双台子河口区水中重金属污染评价及其生态效应分析

对研究区的地表水、地下水以及海水分别采样，并进行重金属含量分析研究，参照有关标准进行了水中重金属污染评价，结果表明：地下水中基本上不存在重金属污染；各种水中不存在砷污染；镉污染相对比较普遍；在海水中，翅碱蓬退化与重金属铜、锌、铅、铬、镍的污染关系密切。     

运用轻便触探和静载荷试验研究黄土的湿陷性(英文)

黄土在应力作用下迂水时力学强度迅速下降 ,产生大范围的快速沉陷。这就是黄土的湿陷性 ,是黄土的诸多特性之一。鉴于对黄土湿陷性以往用各种实验室试验指标进行评价 ,这里提出运用动力触探和静载荷试验进行黄土湿陷性原位评价的一种简便的新方法。该方法的试验程序是 ,先用轻便可变动能触探仪在天然状态和饱水状态下进行触探试验 ,而后在触探孔完成静载荷压缩性试验。运用中国黄土高原黄土原位动力触探和静载荷试验测得的资料 ,详细分析了天然状态的黄土对探头阻力 qdnat,饱水状态的黄土对探头阻力 qdsat,实验室测得的湿陷性指数s压缩曲线参数 (即触探极限压力 ppf,触探蠕变压力ppl 和触探载荷模量Epn)的关系。结果证明所提出的方法适用于原位判定黄土的湿陷性。     

内蒙古某矿矿井水重金属污染特征及来源分析

确定矿井水中重金属污染程度及主要来源,对矿井水的再利用及矿区生态环境保护具有重要的理论意义。以内蒙古某矿区为研究对象,采集地表水、第四系潜水、承压水及矿井水水样49组,检测水体中Zn、Pb、Fe、Mn、As、Cu、Cd、Cr、Hg、Se 10种重金属浓度,分析矿井水中重金属污染特征及超标情况,利用HPI模型定量评价重金属污染程度,并综合数理统计、不同类型水样重金属浓度箱形图及煤/顶板重金属浸出试验,分析矿井水重金属主要来源。结果表明:内蒙古某矿矿井水中Zn、Pb、Fe、Mn、As 5种重金属浓度值超标,其中Fe和Zn的超标率高达100%;7个矿井水样中6个矿井水的HPI值大于临界值100,矿井水重金属污染程度较高;矿井水中的Pb、As主要来源于采煤及运输机械油类物质泄漏,Mn主要来源于Ⅲ含地下水,Fe、Zn主要来源于Ⅲ含地下水及煤层中含Fe、Zn矿物的溶滤。该结论将为矿井水中重金属污染防治提供基础与依据。      

矿用本安型救援系统供电技术

井孔救援探头一般采用井口有线供电方式。按照矿用本质安全型防爆设计要求,分析了电缆线路分布的电感、电容对本质安全性能的影响;给出了救援探头功率、双绞传输线长度和井口电源电压的关系。用两种模型的影响因子,给出在实际设计时,井口电源电压、供电距离和探头功率等参数的选择方法。该长线供电参数的分析与设计方法,在800 m本安型救援系统中应用,证明切实可行。      

理论α系数法波长色散X射线荧光测定土壤中的重金属

近年来,重金属带来的土壤污染问题日益严重,快速、准确、有效地测定土壤中重金属种类及含量对土壤重金属污染评估及后续污染防治具有重要意义。本研究建立了波长色散X射线荧光光谱法同时测定土壤样品中铬、铅、锌、铜、钴、镍、锰、钒8种重金属元素含量的检测方法,通过经验法与理论α系数法的结合,优化了实验条件,方法线性良好,准确度与精密度较高,并且极大的简化了测定过程,提高了工作效率。将应用于土壤重金属含量初步评估,与ICP-MS的测定结果吻合度高。土壤监测结果表明,目标区土壤均符合二级土壤限量标准,该区土壤环境质量总体较好。而且该法减少了实验前处理过程中化学试剂的使用,避免了前处理过程中带来的环境污染问题,适用于规模较大的地质、农业、环境监测分析等生产单位进行土壤中重金属元素的快速测定。     

理论α系数法波长色散X射线荧光测定土壤中的重金属

近年来,重金属带来的土壤污染问题日益严重,快速、准确、有效地测定土壤中重金属种类及含量对土壤重金属污染评估及后续污染防治具有重要意义。本研究建立了波长色散X射线荧光光谱法同时测定土壤样品中铬、铅、锌、铜、钴、镍、锰、钒8种重金属元素含量的检测方法,通过经验法与理论α系数法的结合,优化了实验条件,方法线性良好,准确度与精密度较高,并且极大的简化了测定过程,提高了工作效率。将应用于土壤重金属含量初步评估,与ICP-MS的测定结果吻合度高。土壤监测结果表明,目标区土壤均符合二级土壤限量标准,该区土壤环境质量总体较好。而且该法减少了实验前处理过程中化学试剂的使用,避免了前处理过程中带来的环境污染问题,适用于规模较大的地质、农业、环境监测分析等生产单位进行土壤中重金属元素的快速测定。     

电解二氧化锰制备条件与晶体结构及电气性能的关系.不同电解液体系的影响

在MnSO-4-H-2SO-4和MnCl-2-HCl电解液体系中分别制备出电解二氧化锰(EMD),并在该二电解液中制备出掺杂MnO-2样品,而后用X射线衍射确定其晶型为MnO-2-γ,用扫描电镜观察其表面形貌,用XPS研究掺钛EMD表层物种;用模拟电池在实验室中快速检测掺杂样品的电性能,进而探讨了不同电解液体系中制备所得MnO-2与其晶体结构及电气性能的关系.     

重庆老龙洞地下河间隙水重金属污染及毒性评估

为查明重庆岩溶地区老龙洞地下河重金属污染情况,于2013年9月采集了地下河上覆水体和表层沉积物间隙水共7组水样,用ICP-OES测定地下河上覆水体和表层沉积物间隙水中的Mn含量,ICP-MS测定Cu、Cd、Cr、As和Pb含量,分析了老龙洞地下河表层沉积物间隙水中各重金属元素的空间分布,对不同介质中的重金属元素进行相关性分析,并参考美国EPA推荐的“国家推荐水质标准”对间隙水中重金属可能产生的生物毒性进行评估。结果表明:老龙洞地下河上覆水体中Mn和Pb的浓度超过了GB 5749-2006规定的生活饮用水限值（Mn≤100 ug/L,Pb≤10 ug/L）,不可作为饮用水源;间隙水中各重金属元素的浓度都比上覆水体高,有向上覆水体扩散的潜在可能性。除Pb、Mn外,间隙水中重金属的含量大小依次为上游>中游>下游。上覆水中除Mn与As、Cd与Cr外,其他金属元素之间的相关性不大;间隙水中Cr、Cu、As和Cd的相关系数分别为0.895～0.997,呈高度正相关。间隙水中金属元素除As不会对水生生态系统产生急性毒性外,Cr、Cu、Cd和Pb都会对水生生态系统产生急性毒性,尤以Cr、Cu、Cd最为严重。      

地质物料中痕量硒碲的离子交换分离与诱导比色测定

本文用硝酸或逆王水分解样品,控制硝酸酸度为0.05—0.18N。用活性炭吸附银和有机质,吸取清液上交换柱,使硒、碲与其他干扰离子分离,并直接用金溶胶诱导比色测定洗出液中的硒。然后用0.8—0.9硝酸洗提碲,用金溶胶诱导比色测定之。 方法简便、快速、检测限低、精密度、准确度能满足地球化学找矿的要求。     

ICP-MS检测水中碘的方法研究

建立了电感耦合等离子体质谱法快速检测水中碘的方法。在没有碘标准溶液的情况下,应用经验公式,通过镉、钡、铅的标准曲线能够准确检测水样中碘的质量质量浓度。经验公式计算的曲线与标准曲线不存在显著性差异。方法检出限0.062μg/L,精密度3.53%,加标回收率104.8%。建立的分析方法简便、实用,能够快速检测水中碘的质量质量浓度。     

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.     

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.     

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.     

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