内与其对应的发射强度呈线性关系,方法的检出限为0.000 6~0.010 0mg·L~(-1)。对钾、钠、钙和镁的质量浓度分别为5,100,100,50mg·L~(-1)的混合标准溶液进行测定,钾、钠、钙和镁测定值的相对标准偏差(n=10)依次为0.43%,1.3%,0.43%,0.54%。方法应用于标准物质的分析,测定值与认定值相符。用标准加入法做方法的回收试验,测得回收率为99.6%~102%。实验室开展的比对试验结果表明:此法与传统方法测定结果基本吻合。     

电感耦合等离子体原子发射光谱法测定地热水中钾、钠、钙、镁的含量北大核心CSCD

地热水样品经0.45μm水系微孔滤膜过滤,弃去初始的50~100 mL滤液,收集500mL地热水样品,然后加入适量50%(体积分数)硝酸溶液,使pH不大于2,采用电感耦合等离子体原子发射光谱法测定其中钾、钠、钙、镁的含量。选择钾、钠、钙、镁的分析谱线依次为766.490,589.592,317.933,285.213nm。采用背景扣除及样品稀释的方法校正背景和减小基体效应。4种元素的质量浓度在一定范围内与其对应的发射强度呈线性关系,方法的检出限为0.000 6~0.010 0mg·L^(-1)。对钾、钠、钙和镁的质量浓度分别为5,100,100,50mg·L^(-1)的混合标准溶液进行测定,钾、钠、钙和镁测定值的相对标准偏差(n=10)依次为0.43%,1.3%,0.43%,0.54%。方法应用于标准物质的分析,测定值与认定值相符。用标准加入法做方法的回收试验,测得回收率为99.6%~102%。实验室开展的比对试验结果表明:此法与传统方法测定结果基本吻合。     

电感耦合等离子体原子发射光谱法(ICP-OES)测定地下水中多种元素

应用电感耦合等离子体原子发射光谱法(ICP-OES)测定地下水中钾、钠、钙、镁、铁、锰元素的含量,使用分光光度法测定氟的含量,测定的相对标准偏差为0.7%~2.8%,加标回收率为92.1%~105.2%。结果表明,大部分地区地下水中钠和氟化物的含量均偏高,常量与微量元素的组成含量差别不大。     

电感耦合等离子体原子发射光谱法(ICP-AES)测定地下水中多种元素

应用电感耦合等离子体原子发射光谱法(ICP-AES)测定地下水中钾、钠、钙、镁、铁、锰元素的含量,使用分光光度法测定氟的含量,测定的相对标准偏差为0.7%~2.8%,加标回收率为92.1%~105.2%。结果表明,大部分地区地下水中钠和氟化物的含量均偏高,常量与微量元素的组成含量差别不大。     

钙锶镁同时测定方法的研究进展

对应用于钙、锶和镁同时测定的分析方法如原子吸收光谱法、电感耦合等离子体原子发射光谱法、电感耦合等离子体质谱法、离子色谱法、X-射线荧光光谱法等的现状(主要在1997—2009年间发表的文献)及相关的原理、方法的特点及不足之处作了综述(引用文献63篇)。     

电感耦合等离子体发射光谱法同时测定奶粉中钙铜铁钾镁锰钠锌和磷

通过优化试验确定仪器的最佳工作参数,微波加热硝酸消解样品,采用电感耦合等离子体发射光谱法同时测定奶粉中钙、铜、铁、钾、镁、锰、钠、锌和磷9种元素的含量。分析了4种奶粉样品,所得结果与国标方法的结果一致。方法回收率在96.5%-111%之间。     

电感耦合等离子体原子发射光谱(ICP-AES)法测定铸造用硅砂中的Fe2O3、Al2O3、CaO、MgO、TiO2、K2O、Na2O

建立了电感耦合等离子体原子发射光谱(ICP-AES)法测定铸造用硅砂中Fe_2O_3、Al_2O_3、CaO、MgO、TiO_2、K_2O、Na_2O的方法。研究了溶样方法的选择优化,采用硝酸、氢氟酸溶样,冒高氯酸处理,通过元素分析线的选择,基体和共存元素影响的消除,在最佳的仪器分析条件下得出了方法的线性范围、相关系数及检出限。用硅砂3个梯度含量的标准物质的分析结果评价方法的准确度和精密度。方法的检出限Fe为0.012μg/mL、Al为0.032μg/mL、Ca为0.27μg/mL、Mg为0.003 2μg/mL、Ti为0.002 1μg/mL、K为0.16μg/mL,Na为0.000 44μg/mL。5次数据的相对标准偏差说明方法稳定性较好。方法适用于铸造用硅砂中Fe_2O_3、Al_2O_3、CaO、MgO、TiO_2、K_2O、Na_2O含量的测定。     

水和氯化铵提取-电感耦合等离子体发射光谱(ICP-AES)法测定石灰性土壤中交换性钾钠钙镁

为了提高石灰性土壤中交换性钾钠钙镁的分析效率及分析准确度,本文创新性采用水和氯化铵对石灰性土壤进行处理,并采用振荡交换、离心分离的方式进行石灰盐清洗、钾钠钙镁离子交换提取,提取液直接在电感耦合等离子体发射光谱仪(ICP-AES)上测定。该方法交换性盐基钙、镁、钾、钠的检出限分别为0.01、0.009、0.004、0.012cmol/kg。用国家一级标准物质GBW07498-新疆棕漠土和新疆地区石灰性土壤进行验证,方法精密度均小于5%,回收率在97％~105%。方法适用于石灰性（碱性）土壤（特别是新疆土壤）样品中交换性钾、钠、钙、镁的分析测定。     

Determination of Copper,Cadmium, Zinc And Lead In ArgeŞ River In Romania During Four Seasons By Inductively Coupled Plasma Atomic Emission Spectrometry And Anodic Stripping Voltammetry

ABSTRACT

The paper represents a continued study of selected heavy metals concentration in the Arge? River, the fifth river in length from Romania.

For the determination of metal ion concentration in Arge? river was used Atomic Absorption Spectrometry for sodium, potassium and magnesium; Direct Coupled Plasma Atomic Emission Spectrometry for calcium; Inductively Coupled Plasma Atomic Emission Spectrometry for copper, cadmium, zinc, aluminium, lead, titanium, zirconium, chromium, molybdenum, manganese, iron and nickel.

Copper, cadmium, zinc and lead concentration were determined by ICP–AES and ASV and results were reliable.

By comparison of the results a good agreement between these two techniques is observed.     

Analysis of ions in polar ice core samples by use of large injection volumes in ion chromatography

In the present study a non-suppressed ion chromatography system with conductivity detection was tested in terms of sampling effects, the effects on the ion separation efficiency and analysis detection limits to find optimum conditions for the determination of chloride, nitrate, sulfate, sodium, ammonium, potassium, calcium and magnesium ions in polar ice core samples.     

Atomic-absorption spectrometric determination of calcium, magnesium and potassium in leaf samples after decomposition with molten sodium hydroxide

The decomposition of standard leaf samples of varied origin and nature by fusion with sodium hydroxide in an open system has been studied. The use of sodium nitrate as an auxiliary agent facilitated the mineralization of most of the samples. The solutions obtained were analysed for calcium, magnesium and potassium by flame atomic-absorption spectrometry. The method is fast and quite precise, with absolute standard deviations of 0.04-0.13, 0.002-0.03 and 0.04-0.12% for calcium, magnesium and potassium contents of O.8-5.0, 0.13-0.48 and 0.36-2.2% respectively. The limits of detection (mug/ml) in the determination step were 0.10 for calcium, 0.011 for magnesium, and 0.09 for potassium.     

Natural radioactivity in building materials utilized in the State of Kuwait

A simple radiochemical procedure is described for the determination of⁹⁰Sr in brines, which are very highly concentrated in sodium, calcium, potassium, magnesium, chloride and sulfate ions. The method is based on the different solubility of yttrium as compared to that of strontium, calcium and magnesium in ammonium chloride solutions, and utilizes Eichroms resin TRU·Spec for the purification of the yttrium fraction. The overall time required for the⁹⁰Sr analysis (excluding the counting time) is less than one day. Because the procedure involves only rather simple steps, it is well suited for routine analyses of large sample numbers.     

涡旋提取-电感耦合等离子体发射光谱(ICP-OES)法测定酸性和中性土壤中交换性盐基总量

传统的土壤交换性盐基总量检测方法前处理过程复杂,检测时间长,建立涡旋提取-电感耦合等离子体发射光谱(ICP-OES)法,大大提高了检测效率。采用涡旋提取中性和酸性土壤中交换性盐基总量,结合电感耦合等离子发射光谱仪（ICP-OES）同时测定土壤提取液中交换性盐基总量钙镁钠钾含量。通过考察土液比,涡旋时间,涡旋转速以及方法的精密度和准确度。结果表明,最佳涡旋条件为土液比为1:50,涡旋时间为20 min,涡旋速度为1500 r/min。利用ICP-OES测定国家标准物质RMH-A275、RMH-A274和GBW07458a（ ASA-7a）土壤提取液中交换性盐基总量钙镁钠钾含量,各元素测定结果均在标准值范围内,相对标准偏差均小于2 %,交换性钙镁钠钾的方法检出限分别为0.048 cmol/kg、0.035 cmol/kg、0.038cmol/kg和0.072 cmol/kg。应用该方法检测20份耕地实际土壤样品,与国标法相比,交换性盐基总量钙镁钠钾的测定值相对误差均小于2 %,满足土壤样品分析检测的要求。该方法操作简便、试剂用量少,准确度和精密度好,适用于大批量生态地球化学评价土壤样品中交换性盐基总量钙镁钾钠的测定。     

Determination of magnesium and calcium ions in seawater by capillary zone electrophoresis

Capillary zone electrophoresis is proposed for the determination of magnesium and calcium ions in seawater. A carrier solution containing EDTA was adopted for the complexation of these ions and the effect of sodium chloride concentration in the sample solutions on the results was examined. It was found that magnesium and calcium ions could be determined without any pretreatment by injecting 100-fold diluted seawater samples. Linear calibration graphs were obtained for standard solutions containing up to 10.0 mg/l of calcium ion when both peak area and peak height were used. On the other hand, a linear calibration graph was obtained for standard solutions containing up to 20.0 mg/l of magnesium ion when the peak area was used, while a curved one was obtained when the peak height was used. Relative standard deviations were 0.8 and 1.2% when a standard solution containing 5.0 mg/l of magnesium and 8.0 mg/l of calcium ions was analysed 8 times using the peak area. Limits of detection for magnesium and calcium ions were 0.13 and 0.26 mg/l, respectively. The proposed method was applied to the determination of magnesium and calcium ions in surface and bottom seawater samples.