亚硝酸根的一个高选择性指示反应的研究——溴酸钾-依来铬青R体系

本文研究了亚硝酸根的一个新指示反应。它基于在稀磷酸溶液中,依来铬青R与溴酸钾的反应受亚硝酸根催化而使吸光度降低。方法sandell灵敏度为1.11×10~(-4)μgN/cm~2。有较高选择性。表观活化能为84.52KJ/mol。用于水样中痕量亚硝酸根的测定,对含NO_2~-3.03μg/L和39.8μg/L的水样变异系数(n=9)分别为2.40％和2.42％。精密度亦佳。     

甲基绿-高碘酸钾催化光度法测定痕量铂

利用痕量铂 (IV)在稀磷酸介质中对高碘酸钾氧化甲基绿褪色反应的催化作用 ,建立了测定痕量铂 (IV)的催化动力学光度法。方法检出限为 3.4× 10 - 1 0 g/mL ,线性范围为 0～ 2 4μg/L。用于催化剂及矿石中铂的测定 ,结果满意。     

黄原酯棉富集—火焰原子吸收法测定盐和水样中的痕量铅

本文介绍用黄原酯棉富集-火焰原子吸收法测定盐和水样中的痕量Pb,用于盐样中0.5—20μg/g和水样中5—200μg/L Pb的测定,结果与其它方法基本吻合。     

碱性模式氢化物发生—原子荧光光谱法测定土壤中的痕量硒

土壤样品经王水分解，转化成HCl溶液，再用NaOH溶液调至碱性，样品溶液首先与KBH4混合，然后与酸作用完成氢化物发生，用原子荧光光谱法测定样品中的痕量硒。方法检出限为0.01μg/g。线性范围为1－200μg/L，样品中硒的含量为0.082μg/g和0.34μg/g时，RSD（n=12)分别为4.9%和2.9%。方法经土壤国家一级标准物质中硒的测定验证，结果与标准值相符。     

悬浮液进样石墨炉原子吸收光谱法测定环境样品中痕量铅

提出了悬浮液进样石墨炉原子吸收光谱法测定环境样品中痕量铅的分析方法.讨论了悬浮颗粒粒径、悬浮液浓度、悬浮稳定剂、基体改进剂等因素对测定结果的影响.实验结果表明: 样品粒径 < 38μm, 以0.2g/L的Triton - 100为悬浮剂, 3g/L的(NH₄)₂HPO₄为基体改进剂, 电磁搅拌进样可简便快速地测定地质样品中的痕量铅, 方法的检出限为0.10ng/g, 精密度为3.31% (n =10).43GSD标样测定结果与推荐值一致      

冷蒸气原子荧光法测量地球化学样品中痕量汞

用冷蒸气原子荧光法测量地球化学样品中痕量汞,对载气流量、试液酸度、硼氢化钾浓度等进行了试验。工作曲线线性范围为0～4μg/L,方法检出限为0.002 3μg/g,精密度RSD%为1.1~5.0。方法用国家一级地球化学标准物质中汞的测定,结果与标准值一致。     

巯基棉分离富集-荧光分光光度法测定地下水中的痕量硒

在盐酸介质中,利用巯基棉分离富集地下水中痕量硒,然后在HC l-HNO3混合酸溶液及沸水浴加热条件下解脱富集的硒。通过测定2,3-二氨基萘与Se(Ⅳ)反应生成4,5-苯并苤硒脑的荧光强度,进而实现地下水中痕量硒的测定。实验表明,荧光光度法测定硒的线性范围为0~1.0μg,最低检测浓度为0.03μg/L,应用此法测定0.1μg/L硒的地下水,相对标准偏差小于7%,回收率达91%~105%,可满足地下水中硒的测定要求。     

连续流动化学发光法测定地质样品中的银

采用732阳离子交换树脂静态吸附分离，以Luminol-K2S208-Ag^ -乙二胺体系，连续流动化学发光法测定地质样品中的痕量银。该方法的检出限为4μg／L，9次测定8．8μg/Ag的标样07-GRD-35，x＝8．5μg／g，RSD为2．5％，经地质标样测定，验证结果的相对误差小于15％，适于野外快速测定银。     

分散液-液微萃取—火焰原子吸收光谱法测定水样中的痕量铅

对萃取剂和分散剂进行了筛选,并研究了pH、APDC的用量、萃取时间等试验条件对萃取效率的影响。将分散液-液微萃取(DLLME)与火焰原子吸收光谱法(FAAS)相结合,建立了快速、高灵敏度测定水样中痕量铅的新方法。在优化条件下,富集6.0mL样品溶液,铅的检出限为1.35μg/L,线性范围10.0～600.0μg/L,对含有20μg/L和400μg/L Pb2+的标准溶液平行萃取测定11次,相对标准偏差分别为3.35%和2.78%。本方法应用于自来水、河水、地下水和海水中痕量铅的分析,加标回收率在95.5%～99.7%之间。     

原子吸收法测定煤矿地下水中痕量铜、铅、锌

我们用原子吸收法测定煤矿地下水中痕量铜、铅、锌。其测定范围为0.001—2.00mg/L,回收率为96—102％,变动系数<10％,铜锌灵敏度为0.044μg/ml,铅灵敏度为0.097μg/ml。      

The terrestrial fauna of the Late Triassic Pant-y-ffynnon Quarry fissures,South Wales,UK and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia)

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.     

The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts

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.     

Quaternary stresses revealed by calcite twinning inversion: insights from observations in the Savonnières underground quarry (eastern France)

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).     

HYDROGEOLOGY

正20141756 Chen Ruige(Mathematical College,China University of Geosciences,Beijing100083,China);Zhou Xun Numerical Simulation of Groundwater Level Fluctuation in a Coastal Confined Aquifer with Sloping Initial Groundwater Level Induced by the Tide(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(7),2013,p.1099-1104,6 illus.,16 refs.) Key words:confined water,groundwater level     

METAMORPHIC PETROLOGY

正20141408 Cai Jia(Institute of Geology,Chinese Academy of Geological Sciences,Beijing100037,China);Liu Fulai Petrogenesis and Metamorphic P-T Conditions of Garnet-Spinel-Biotitebearing Paragneiss in Danangou Area,Daqingshan-Wulashan Metamorphic Complex Belt(Acta Petrologica Sinica,ISSN1000-0569,CN11-1922/P,29(7),     

SERIALS

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GEOPHYSICAL EXPLORATION

正20142386An Guoying(China Aero Geophysical Survey and Remote Sensing Center for Land and Resources,Beijing 100083,China)Application of Satellite Remote Sensing in Regional Hydrogeological Investigation:Taking Cenozoic Strata in Wenquan Sheet(1∶250 000)of Karakoram Range as an Example(Geosci-     

QUATERNARY GEOLOGY & GEOMORPHOLOGY

正20141016An Chengbang(Key Laboratory of Western China’s Environmental Systems,Ministry of Education,Lanzhou University,Lanzhou 730000,China);Zhao Yongtao Lake Records during the Last Glacial Maximum from Xinjiang,NW China and Their Climatic Impli-     

PETROLEUM GEOLOGY

正20141538 Cao Qing(School of Earth Sciences and Engineering,Xi’an Petroleum University,Xi’an 710065,China);Zhao Jingzhou Characteristics and Significance of Fluid Inclusions from Majiagou Formation,Yichuan Huangling Area,Ordos Basin(Advances in Earth Science,ISSN1001-8166,CN62-1091/P,28(7),2013,p.819-828,7 illus.,3 tables,43 refs.)     

GEOCHEMISTRY

正20142002 Wei Hualing(Institute of Geophysical and Geochemical Exploration,Chinese Academy of Geological Sciences,Langfang065000,China);Zhou Guohua Element Content and Mineral Compositions in Different Sizes of Soil in Tongling Area,Anhui Province(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(11),2013,p.1861