巯基棉富集-分光光度法测定铂

样品溶解后,加入还原剂氯化亚锡及助吸附剂水合肼,用巯基棉吸附微量铂。吸附物灰化后,灰分用王水溶解,溶液用双十二烷基二硫代乙酰胺(DDO)分光光度法测定铂。方法检出限为0.2μg/g(10.0g样品),铂量在0~20μg/g线性关系较好。方法经国家一级标准物质验证,铂的测定结果与标准值相符,12次测定的相对标准偏差(RSD)小于10%。     

巯基棉富集-光度法连续测定铬铁矿中的铂钯

在建立巯基棉富集-分光光度法联用系统的基础上,对螯合反应的pH、吸附酸度、显示剂用量、显色温度及体系稳定性等进行了优化选择,并将联用系统成功地应用于实际样品的富集分离分析。在盐酸介质中,α-呋喃二肟与钯得黄色络合物,于λmax=380nm处测定其吸光度,HSCT与铂反应生成2：1稳定络合物,于λmax=540nm处测定其吸光度,对Pt,Pd的检测限（3）分别为0．01μg／ml,0．005μg／ml,对国家一级标准物质进行验证,结果与标准值相符,加标回收率98．0％～102．5％,相对标准偏差为3．88％～8．97％。应用于实际样品的测定．结果满意。     

石墨炉原子吸收光谱法测定地质样品中的痕量铂、钯

本文提出了用717阴离子交换树脂富集铂、钯的石墨炉原子吸收光谱分析方法。对富集铂、钯的条件,共存离子的干扰情况以及在GF-2000型石墨炉中测定铂、钯的最佳条件进行了研究。样品用王水分解后,在10％的王水介质中,用717阴离子交换树脂富集铂、钯,以热的硫脲溶液解脱,在拟定的工作条件下,于石墨炉原子吸收光谱仪上进行测定,大量的共存离子不干扰测定。方法简便快速,检出限分别为Pt8.8×10~(-9)g/ml,Pd3.4×10~(-9)g/ml,方法的相对标准偏差分别为Pt7.09％Pd11.48％,适用于地质样品中铂、钯的测定,结果令人满意。     

双硫腙改性氧化石墨烯/壳聚糖复合微球固相萃取在线富集-原子荧光光谱法测定地质样品中痕量汞

汞可以指示矿床或矿化存在,是一种重要的地质过程示踪元素,因此汞的测定是十分重要的。由于汞在地质矿床中丰度较低,直接测定存在困难,需要进行预分离富集处理。目前采用的分离富集手段大多数是离线,自动化程度较低。本文将合成的双硫腙改性氧化石墨烯/壳聚糖复合微球制成固相萃取小柱,考察了溶液pH、吸附剂种类和体积对汞的吸附效果的影响,优化了固相萃取在线采样/洗脱时间和速率对汞的吸附/洗脱效果的影响,建立了固相萃取在线富集-原子荧光光谱法测定地质样品中痕量汞的分析方法。结果表明:溶液pH=3.0时,以5 mL/min的采样速率进样5 min,汞的吸附率大于90%;用20 g/L硫脲-1.0mol/L硝酸混合溶液作洗脱液,以1 mL/min的洗脱速度洗脱1 min,洗脱率大于95%。汞含量在0.050~5.0μg/L范围内线性关系良好,富集因子为22,检出限为0.0019μg/L。采用本方法测定了土壤和沉积物国家标准物质样品,Hg的测定值与参考值的相对误差小于±13%。与离线分析相比,本方法具有灵敏度高、操作简单快速等特点。     

聚酰胺树脂富集分离-光度法连续测定铂和钯

试验了在柱层析操作条件下,聚酰胺树脂对铂和钯的吸附性能.结果表明,在 0.001～3.5 mol/L的HCl(或王水)介质中,聚酰胺树脂对铂和钯的吸附容量分别为20.92和19.20 mg/g,被酸性硫脲溶液洗脱后,用双十二烷基二硫代乙二酰二胺光度法测定.方法用于矿石中微量铂、钯的富集分离和测定,结果与等离子体发射光谱法及推荐值相符.铂、钯回收率均在93.7%～99.2%,相对误差分别为5.56%和4.44%.     

D290树脂-活性炭吸附富集电感耦合等离子体质谱法测定铜精矿中铂钯

矿产品中痕量贵金属元素的测定通常需要富集分离,在检测过程中谱线干扰较多。本文对铜精矿样品在高温下灼烧除去碳和硫,采用盐酸+王水+氢氟酸消解体系进行分解,利用D290阴离子交换树脂-活性炭作为吸附剂富集铂和钯,以Y、In、Bi为内标元素,105Pd和195Pt作为测量同位素,用电感耦合等离子体质谱法(ICP-MS)测定铂和钯的含量。铂和钯的吸附率均达到90%以上,加标回收率分别为92.0%和96.0%,检出限分别为0.126 ng/g和0.105 ng/g,方法精密度(RSD,n=6)小于4%。应用于实际铜精矿样品分析,测定值与锍镍试金-ICP-MS测定结果一致。本法的样品处理体系最大限度地减少了样品中其他金属离子对待测元素的影响,选择的内标元素和高纯氦碰撞反应可有效地减少基体效应和同质异位素干扰。相比于锍镍试金法,该方法的样品前处理简单,铂和钯的富集效果明显,测定检出限低。     

聚酰胺树脂富集分离—原子吸收法测定地质样品中钯

拟定了以聚酰胺树脂为吸附剂在静态和动态操作条件下，对微量钯的选择性吸附分离方法。实验表明，树脂在0.001-2.0mol/L的HCl介质中，对钯的吸附性能很好，饱和吸附容量为19.22-12.88mg/g，平均吸附率为98.40%，吸附到树脂中的钯可用中性30g/L硫脲溶液（静态)和50g/L 硫脲溶液（动态）解脱，平均解脱率为96.95%，富集倍数可达100倍。结合原子吸收光度法，可用于矿石中微量钯的富集分离和测定，标准加入回收试验，回收率为96.0%-103.0%，标样分离结果与推荐值相符。     

巯基棉分离富集光度法测定矿石中微量钯

本文系统地研究了巯基棉柱分离富集钯(Ⅱ)的最佳条件,建立一种用0.1克巯基棉对微量钯(Ⅱ)分离富集的可行方法。解决了湿法溶样,用3,5-diCl-PADAT光度法测定矿石中微量钯时,常见离子Fe~(3+)、Al~(3+)和Ti(Ⅳ)等的干扰问题。方法操作简便、快速,结果准确。用于矿石样品测定,结果满意。     

ICP-MS法测定化探样品中痕量金铂钯的富集分离方法研究

本方法用HCl和H_2O_2分解试样,以泡沫塑料富集Au、Pt和Pd,在酸性介质中解脱,用电感耦合等离子体质谱法测定化探样品中痕量金铂钯,研究了富集解脱介质及浓度。结果表明,在0.5%NaI+0.5%KBr+20%HCl介质中泡沫塑料对Au、Pt、Pd的吸附率大于95%;在1%硫脲+2%KSCN+2%HCl解脱介质中Au、Pt、Pd的回收率高于90%。方法检出限为Au 0.072 ng/g,Pt 0.17 ng/g,Pd 0.096 ng/g,标准物质的测定值与标准值基本一致,准确度和精密度满足相关规范要求,因此该方法对化探样品中痕量金铂钯的测定有一定实用性。     

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。     

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.     

Inter-regional correlation of transgressions and regressions in the Cretaceous period

Well investigated platforms have been selected in each continent, and the history of Cretaceous transgressions and regressions there is concisely reviewed from the available evidence. The factual records have been summarized into a diagram and the timing of the events correlated between distant as well as adjoining areas.On a global scale, major transgressions were stepwise enlarged in space and time from the Neocomian, via Aptian-Albian, to the Late Cretaceous, and the post-Cretaceous regression was very remarkable. Minor cycles of transgression-regression were not always synchronous between different areas. Some of them were, however, nearly synchronous between the areas facing the same ocean.Tectono-eustasy may have been the main cause of the phenomena of transgression-regression, but certain kinds of other tectonic movements which affected even the so-called stable platforms were also responsible for the phenomena. The combined effects of various causes may have been unusual in the Cretaceous, since it was a period of global tectonic activity. The slowing down of this activity followed by readjustments may have been the cause of the global regression at the end of the Cretaceous.     

The lamprophyres of Afyon stratovolcano,western Anatolia,Turkey: description and genesis

The Afyon stratovolcano exhibits lamprophyric rocks, emplaced as hydrovolcanic products, aphanitic lava flows and dyke intrusions, during the final stages of volcanic activity. Most of the Afyon volcanics belong to the silica-saturated alkaline suite, as potassic trachyandesites and trachytes, while the products of the latest activity are lamproitic lamprophyres (jumillite, orendite, verite, fitztroyite) and alkaline lamprophyres (campto-sannaite, sannaite, hyalo-monchiquite, analcime–monchiquite). Afyon lamprophyres exhibit LILE and Zr enrichments, related to mantle metasomatism.     

METAMORPHIC PETROLOGY

正20140751 Guo Xincheng(Geological Party,BGMRED of Xinjiang,Changji 831100,China);Zheng Yuzhuang Determination and Geological Significance of the Mesoarchean Craton in Western Kunlun Mountains,Xinjiang,China(Geological Review,ISSN0371-5736,CN11-1952/P,59(3),2013,p.401-412,8     

GEOCHEMICAL EXPLORATION

正20141058 Chen Ling(Key Laboratory of Mathematical Geology of Sichuan Province,Chengdu University of Technology,Chengdu610059,China);Guo Ke Study of Geochemical Ore-Forming Anomaly Identification Based on the Theory of Blind Source Separation(Geosci-     

SEISMIC GEOLOGY

正20141334 Chen Kun(Institute of Geophysics,China Earthquake Administration,Beijing100081,China);Yu Yanxiang Shakemap of Peak Ground Acceleration with Bias Correction for the Lushan,Sichuan Earthquake on April20,2013(Seismology and Geology,ISSN0253-4967,CN11-2192/P,35(3),2013,p.627-633,2 illus.,1 table,9 refs.)Key words:great earthquakes,Sichuan Province     

HISTORICAL GEOLOGY & STRATIGRAPHY

正20141624 Cai Xiongfei(Key Laboratory of Geobiology and Environmental Geology,Ministry of Education,China University of Geosciences,Wuhan 430074,China);Yang Jie A Restudy of the Upper Sinian Zhengmuguan and Tuerkeng Formations in the Helan Mountains(Journal of Stratigraphy,ISSN0253-4959CN32-1187/P,37(3),2013,p.377-386,5 illus.,2 tables,10 refs.)     

PALEONTOLOGY

正20142263Lü Shaojun(Geological Survey of Jiangxi Province,Nanchang 330030,China)Early-Middle Permian Biostratigraphical Characteristics in Qiangduo Area,Tibet(Resources SurveyEnvironment,ISSN1671-4814,CN32-1640/N,34(4),2013,p.221-227,2illus.,2tables,22refs.)Key words:biostratigraphy,Lower Permian,Middle Permian,Tibet     

MATHEMATICAL GEOLOGY

正20142560Hu Hongxia(Regional Geological and Mineral Resources Survey of Jilin Province,Changchun 130022,China);Dai Lixia Application of GIS Map Projection Transformation in Geological Work(Jilin Geology,ISSN1001-2427,CN22-1099/P,32(4),2013,p.160-163,4illus.,2refs.)     

GEOCHEMISTRY

正20140692 Duo Tianhui(No.402 Geological Team,Exploration of Geology and Mineral Resources of Sichuan Authority,Chengdu611730,China);Wang Yongli Computer Simulation of Neptunium Existing Forms in the Groundwater(Computing Techniques for Geophysical and Geochemical Exploration,ISSN1001-1749,CN51-1242/P,35(3),