用双波长分光光度法研究偶氮氯膦-mA与钍的显色反应

偶氮氯瞵-mA[2-(4-氯-2-膦酸基苯偶氮)-7-(3-乙酰苯偶氮)-1,8-二羟基-3,6-萘二磺酸)作为稀土元素高灵敏度显色剂,已有文献报导。本文用双波长分光光度法研究了偶氮氯膦-mA与钍的显色反应条件,实验证明,在0.02～0.3mol/L的盐酸介质中,偶氮氯膦-mA可与钍生成非常稳定的蓝紫色络合物,最大吸收在676nm。选用有色络合     

一些不对称双偶氮氯膦类显色剂测定钪的比较

华东师大合成的不对称双偶氮氯膦类显色剂是一类新型的稀土显色剂。这类显色剂有偶氮氯膦-mA,偶氮氯膦-mN,偶氮氯膦-mK,偶氮氯膦-PN(以下简称CPA-mA、mN、mK、pN)它们的结构式分别为:     

偶氮氯膦-mK双波长分光光度法测定硅石中的钛

在稀H2SO4介质中,乳化剂OP存在下,Ti(Ⅳ)与偶氮氯膦-mK发生显色反应,可用波峰(672nm)波谷(550nm)双波长吸光度叠加的方法测定Ti(Ⅳ)。显色反应的表观摩尔吸光系数为4.7×104L·mol-1·cm-1,灵敏度较单波长测定提高1.1倍。0～1200μg/LTi(Ⅳ)符合比尔定律。测定了硅石、焦宝石等试样中的钛,结果与标准值符合,6次测定的RSD<5%。     

2-(2-咪唑偶氮)-5-二乙氨基酚与钒的显色反应及其应用

研究了新试剂 2 - (2 -咪唑偶氮 ) - 5-二乙氨基酚 (IZAPN)与V(Ⅴ )的显色反应 ,在pH 5的HAc NaAc介质中 ,V(Ⅴ )与IZAPN形成稳定的紫红色络合物 ,其组成比为nV∶nR=1∶2 ,最大吸收波长位于 575nm ,表观摩尔吸光系数为 2 96× 1 0 4 L·mol- 1 ·cm- 1 ,V(Ⅴ )在 0～ 0 8mg/L内服从比尔定律。在NaF和硫脲联合掩蔽下 ,方法可用于铝合金和合成废水中V(Ⅴ )的测定 ,加标回收率 1 0 0 0 %～ 1 0 0 5% ,RSD(n =6)≤ 2 0 %。     

偶氮溴膦-pSN光度法测定地质样品中微量钪

本文主要研究了新显色剂偶氮溴膦—pSN(BPA—pSN)同钪的反应条件。拟定了光度测定地质样品中的的微量钪的测试方法。方法手续简便,灵敏度高。摩尔吸光系数为1.06×10~5L·mol~(-1)·cm.(-1)。Sc量在0～25μg/25ml范围服从比尔定律。对标准样品进行分析对照,结果满意。     

二安替比林对羟基苯乙烯基甲烷与钒的高灵敏显色反应

合成了试剂二安替比林对羟基苯乙烯基甲烷 (DApHVM) ,研究了它与V(Ⅴ )的显色反应。在H3PO4介质中 ,Mn(Ⅱ )和Tween 2 0协同作用下 ,DApHVM与V(Ⅴ )生成红色产物 ,λmax为 540nm ,ε=1 0 3× 1 0 6 L·mol-1 ·cm-1 ,V(Ⅴ )的质量浓度在 0～ 50 μg/L内符合比尔定律。方法用于中草药及钢样中V(Ⅴ )的测定 ,结果与原子吸收法一致 ,加标回收率在 96%～ 1 0 5 % ,5次测定结果的RSD <3 5 %。     

偶氮氯磷mA-溴化十六烷基吡啶光度法测定化探样品中钍

铀试剂Ⅲ光度法测定钍一般能满足岩石矿物分析要求,但对ppm级钍的化探样品的分析,由于试剂质量问题难以达到要求。偶氮氯膦Ⅲ虽然灵敏度较高,但需用有机溶剂萃取,且稀土和铀的干扰严重。偶氮氯膦mA[2-(4—氯—2—膦酸—苯偶氮)—7—(3—乙酰苯偶氮)—1,8—二羟基萘—3,6—二磺酸)]作为     

2—（四氮唑偶氮）—5—二乙氨基苯甲酸的合成及光度法测定钒

研究了新显色剂2 (四氮唑偶氮) 5 二乙氨基苯甲酸(简称TTZDBA)的合成。经元素分析、红外光谱、紫外光谱、核磁共振谱等方法测试确定其组成和结构。研究了试剂的性质及其与钒的显色反应的条件,建立了光度法测定钒的新方法。在pH3.5的HAc NaAc介质中,TTZD BA与V(Ⅴ)形成摩尔比为2∶1的紫红色配合物,配合物至少稳定18h,其最大吸收波长在566nm处,表观摩尔吸光系数为3.52×104L·mol-1·cm-1,V(Ⅴ)质量浓度在0～0.8mg/L内遵守比尔定律。经标样分析验证,结果与标准值相符,加标回收率为101.3%～102.8%,RSD(n=6)在1.0%～2.5%。所拟方法可不经分离直接测定铝合金样品及合成废水中的钒。     

2-（5-硝基-2-吡啶偶氮）-5-二甲氨基苯胺分光光度法测定铜

研究了2 (5 硝基 2 吡啶偶氮) 5 二甲氨基苯胺(5 NO2 PADMA)与铜的显色反应。结果表明,在pH4.5的HAc NaAc介质中,Cu与5 NO2 PADMA形成1∶2的紫红色配合物,λmax=550nm,ε=3.24×104L·mol-1·cm-1,Cu的含量在0～1.4mg/L内符合比尔定律。方法经铝合金和矿样管理样品分析验证,结果与原结果相符,5次测定的RSD小于0.7%。     

1-偶氮苯-3-（5-氯-2-吡啶）-三氮烯的合成及其与镍的显色反应

报道了新显色剂1-偶氮苯-3-(5-氯-2-吡啶)-三氮烯的合成及其与镍的显色反应。在pH10. 5的Na2B4O7-NaOH缓冲溶液中和表面活性剂OP存在下, 1-偶氮苯-3-(5-氯-2-吡啶)-三氮烯可与镍发生显色反应,生成3∶1的红色配合物,据此建立了分光光度法测定镍的方法。配合物的最大吸收峰位于540nm处,表观摩尔吸光系数为1. 62×105 L·mol-1·cm-1。Ni2+的质量浓度在0~480μg/L符合比尔定律。用拟定方法测定合金中的微量镍,结果与标准值相符, 6次测定的相对标准偏差(RSD) <2%。     

Définition d'une limite multicritère ; stratigraphie du passage Campanien–Maastrichtien du site géologique de Tercis (Landes,SW France)Definition of a multi-criteria boundary; stratigraphy of the Campanian–Maastrichtian interval of the geological site at Tercis (Landes,SW France)

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.     

Late Wuchiapingian (Late Dzhulfian,early Late Permian) limestone olistolites within the Tertiary flysch of Glypia Unit (Mount Parnon,central–eastern Peloponnesus,Greece)

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.     

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.)     

GEOCHEMICAL EXPLORATION

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.)     

MICROPALAEONTOLOGY

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.)     

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.,     

ENVIRONMENTAL GEOLOGY

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     

PROSPECTING EXPLORATION

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     

OCEANOGRAPHY & MARINE GEOLOGY

正20140582 Fang Xisheng(Key Lab.of Marine Sedimentology and Environmental Geology,First Institute of Oceanography,State Oceanic Administration,Qingdao 266061,China);Shi Xuefa Mineralogy of Surface Sediment in the Eastern Area off the Ryukyu Islands and Its Geological Significance(Marine Geology Quaternary Geology,ISSN0256-1492,CN37     

ENVIRONMENTAL GEOLOGY

正20141810 Bian Yumei(Geological Environmental Monitoring Center of Liaoning Province,Shenyang 110032,China);Zhang Jing Zoning Haicheng,Liaoning Province,by GeoHazard Risk and Geo-Hazard Assessment(Journal of Geological Hazards and Environment Preservation,ISSN1006-4362,CN51-1467/P,24(3),2013,p.5-9,2 illus.,tables,refs.)