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1.
本文简述了等离子体质谱法测定二氧化铀和八氧化三铀粉末中的硼、钛、钒、钼、铬、锌、镉等7个痕量元素的方法。本方法采用TBP萃取色层分离铀基体后,用高分辨等离子体质谱仪(ICP-MS)测定多个痕量元素,测定下限达1×10-9g/g,测定的相对标准偏差小于15%。核工业14个实验室比对试验结果表明,本方法结果准确可靠  相似文献   

2.
全反射X射线荧光光谱法同时测定天然水中多种元素   总被引:4,自引:0,他引:4  
李国会  张天估 《岩矿测试》1998,17(2):123-126
利用自行研制的有3个反射体的全反射X射线荧光分析仪,以Se作内标,同时测定天然水中的痕量Ni、Cu、Zn、Pb、Rb和Sr。对纳克级元素,方法的检出限为10-10~10-11g,水样分析结果与无火焰原子吸收法和ICPMS法相符,精密度好,对纳克级痕量元素测定的RSD(n=5)小于72%。  相似文献   

3.
朱金荣  宫明岗 《岩矿测试》1995,14(3):180-184
建立了采用电感耦合等离子体发射光谱测定锂辉矿中的主、次、痕元素的方法。样品经酸溶和碱熔处理后,直接进行了20种元素的测定。其检出限在0.5-14.6μg/g。样品测定的RSDn=11),其主量成分<0.5%,痕量成分<10%。标准加入回收率为87.2%-114.3%。  相似文献   

4.
尹明  符廷发 《岩矿测试》1993,12(4):246-250
文章报道了用感耦等离子体质谱法测定高纯氧化钪中15个痕量稀土杂质的研究,考察了测定中的各种干扰和影响因素,选择Cs为内标元素补颈体抑制效应和灵敏度漂移。各稀土元素的检出限在0.005-0.027ng/ml范围,标准加入回收率为94.5%-103.7%,精密度为0.85%-1.95%,称取10mg样品,酸溶解后可直接测定高纯氧化钪中总量低于2μg/g的15个稀土杂质。  相似文献   

5.
李冰 《岩矿测试》1994,13(1):20-24
研究了用感耦等离子体发射光谱(ICP-AES)测定纯氧化镧中Ce,Pr,Nd,Sm,Y,Fe,Al,Ca,Mg和Si10个杂质元素的方法。考察了基体镧的光谱干扰,共存元素间光谱干扰及校正方法,方法检出限为0.0005-0.039μg/ml;标准加入量1μg/ml时,回收率为95%-106%;10μg/ml的标准溶液,测定10次,RSD为0.24%-1.01%。方法简单,快速,不震分离富集,适用于氧  相似文献   

6.
曾惠芳  周绍箕 《岩矿测试》1994,13(4):259-263
研究了三烷基氧膦纤维素色层分离富集痕量元素W、Mo和Sn的条件,根据吸附与洗脱实验中的现象初步探讨了TRPO与W、Mo,Sn的反应机理。以Rh为内标采用感耦等离子体质谱法进行测定,标准加入回收率为98%-101%;W、Mo,Sn的测定下限分别为0.02、0.01、0.1μg/g;重复取样测定的RSD均小于10%。经对地球化学标准物质分析,结果与推荐值相符。  相似文献   

7.
电感耦合等离子体质谱法测定含气天然矿泉水中的铬   总被引:4,自引:3,他引:1  
张保科  王蕾  马生凤 《岩矿测试》2013,32(4):568-571
含气天然矿泉水含有高浓度的HCO;和CO2,其中元素Cr的浓度在电感耦合等离子体光谱(ICP-AES)的检出限附近甚至更低,应用电感耦合等离子体质谱(ICP-MS)测定又容易形成多原子离子40 Ar12C,对52 Cr的测定形成干扰,致使ICP-MS不能直接准确测定含气天然矿泉水中的Cr元素.本文对水样进行前处理,加热煮沸2 min后放置至室温,加入硝酸调节水样酸度为5%,促进HCO3-与H+反应生成大量的CO2迅速释放出来,消除了40Ar12C对52Cr产生的质谱干扰,实现了ICP-MS能够直接准确分析Cr的含量,方法检出限为0.23 ng/mL,加标回收率为92.3%~93.7%,相对标准偏差(RSD)小于10%.此方法简单实用,精确度和准确度能够满足天然矿泉水分析测试的要求,还可同时测定此批前处理水样中的锌铜砷镉铅等痕量元素.  相似文献   

8.
光度法测定痕量钛的研究   总被引:6,自引:1,他引:6  
周之荣 《岩矿测试》1997,16(4):303-306
基于痕量Ti(Ⅳ)在稀H2SO4介质中对EDTA还原Cr2O2-7褪色反应的抑制作用,建立了测定痕量Ti(Ⅳ)的光度法。测定范围为24~24μg/L,检出限为106×10-7g/LTi(Ⅳ)。结合萃取分离富集技术,方法用于测定人发及茶叶样品中的痕量Ti(Ⅳ),结果与标准值相符,加标回收率在95%~100%,RSD(n=6)为11%~20%。  相似文献   

9.
刘颖  李献华 《岩矿测试》1998,17(2):112-116
用等离子体质谱(ICP-MS)对美国玄武岩标准物质BHVO-1、W-2和中国玄武岩标准物质GBW07105(GSR-3)进行了39种痕量元素分析。三个标准物质的大多数元素测定值与标准值在误差范围内一致。GSR-3中Cs、Pb、Y、Nb、Tm、Yb等元素的ICP-MS测定值与标准值存在不同程度的偏差。用同位素稀释法对GSR-3中的Pb做了进一步的精确测定,结合玄武岩的元素地球化学分析,认为GSR-3  相似文献   

10.
双指示催化光度法测定天然水中痕量锰   总被引:1,自引:0,他引:1  
阎永胜  洪军 《地质实验室》1996,12(4):214-216
研究表面活性剂在下双指示动力学法测定痕量锰的新方法,考察了测定条件。方法灵敏度较高,ε=7.8×10^7L.mol^-1cm^-1.RSD=2.7%。已用于天然水中痕量锰的测定。  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.
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.  相似文献   

13.
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   

14.
Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by Paradunbarula (Shindella) shindensis, Hemigordiopsis cf. luquensis and Colaniella aff. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions. To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.  相似文献   

15.
PALEONTOLOGY     
正20141596 Liu Yunhuan(School of Earth Sciences and Resources,Chang’an University,Xi’an 710054,China);Shao Tiequan Early Cambrian Quadrapyrgites Fossils of Xixiang Boita in Southern Shaanxi Province(Journal of Earth Sciences and Environment,ISSN1672-6561,CN61-1423/P,35(3),2013,p.39-43,3 illus.,20 refs.)  相似文献   

16.
正20141719 Chen Zhijun(State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China);Chen Jianguo Automated Batch Mapping Solution for Serial Maps:A Case Study of Exploration Geochemistry Maps(Journal of Geology,ISSN1674-3636,CN32-1796/P,37(3),2013,p.456-464,2 illus.,2 tables,10 refs.)  相似文献   

17.
正20140962 Chen Fenning(Xi’an Institute of Geology and Mineral Resources,Xi’an710054,China);Chen Ruiming Late Miocene-Early Pleistocene Ostracoda Fauna of Gyirong Basin,Southern Tibet(Acta Geologica Sinica,ISSN0001-5717,CN11-1951/P,87(6),2013,p.872-886,6illus.,56refs.)  相似文献   

18.
PETROLOGY     
正1.IGNEOUS PETROLOGY20142008Cai Jinhui(Wuhan Center,China Geological Survey,Wuhan 430205,China);Liu Wei Zircon U-Pb Geochronology and Mineralization Significance of Granodiorites from Fuzichong Pb-Zn Deposit,Guangxi,South China(Geology and Mineral Resources of South China,ISSN1007-3701,CN42-1417/P,29(4),2013,p.271-281,7illus.,  相似文献   

19.
正20141205Cheng Weiming(State Key Laboratory of Resources and Environmental Information System,Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing 100101,China);Xia Yao Regional Hazard Assessment of Disaster Environment for Debris Flows:Taking Jundu Mountain,Beijing as an  相似文献   

20.
正20141266Fan Chaoyan(Guangdong Provincial Key Laboratory of Mineral Resources and Geological Processes,Guangzhou 510275,China);Wang Zhenghai On Error Analysis and Correction Method of Measured Strata Section with Wire Projection Method(Journal of  相似文献   

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