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1.
地质样品中微量金银的在线分离富集方法   总被引:4,自引:0,他引:4  
提出用VS-Ⅱ型强碱性阴离子交换纤维定量富集,硫脲解脱,流劝注射在线分离富集-火焰有收光谱法测定地质样品中痕量金银的分析方法。该方法检出限低,金为1.4μg/mL,银为0.35μg/mL,相对标准偏差小于2%,采样频率为120次/h,用于地质样品中痕量金银的直接测定,结果令人满意。  相似文献   

2.
流动注射液-液萃取分光光度法测定地质样品中的碘   总被引:2,自引:0,他引:2  
研究了流动注射在线液液萃取技术,设计了一种既适用于水相又适用于有机相光度分析的流通池,进行了地质样品中痕量碘的在线萃取及光度测定,方法的富集因子50,富集效率25,测定样品速度为30样次/h,检出限为38μg/L,对于20μg/L的I-,其RSD(n=11)为17%,方法用于水系沉积物和土壤标样中碘的验证,结果与标准值吻合  相似文献   

3.
流动注射液—液萃取分光光度法测定地质样品中的碘   总被引:2,自引:0,他引:2  
师琴  向雪云 《岩矿测试》1996,15(3):222-225
研究了流动注射在线液-液萃取技术,设计了一种既适用于水相又适用于有机相光度分析的流通地,进行了地质样品中痕量碘在线萃取及光度测定,方法的富集因子50,富集效率25,测定样品速度为30样次/h,检出限为3.8μg/L的I^-,其RSD为1.7%,方法用于水系沉积物和土壤标样中碘的验证,结果与标准值吻合。  相似文献   

4.
本研究采用自行合成的二苯硫脲纤维素作为在线富集介质,流动注射与原子吸收法联用快速测定地质样品中痕量金。在本法选定条件下,测定速度为30样/h,测定灵敏度为0.31μg/ml(1%吸收),RSD为2.59%。  相似文献   

5.
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   

6.
李良万  苏庆平 《矿物岩石》1998,18(3):112-114
本研究采用自行合成的二苯硫脲纤维素作为在线富集介质,流动注射与原子吸收法联用快速测定地质样品中痕量金,在本法选定条件下,测定速度为30样/h,测定灵敏度为0.31μg/ml(1%吸收),RSD为2.59%。  相似文献   

7.
催化还原褪色光度法测定痕量锡的研究   总被引:2,自引:0,他引:2  
痕量锡在稀磷酸介质中对次磷酸钠还原甲基绿褪色反应有催化作用。基于此,本文建立了痕量锡的动力学光度分析法。方法检出限为0.0066μg/L,线性范围为0 ̄4μg/L。结合磷酸三了酯色谱分离,实现地质样品中痕量锡的测定,结果与标准值相符。  相似文献   

8.
张勤  孙晓玲 《岩矿测试》1996,15(3):183-187
经萃取分离富集后,在pH2.6的苯二甲酸氢钾HCl介质中,用电流氧化溶出计时电位法测定地质物料中痕量In。方法检出限为0.01μg/g,标样中In的含量为0.10μg/g时的方法精密度(RSD,n=11)为8.76%,加标回收率为98%~105%。应用此方法测定了国家一级地球化学标准参考物质(GSR1~6,GSS1~8,GSD9~12)中的痕量In,获得了较为满意的测定结果  相似文献   

9.
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   

10.
作者对激光热透镜光谱法测定微量钼进行了研究.试验表明,在丙酮介质中,Mo6+能被还原成Mo5+并形成钼蓝同多酸,最大吸收彼长在670um处,利用He-Ne激光器输出的632.8um的激光作光源,进行微量钼的热透镜法分析测定.两酮的存在能增强热透镜信号强度。钼含量在0.01—2.0μg/mL范围内与激光热透镜信号强度呈良好的线性关系,方法检出限为0.005μg/mL钼,已用于地质样品中微量钼的高灵敏度测定.结果满意.  相似文献   

11.
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   

12.
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.
正20141520 Bo Ying(Key Laboratory of Metallogeny and Mineral Assessment,MLR,Beijing 100037,China);Liu Chenglin Saline Spring Hydrochemical Characteristics and Indicators for Potassium Exploration in Southwestern and Northern Tarim Basin,Xinjiang(Acta Geoscientica Sinica,ISSN1006-3021,CN11-3474/P,34(5),2013,p.594-602,5 illus.,3 tables,28 refs.)  相似文献   

15.
正20141243Chen Ge(Hangzhou Research Institute of Petroleum Geology,PetroChina,Hangzhou 310023,China);Si Chunsong Study on Sedimentary Numerical Simulation Method of Fan Delta Sand Body(Journal of Geology,  相似文献   

16.
正20142599Chen Sanming(Guangxi Key Laboratory of Concealed Deposits Exploration,Guilin University of Technology,Guilin541004,China);He Yuzhou Block Model and Reserves Estimation of Panzhihua Iron Deposit Based on 3D Geological Modeling(Journal of Guilin University of Technology,ISSN1674-9057,CN45-1375/N,33(4),2013,p.610-615,9illus.,1table,15refs.)  相似文献   

17.
正20140594 Bai Daoyuan(Hunan Institute of Geology Survey,Changsha 410016,China);Zhong Xiang Faults in the Jingzhou Basin and Their Tectonic Settings(Geotectonica et Metallogenia,ISSN1001-1552,CN44-1595/P,37(2),2013,p.173-183,6illus.,59refs.)Key words:basin evolution,tectonic setting,South China In the Upper Paleozoic and Jurassic se-  相似文献   

18.
正20141912Cao Hui(State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)Gravitational Collapse and Folding during Orogenesis:A Comparative Study of FIA Trends and Fold Axial Plane Traces(Geology in China,ISSN1000-3657,CN11-1167/P,40(6),2013,p.1818-1828,9illus.,35refs.,with  相似文献   

19.
PALEOZOOLOGY     
正20141609 Chen Guiying(College of Earth Sciences,Guilin University of Technology,Guilin 541004,China);Han Nairen New Materials of Stylophora from the Upper Cambrian of the Jingxi Area,Guangxi,South China(Acta Palaeontologica Sinica,ISSN0001-6616,CN32-1188Q,52(3),2013,p.288-293,2 illus.,12 refs.)Key words:Stylophora,Guangxi  相似文献   

20.
GEOPHYSICS     
正20140634 Cao Lingmin(Key Laboratory of Marine Geology and Environment,Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071,China);Xu Yi Finite Difference Tomography of the Crustal Velocity Structure in Tengchong,Yunnan Province(Chinese Journal of Geophysics,ISSN0001-5733,CN11-2074/P,56(4),2013,p.1159-1167,6illus.,35refs.,with English abstract)  相似文献   

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