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1.
石墨炉原子吸收法测定矿石中痕量铷和铯   总被引:1,自引:0,他引:1       下载免费PDF全文
铷、铯属碱金属元素,其电离电位很低(Cs 3.983 eV、Rb 4.676 eV),常用火焰原子吸收(或发射)法测定。该法只适用于测定常量铷、铯。对痕量铷、铯多用X—荧光光谱法或中子活化法测定,很少有人用石墨炉原子吸收法。Z.Grobenski等介绍了石墨炉原子吸收法测定铷、铯的方法。提  相似文献   

2.
石墨炉原子吸收法测定矿石中痕量铊   总被引:2,自引:0,他引:2  
胡吉顺 《岩矿测试》1986,(2):118-121
痕量铊的分析方法国内外有较多的报导,但利用萃取色层分离富集—石墨炉原子吸收法测定痕量铊的分析方法,尚未见过报导。萃取色层法是比较好的分离富集手段之一,我们曾进行过以磷酸三丁酯—聚三氟氯乙烯萃取色层分离富集—石墨炉原子吸收法测定痕量金的试验研究,在此基础上,又确立了测定痕量铊的新方法。  相似文献   

3.
郑民奇 《岩矿测试》1986,(4):282-284
地质样品中微量铊的分析,常采用有机试剂萃取分离后,进行比色法测定,其分析手续较繁、灵敏度低。近年来,随着原子吸收分析技术的发展,使用石墨炉原子吸收法测定痕量铊已有报导,也有用钒作为基体改进剂测定矿石中痕量镓、铟、铊。本文提出在盐酸-碘化钾-抗坏血酸介质中,用甲基异丁基甲酮(MJBK)萃取铊,不加基体改进剂,直接用自制的简易石墨炉平台测定有机相中的铊。  相似文献   

4.
采用石墨炉原子吸收光谱法测定土壤中的痕量铊。比较了两种不同的样品分解体系,建立了一种使用HNO_3+HF+H_2SO_4酸消解体系测量土壤中痕量铊的方法,同时探讨了石墨炉原子吸收光谱法测定铊的最佳仪器条件,并对基体改进剂浓度和体积、吸附解脱体系、吸附酸度以及震荡时间等条件进行了优化。该方法检出限为0.015×10-6,RSD为5.49%~13.42%,方法经国家一级标准物质验证,结果准确可靠。  相似文献   

5.
本试验确立的聚三氟氯乙烯—磷酸三丁酯(1:0.6)为固定相,反相萃取色层分离富集、石墨炉原子吸收法测定矿石中痕量金的分析方案,在选定的条件下,基本上无背景吸收和共存元素的影响。实测绝对灵敏度为8.9×10~(12)克/1%吸收;检出限为1.1×10~(-4)克/吨、定量测定下限为2.2×10~(-4)克/吨;  相似文献   

6.
本试验确立的聚三氟氯乙烯—磷酸三丁酯(1∶0.6)为固定相,反相萃取色层分离富集、石墨炉原子吸收法测定矿石中痕量金的分析方案,在选定的条件下,基本上无背景吸收和共存元素的影响。实测绝对灵敏度为8.9×10~(-12)克/1%吸收;检出限为1.1×10~(-4)克/吨、定量测定下限为2.2×10~(-4)克/吨;  相似文献   

7.
陈友Wei 《岩矿测试》1993,12(2):137-138
固体悬浮液超声波混匀器是为石墨炉原子吸收光谱法测定物料中痕量和超痕量无机成份而设计。均匀的悬浮液可手工进样,更适用于各种型号有自动进样装置的仪器。 1 悬浮液进样分析固体样品的优点 (1)悬浮液进样避免了使用强酸强碱分解过程中对人体和环境的毒害,减少了对待  相似文献   

8.
石墨炉原子吸收法测定化探样品中的痕量金   总被引:2,自引:0,他引:2  
试样经灼烧、王水(1 1)分解后,置于10%±的王水介质中经泡塑富集,高温灰化,小体积王水浸取后,以N i作为A u的稳定改进剂,用石墨炉原子吸收法测定A u。本方法检出限为0.18ng/mL,相对标准偏差为3.98%~6.12%。适用于地质、化探样品中痕量金的测定。  相似文献   

9.
研究报告410哌啶树脂在分离富集中的应用研究 I.岩矿中痕量金银铊镓铟的分离富集…………………………… ……………………………………………………………………………………李玉珍、饶竹、朱玉伦(1)雾化进样石墨炉原子吸收光谱法的研究I.直接雾化进样装置及其性能………………侯书恩、常诚(6)流动注射一光度法测定地质样品中痕量碘…………………………………………李锦听、邵一立、刘国均(11)流动注射在线萃取一火焰原子吸收光谱法测定地质试样中痕量银……汤志勇、金泽祥、陆琴、田凤英(14)微波诱导等离子体原子发射光谱法测定汞的研究…  相似文献   

10.
对石墨炉原子吸收光谱法测定地质样品中微量银进行了研究。样品经四酸溶解,在3mol/L的HCl介质中以EDTA-抗坏血酸溶液作为基体干扰改进剂,用石墨炉原子吸收光谱法测定地质样品中微量银。方法检出限为0.051ng/mL,精密度(RSD,N=11)5.91%~12.83%。能满足地质样品中w(Ag)/10-6=0.03~5范围内银测定的准确度和精密度的要求。  相似文献   

11.
Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.  相似文献   

12.
Robert L. Linnen   《Lithos》2005,80(1-4):267-280
The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H2O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H2O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.  相似文献   

13.
Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ1 roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003).  相似文献   

14.
HYDROGEOLOGY     
正20141756 Chen Ruige(Mathematical College,China University of Geosciences,Beijing100083,China);Zhou Xun Numerical Simulation of Groundwater Level Fluctuation in a Coastal Confined Aquifer with Sloping Initial Groundwater Level Induced by the Tide(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(7),2013,p.1099-1104,6 illus.,16 refs.) Key words:confined water,groundwater level  相似文献   

15.
正20141408 Cai Jia(Institute of Geology,Chinese Academy of Geological Sciences,Beijing100037,China);Liu Fulai Petrogenesis and Metamorphic P-T Conditions of Garnet-Spinel-Biotitebearing Paragneiss in Danangou Area,Daqingshan-Wulashan Metamorphic Complex Belt(Acta Petrologica Sinica,ISSN1000-0569,CN11-1922/P,29(7),  相似文献   

16.
17.
正20142386An Guoying(China Aero Geophysical Survey and Remote Sensing Center for Land and Resources,Beijing 100083,China)Application of Satellite Remote Sensing in Regional Hydrogeological Investigation:Taking Cenozoic Strata in Wenquan Sheet(1∶250 000)of Karakoram Range as an Example(Geosci-  相似文献   

18.
正20141016An Chengbang(Key Laboratory of Western China’s Environmental Systems,Ministry of Education,Lanzhou University,Lanzhou 730000,China);Zhao Yongtao Lake Records during the Last Glacial Maximum from Xinjiang,NW China and Their Climatic Impli-  相似文献   

19.
正20141538 Cao Qing(School of Earth Sciences and Engineering,Xi’an Petroleum University,Xi’an 710065,China);Zhao Jingzhou Characteristics and Significance of Fluid Inclusions from Majiagou Formation,Yichuan Huangling Area,Ordos Basin(Advances in Earth Science,ISSN1001-8166,CN62-1091/P,28(7),2013,p.819-828,7 illus.,3 tables,43 refs.)  相似文献   

20.
GEOCHEMISTRY     
正20142002 Wei Hualing(Institute of Geophysical and Geochemical Exploration,Chinese Academy of Geological Sciences,Langfang065000,China);Zhou Guohua Element Content and Mineral Compositions in Different Sizes of Soil in Tongling Area,Anhui Province(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(11),2013,p.1861  相似文献   

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