偏重钻铤在丁集矿冻结造孔施工中的应用

钻井技术的关键是预防及控制孔斜,通过对目前常用4种防斜钻具组合的适岩性、井深、井斜及钻效等指标对比,在冻结造孔施工中选用了适用地层广、防斜性能好并具有纠斜作用的偏重钻铤。为发挥偏重钻铤的防斜作用,宜增大转速,并使钻铤减去部分的重量应位于离轴线尽可能远的部位。在淮南丁集冻结孔施工的三十多口钻孔中,井斜一般均在0．5°以内,钻效超过2400m/台·月。     

孔底注浆护壁在砂质含水层长螺旋钻孔灌注桩中的应用

阐述长螺旋钻机在含水砂层施工中钻孔坍塌的原因和孔底注浆护壁的工艺原理,并通过工程实例,介绍孔底注浆护壁工艺在长螺旋钻孔灌注桩中的应用和效果,拓展了长螺旋钻孔灌注桩的适用条件范围。     

护壁液在桥梁下部施工中的应用

本文介绍护壁液(泥浆)在钻孔灌注桩施工中的孔壁防护作用,分述了其类型、性能方式选用等内容,提出了施工过程中孔壁防护作业的注意事项。     

云南金平长安金矿大倾角钻孔绳索取心施工技术

金平长安金矿区矿体以硫化矿形式赋存于砂岩中,属于埋藏较深、倾角较陡、勘查难度较大的金矿。矿区的勘查钻孔设计范围为：方位70°～250°、倾角30°～75°、孔深100～800 m。针对该矿区地层呈现硬、碎、漏复杂情况,钻孔设计倾角大、孔斜要求高等特点,采用了新型设备（XDJ4型全液压岩心钻机）钻孔及低粘、低密度、润滑性好的冲洗液护壁方法,采取“控制钻机安装”、“减速法”或“小径导向增压纠斜法”等措施进行控斜及纠斜。有效地解决了易斜、易漏等斜孔施工问题,保质保量按期完成了施工任务,取得了很好的经济和社会效益。本文总结了该矿区大倾角钻孔施工中的部分经验和存在问题,为同类工程施工提供了较好的参考。     

《水文地质工程地质》1983年总目录

第一期盐池河磷矿山体崩塌破坏机制的研究播家口水库坝基地应力测量和断层稳定性的探讨关于工程地震工作中地震微区划的工程地质法城市烈度小区划工作的原则和方法热水岩溶与热水成矿初探”··“”·“··““·“·“·”·“·”·“二气朱庄水库库区温泉的引流”··”“·“··““·“·“···”·”··.’,“.数值模拟··试验研究··问题讨论··技术方法·溶质运移问题的有限元解法及其在地下水水质改良中的应用关于过滤器有效长度问题讨论”·“·“·“·“·”一‘”’”‘·’“’“’“厚层状细颗粒含水层中钻孔涌水量…     

护壁防塌泥浆在贵州晴隆沙子煤矿ZK209号孔中的应用

结合以往深孔泥浆的使用经验和理论知识,针对钻孔的护壁防塌问题,配制了2种护壁防塌泥浆,分别为广谱—沥青护壁防塌泥浆和聚丙烯腈胺盐—广谱—植物胶护壁防塌泥浆。经过多个钻孔检验,2种泥浆具有良好的使用性能,具有低失水性、强抑制性、造壁好、稳定性高等特点。以贵州省晴隆县沙子煤矿ZK209号钻孔为例介绍了2种护壁防塌泥浆的应用效果。     

汶川地震断裂带科学钻探项目WFSD-4孔套管护壁技术

护壁技术是解决复杂地层钻探难题的关键技术之一。介绍了一些特殊的套管护壁技术在WFSD-4号孔钻探中的应用情况,包括在小间隙条件下下大直径套管技术、复杂钻孔活动套管护壁取心技术和用于强缩径地层的两阶段下套管固井技术等。     

有机泥浆理化特性研究及其工程应用

分析了普通无机泥浆护壁机理,提出了钻孔护壁有机泥浆新概念,并通过室内对比试验研究了桩基钻孔护壁有机泥浆的物理性能与HPAM加入量的相关关系以及HPAM的降解过程,并将有机泥浆应用于成都某卵石地层钻孔灌注桩施工。通过室内试验与实际工程应用,综合分析了不同黏粒含量有机泥浆的优缺点,提出了适用于钻孔护壁的有机泥浆配比,并对有机泥浆的降解和环保做了深入地分析,得出有机泥浆是可降解的结论,为钻孔灌注桩护壁施工提供了新的途径。     

泥浆与桩侧摩阻力关系的工程实例浅析

本文通过工程实例，围绕提高桩的承载力阐明了钻孔灌注桩中，泥浆护壁对桩侧摩阻力的影响，为合理控制泥浆在灌注桩工程中的作用有很大的现实意义。     

全套管护壁与泥浆护壁灌注桩成孔效益比较

通过对 2幢相邻高层建筑物桩基础的比较分析 ,证明全套管护壁成孔比传统的泥浆护壁成孔大口径钻孔灌注桩在承载力、钻孔质量、经济效益等方面具有明显的优势 ,在实际工程中值得大力推广。     

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