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1.
氢化物-原子荧光光谱法直接测定地质物料中痕量锗   总被引:1,自引:0,他引:1  
采用特种空心阴极灯作激发光源和具有氩氢火焰低温自动点燃装置的原子荧光仪,氢化法直接测定地质物料中痕量锗,方法的测定下限为0.02μg/g,线性范围1~400μg/L,精密度(RSD,n=11,116μg/gGe)为1.79%,加标回收率97.8%。经标样和大批量样品分析验证,方法可靠实用  相似文献   

2.
发展了一种可在野外快速测定0.010—50μg/g银量的新方法。此法由两个各自独立而又配套的部分组成。一是直接测定0.25—50μg/g银量的Ag-TMK-SDS三元络合物光导比色测定法;二是测定0.010—0.25μg/g银量的巯基棉分离富集微珠析出比色法。可在同一份试液中依次完成。前者检出限为0.006μg/ml(K=3);测定铜、铅和锌矿石标样GSO-Cu-1(含银3.87μg/g)、GSO-Ph-1(含银14.7μg/g)和GSO-Zn-1(含银13.5μg/g)中的银,RDS(n=11)分别为1.6%、3.7%和3.4%;后法可检出5ng/g银;测定地球化学标样GSD-3(含银0.59μg/g)中的银,RSD(n=11)为6.t%。方法较为简便、快速、准确和灵敏。用光导比色计测定,结果准确度、精度均有较大改善,且与室内原子吸收法相当。故所定方法具有广阔的应用前景。  相似文献   

3.
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   

4.
催化还原褪色光度法测定痕量锡   总被引:7,自引:1,他引:6  
周之荣 《岩矿测试》1998,17(4):279-281
痕量锡在0.04mol/LH3PO4介质中对NaH2PO2还原罗丹明B褪色反应有催化作用,催化程度与Sn量、温度和加热时间线性相关。基于此,建立了痕量锡的动力学光度分析方法。方法检出限为0.034μg/L,线性范围为0~20μg/L,结合磷酸三丁酯色谱分离,实现了地质样品中痕量Sn的测定。方法经国家地质标准物质分析验证,结果与标准值相符。对于w(Sn)为10-6水平的试样其RSD(n=6)<6.5%。  相似文献   

5.
悬浮液原子荧光光谱法测定化探样品中的痕量汞   总被引:3,自引:0,他引:3  
王桂清  刘汉东 《岩矿测试》1996,15(4):293-295
拟定了将悬浮液技术与汞蒸气原子荧光光谱法相结合测定化探样品中痕量Hg的分析方法。控制悬浮液中试样粒度在200目,试样质量浓度15g/L,用电磁搅拌和载气搅拌保证悬浮液分散稳定,水溶液标准作校正曲线,方法的检出限为6ng/gHg。对水系沉积物国家标准物质中痕量Hg进行测定,结果与标准值相符,对含Hg010μg/g的GBW07305(GSD5)测定11次,x为0105μg/g,RSD为54%。  相似文献   

6.
汤志勇  敖愫 《岩矿测试》1998,17(4):285-289
建立了一个碱性体系在线氢化物发生原子荧光光谱法测定铜矿石中痕量砷、锑、铋的分析方法。设计了在线氢化物发生流路及操作程序。选择了碱性体系氢化物发生的各项最佳条件,避免了Cu、Fe等大量基体元素的干扰。方法检出限为As0.6μg/L,Sb0.4μg/L,Bi0.9μg/L,As、Sb、Bi的工作曲线均在0~400μg/L内呈良好的线性,经铜矿石国家一级标准物质分析验证,砷锑铋的测定结果与标准值吻合,相对标准偏差(RSD,n=5)在4.2%~8.8%。  相似文献   

7.
研究了在KH2PO4Na2B4O7缓冲介质中,痕量镍催化H2O2氧化胭脂红褪色的指示反应及动力学条件,测定了反应活化能,建立了动力学光度法测定痕量镍的新方法。方法检出限为240×10-8g/L,测定范围为008~24μg/L。结合丁二酮肟正丁醇萃取分离,实现了对铝合金标样中痕量镍的测定,RSD(n=6)小于3%。  相似文献   

8.
钼—邻苯二酚紫多元配合物协同增敏显色的研究   总被引:1,自引:0,他引:1  
陈昭国  陈曦 《岩矿测试》1999,18(1):50-52
研究了在pH4~6的弱酸性介质中,羟胺(HY)和溴化十二烷基吡啶(DPB)在钼、邻苯二酚紫(PV)配合物中的增敏作用和显色条件。有色配合物的最大吸收峰为718nm,表观摩尔吸光系数达1.2×106L·mol-1·cm-1,钼的检出限为0.6μg/L,反应在室温下瞬间完成,方法的线性范围在0.8~100μg/LMo,对w(Mo)在10-3水平的试样测定4次,RSD为4.6%~6.2%。对企业标准钢样的测定结果与推荐值相符。  相似文献   

9.
发射光谱法测定碳酸盐岩石样品中8个痕量元素   总被引:4,自引:3,他引:4  
张文华  张芳 《岩矿测试》1995,14(1):37-40
文章报道了用于测定碳酸盐岩石样品中痕量Be,B,Sn,Ag,Mo,Cu,Pb和Ga的交流电弧光谱定量分析方法,研究了多种缓冲剂的缓冲效果和分馏效应,选择了最佳工作电流,电极规格和内元素。方法检出限为0.04~2.8μg/g精密度RSD(n=10)在5.2%~9.9%,经国家一极碳酸盐岩石标样和批量岩石样分析均获满意结果,方法能满足区域化探要求。  相似文献   

10.
感耦等离子体质谱法同时测定岩石中痕量元素的研究   总被引:3,自引:5,他引:3  
试验了含难熔组分的岩石样品的分解方法、熔剂用量,以及溶液中可溶盐量的控制和标准系列的熔剂匹配等问题;分别采用Re、Rh和In作内标,解决了基体效应及其基体导致的灵敏度漂移的影响,实现了不经分离富集直接用ICP-MS法测定岩石样品中34个痕量元素。方法测定限0.01~5μg/g,RSD(n=10)为2.6%~13%,已应用于地质试样分析,岩石标样分析结果与标准值相符。  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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