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1.
研究了表面活性剂在Se和Te诱导反应中的作用,对反应机理进行了初步探讨.实验表明,在选定条件下,加入适量非离子表面活性剂Tween-80,使Te的诱导反应速度加快,灵敏度提高1倍,并利用其对Se有抑制反应速度的作用,使Te对Se的抗干扰能力增强.阴离子表面活性剂十二烷基苯磺酸钠对Se和Te均有加速反应的作用,Se的灵敏度提高1.3倍;Te的灵敏度提高40%.基于此,所建立的方法可用于地质样品中纳克级Se和Te的测定.测定Te的线性范围0.01~0.4 μg/L,相对标准偏差(n=5) 5.6%;测定Se的线性范围0.1~2 μg/L,相对标准偏差(n=5)7.5%.经4种地质标样分析验证,结果与标准值相符.  相似文献   

2.
水解—火焰原子吸收法测定地质样品中高含量铂   总被引:1,自引:0,他引:1  
龙小玲  苏晓 《矿物岩石》1991,11(1):111-113
本文研究了在空气-乙炔火焰中于pH6—8的水相介质直接进行贵金属铂(1V)的测定方法。测定的灵敏度0.5μg/ml 1%;2.5μg/ml,RSD(n=4)1.26%。在部分铜镍矿和黄铁矿地质样品中进行人工模拟试验,表明该法是可行的,可以测定同类地质样品中0.000 x%以上的铂。  相似文献   

3.
氢化物发生-原子荧光光谱法测定地球化学样品中痕量铋   总被引:4,自引:0,他引:4  
样品经王水溶解后,加入KMnO4溶液氧化,草酸除去过量KMnO4后的体系,直接用氢化物发生原子荧光光谱法测定地质样品中痕量Bi。方法使Au、Pd、As、Sb、Se、Te等元素的允许量大为提高,减少了不同测定体系中共存元素对Bi测定的干扰。方法的检出限(6s)为0.042μg/g,精密度(RSD,n=12)为1.88%~5.57%。经国家一级地质标准物质验证,测定值与标准值吻合。  相似文献   

4.
氢化物-原子荧光法测定铜矿中微量硒和碲   总被引:11,自引:11,他引:11  
李刚  李文莉 《岩矿测试》2002,21(3):223-226
采用Fe3 + 盐和 1 ,1 0 -二氮杂菲作干扰抑制剂 ,氢化物 -原子荧光光谱法直接测定铜矿中微量硒和碲。H2 SO4和HClO4的存在对硒、碲有明显的增敏作用。方法检出限分别为LD(Se) =0 .1 5 μg/L ,LD(Te) =0 .2 0 μg/L。方法适用于w(Cu) <2 5 %的铜矿和其它岩石样品中硒和碲的测定 ,经标样分析验证 ,结果与标准值相符 ,1 2次测定的RSD分别为RSD(Se) =4.2 2 % ,RSD(Te) =6.3 1 %。  相似文献   

5.
文章描述了一种火焰原子吸收光谱法测定矿物及精矿中铌钽的方法。样品经KHSQ_4熔融,柠檬酸提取,在1000μg/ml Al存在下直接喷入N_2O—C_2H_2火焰。Al的存在不仅对Nb、Ta吸收信号有较强的增敏作用。而且还能消除Nb、Ta相互干扰及Ca、Ti、V对Nb、Ta的干扰。本法测定Nb、Ta的炅敏度分别为8.8μg/ml和13.7μg/ml。与使用有毒、危害较大的HF方法灵敏度相当或有所提高(Nb 22μg/ml、Ta 11μg/ml)。此法适合于矿物及精矿中含量大于5%Nb_2O_5和Ta_2O_5的测定。  相似文献   

6.
研究了多种负载泡塑对Au、Ag、Ti、Cd的富集行为。提出了在HCI-KI-抗坏血酸介质中用甲基异丁基酮(MIBK)负载泡塑同时萃取,然后用2%硫脲-1%HCl解脱的富集方法,并采用火焰原子吸收连续测定地质样品中痕量Au、Ag、Tl和Cd,方法的测定下限(μg/g)分别为:0.2g、0.05、0.20和0.04。  相似文献   

7.
何炼  杨威 《地质与资源》2004,13(3):175-177
应用氢化物-原子荧光光谱法同时测定化探样品中的Bi和Se,用1:1王水处理样品,在10%的盐酸介质中测定Bi、Se,其检出限分别为0.0005μg/mL和0.0002μg/mL.本方法具有一次熔矿便可以同时测定Bi、Se的含量,且具操作简单、快速、基体干扰少、灵敏度高、其结果稳定、可靠、节省试剂等特点,适用于大批化探样品中Bi、Se同时联测.  相似文献   

8.
离子色谱法同时测定地质样品中氟氯磷硫   总被引:5,自引:0,他引:5  
陈德勋  梁汉文 《岩矿测试》1991,10(3):189-192199
本文研究了离子色谱同时测定地质样品中F~-、Cl~-、PO_4~(3-)、SO_4~(2-)的前处理过程,选择了色谱测定最佳条件。在Na_2CO_3全熔的样品溶液中,加入(NH_4)_2CO_3使Si、Al随大多数金属离子同时沉淀;再用预处理柱除去熔剂引入的大量Na~+及CO_3~(2-)消除其干扰;并在流出液中补加相应试剂与淋洗液相匹配,实现了多种地质样品中F~-、Cl~-、PO_4~(3-)和SO_4~(2-)的测定。方法检出限(3s,μg/ml)分别为F~-0.05、Cl~-0.1、PO_4~(3-)0.3、SO_4~(2-)0.5。测定范围为F~-0.05—3μg/ml,Cl~-0.1—6μg/ml,PO_4~(3-)0.3 —30μg/ml,SO_4~(2-)0.5—30μg/ml。  相似文献   

9.
张佩瑜  金义 《岩矿测试》1988,(3):224-227
研究了辉锑矿中微量砷的氢化物发生一原子吸收光谱测定方法,选择高锰酸钾溶液消除大量锑氢化物的干扰。方法简便快速、灵敏。在选定最佳条件下,测定砷的灵敏度为0.26ng/ml(1%吸收),700μg/ml的锑不干扰砷的测定。对0.02μg/ml砷的测定,相对标准偏差为1.8%。可用于测定辉锑矿中0.0001%以上的砷。  相似文献   

10.
氢化物发生-火焰分子发射光谱法测定地质样品中的砷   总被引:2,自引:0,他引:2  
本文研究了氢化物发生-火焰分子发射光谱测定地质样品中As的方法,提出并采用了一种新型分子发射炉(腔)——长缝式石英炉。该方法具有设备简单、操作方便、干扰少、线性动态范围宽等特点。方法检出限为0.02μg/ml,对0.5μg/ml As的样品测定,其RSD(n=10)为1.5%。用GSS及MGD系列部分标样验证了方法的可靠性。  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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