基体改进剂对石墨炉原子吸收法测定钡的影响

根据EPA方法7081、ISO方法208.2测定钡的原理,添加基体改进剂,确定<基体改进剂石墨炉原子吸收法测定钡>方法灵敏度及测试条件.方法用于测量水中微量钡,结果令人满意.     

石墨炉原子吸收分光光度法测定饮用水中钡的实验研究

文章通过实验研究优化了一种石墨管原子吸收法测定饮用水中钡的方法。分别采用普通石墨管和ELC石墨管,通过优化灰化温度和原子化温度以及实际样品检测验证了方法的可行性。结果表明,采用普通石墨管检出限为4.69μg/L,相对标准偏差为9.5%,实际样品加标回收率为92%~100%;采用ELC石墨管检出限为1.90μg/L,相对标准偏差为8.7%,实际样品加标回收率为98%~101%,两种方法均可满足实验室饮用水中钡的测定要求。     

巯基棉富集分离水中痕量铅,镉,铜——火焰原子吸收测定法的研究

水中痕量铅、镉、铜的测定一般需采用石墨炉原子吸收法,此法对仪器要求高,耗费大,精密度、准确度相对较差.本文对巯基棉富集后用火焰原子吸收测定上述元素的方法进行了研究,并与蒸发浓缩和石墨炉原子吸收法作了对比.结果证明巯基棉富集——火焰原子吸收法测定水中微量铅、镉、铜能获得满意的结果.     

水中微量偏二甲基肼检测方法的研究和应用

偏二甲基肌是川作火箭推进剂燃料，有较大的毒性，也是环境污染物。它的水中最大允许浓度为０．０６ｍｇ／Ｌ。本研究建立了一种水中微量偏二甲基肼的检测方法，采用钼酸铵作为试剂的比色测定法，方法简便、准确、灵敏度高，可川于现场检测。本文还报道了应用本法测定了水中微量肼和甲基肼的稳定性的结果。     

《干旱环境监测》2006年第20卷总目次

监测方法研究4,5-二甲基-2-噻唑偶氮重氮氨基偶氮苯固相萃取光度法测定环境样品中锌的研究………………………………………………………………微波萃取—高效液相色谱(HPLC)法测定土壤中16种多环芳烃的研………………究杨杰(1 5)石墨炉原子吸收光谱法测定水中微量…………………钡梁延鹏刘辉利朱义年卢洁(2 65)微波消解ICP—AES法测定土壤及底泥等中常量及微量元素陈素兰胡冠九陈波王霞(2 69)……………………………………………………………………………………………………分光光度法测定环境水样中铂的研究谢琦莹王宇韦群艳杨项军黄章…     

高效液相色谱荧光检测湖泊沉积物间隙水中的微量硫醇

提出了测定天然水中微量低分子质量硫醇的灵敏、可靠方法,即采用7-氟苯并-2-氧-1,3-二唑-4-磺酸铵盐(SBDF)柱前衍生化、逆相高效液相色谱分离和荧光检测技术。文中详细研究了一些洗脱条件,如流动相的组成、pH值和洗脱模式对色谱保留行为的影响,从而获得了最佳的洗脱条件。对于被研究的5种低分子质量硫醇,获得了其浓度在25~250nmol/L范围内的标准曲线和测定限。本方法成功地测定了湖泊沉积物间隙水中的微量硫醇。     

氢化物发生-原子荧光法同时测定水中的砷和铅的研究

目的是建立一种同时测定水中微量砷和铅的方法。方法采用酸消解法消解水样,氢化物发生-原子荧光法同时测定水中微量砷和铅。结果显示,砷和铅方法的检出限分别为0.20μg/L和0.24μg/L,回收率分别为92.9%~104.4%和93.5%~103.8%,相对标准偏差分别为2.3%和3.5%。水中微量砷和铅用氢化物发生-原子荧光法测定能满足要求,可以同时测定。     

新分光光度法测定水中微量亚硝酸根

本文提出用对氨基苯甲酸和8—羟基喹啉作为重氮化和偶联试剂,光度法测定水中微量亚硝酸根。试验了影响测定结果的因素,确定了测定亚硝酸根的最佳条件。该方法可以测定浓度在0.01—2.5μg/ml的NO_2~-,测定结果变异系数不超过2.0％。     

火焰原子吸收分光光度法测定水中微量钙

水中微量钙虽有许多测定方法(如原子吸收法、电感耦合等离子体发射光谱分析法、离子电泳法、离子电极法和离子色谱法等直接定量法),但这些方法都易受共存离子的影响.此外,当采用这些方法测定微量钙时,需浓缩或溶剂萃取等,操作烦琐.现已研究出采用火焰原子吸收分光光度计(F-AAS)测定水中微量钙的方法.     

消除水中硫酸盐测定干扰的方法

铬酸钡间接原子吸收法测定水中硫酸盐时,样品的稀释倍数、盐度、酸度对测定结果影响较大.通过试验得出消除干扰的方法,使得测定结果准确、可信.     

石墨炉原子吸收光谱法测定海河下游水中痕量镉

原子吸收光谱法直接测定高盐水中痕量镉时，有很大背景吸收和误差。本文采用络合—萃取技术使共存元素与待测元素分离，既消除了基体干扰，又达到了富集作用，使测定结果准确可靠。     

无火焰原子吸收石墨炉法测定海水中的总铬

研究了使用无火焰原子吸收石墨炉法测定海水中总铬的分析方法。在氧化过程后采用络合 -萃取技术使共存元素与待测元素分离 ,既消除了基体干扰 ,又达到了富集作用 ,使测定结果准确可靠。方法的相对标准偏差 6.34 % ,回收率85.2 %。     

原子吸收光度法测定镉时铁的基体改进效应研究

用石墨炉原子吸收分光光度法测定环境废水中的痕量镉时,Mn、Cr、Ni、Cu、Co、Zn等共存元素干扰严重。用100mg／L的铁作为基体改进剂可消除上述共存元素的干扰,测定结果令人满意。     

无火焰原子吸收法测定水中的银

以硝酸做介质,用石墨炉原子吸收光度法可测定自来水及环境污水中的微量银,钙,镁,铁等对银的测定有轻微干扰,其它共存元素不干扰测定,结果令人满意。     

石墨炉原子吸收光谱法测定土壤中银

建立了土壤样品中痕量银的石墨炉原子吸收光谱测定方法,优化了试验条件,标准曲线线性关系良好,当取样质量为0.25 g,定容体积为25 mL时,方法检出限为0.01 mg/kg.经标准样品验证,方法准确度符合土壤样品分析要求.     

两种原子吸收法测定环境水样中镍的比较

用加热浓缩-火焰原子吸收光谱法和石墨炉-原子吸收光谱法对环境水样中的镍进行了比较测定,结果表明,两种方法测定镍的各项指标均在要求范围,两种方法测定结果的相对误差均＜7.1%,表明两种方法可以视为等效方法,作用可以相互替补使用.     

石墨炉原子吸收法在环境样品测定中的应用

评述了石墨炉原子吸收光谱法在环境样品测定中的应用 ,内容包括装置与技术、水与废水、土壤与底质 ,以及大气与废气     

Determination of trace metals in drinking water in Irbid City-Northern Jordan

Drinking water samples from Irbid, the second populated city in Jordan were analyzed for trace metals (As, Ba, Cd, Pb, Cr, Cu, Fe, Zn, Mn, Ni, and Se) content. The study was undertaken to determine if the metal concentrations were within the national and international guidelines. A total of 90 drinking water samples were collected from Al-Yarmouk University area. The samples were collected from three different water types: tap water (TW), home-purified water (HPW), and plant-purified water (PPW). All the samples were analyzed for trace metals using an inductively coupled plasma-optical emission spectrometry. All the samples analyzed were within the United States Environmental Protection Agency admissible pH limit (6.5–8.5). The results showed that concentrations of the trace metals vary significantly between the three drinking water types. The results showed that HPW samples have the lowest level of trace metals and the concentrations of some essential trace metals in these samples are less than the recommended amounts. Slight differences in the metal contents were found between HPW samples, little differences between PPW samples; however, significant differences were found between TW samples. Although some TW samples showed high levels of trace metals, however, the mean level of most elements determined in the samples were well within the Jordanian standards as well as the World Health Organization standards for drinking water.     

火焰、石墨炉原子吸收法测定地表水中铜和镉

对浓缩火焰原子吸收法和石墨炉原子吸收法测定地表水中痕量铜和镉的结果作了比较。试验结果表明，两种方法测定结果间无明显差异，加标回收率为88．7％～103％，可互相替代，等效使用。     

Trace element concentration in groundwater of Pesarlanka Island, Krishna Delta, India

There is a growing concern over the potential accumulation of trace element concentration in groundwater of coastal aquifer owing seawater encroachment in the last several decades. A total of 29 groundwater samples collected from Pesarlanka Island, Krishna delta, Andhra Pradesh, India were analyzed for 13 trace elements (B, V, Mn, Fe, Ni, Co, Cu, Zn, As, Sr, Cd, Ba, and Pb) using inductively coupled plasma mass spectrometry. The results reveal that B, Fe, Ni, As, Sr, and Pb vary from 11.22 to 710.2, 1.25 to 684.6, 0.02 to 37.33, 27.8 to 282.3, 164.1 to 7,009, and 1.97 to 164.4 μg/l, respectively. Ba, Cd, Co, Cu, Ni, V, and Zn are almost within permissible limits for drinking water, but As, Fe, Mn, Pb, B, and Sr are above the permissible limit. The toxic element Pb is 1.64 times more than the maximum permissible limits of drinking water. The minimum value of As is also 2.78 times more, whereas the maximum is 28.2 times the permissible limit. The spatial distributions of alkaline earths (Sr, Ba), transition metals (V, Co, Ni, Fe), metallic elements (Cu, Pb), and (As) were found in considerable variation in the entire Island. Good cross-correlations were found between As, B, Co, and Sr with total dissolved solids and among other trace elements such as B, As, Co, and Sr. The variability observed within the groundwater samples is closely connected to the sea spray input; hence, it is primarily a consequence of geographical and meteorological factors, such as distance from the ocean and time of year. The trace element levels, in particular those of heavy metals, are very low, suggesting an origin from natural sources rather than from anthropogenic contamination. A few trace elements (Sr and B) are found as sensitive parameters responding to changes in fresh to saline groundwater environment. The highly elevated trace elements in this area which may be attributed to marine sediments or death and decay of plants are presented in this paper.