绳索取心钻具内管总成打捞器

我公司多年采用绳索取心钻具,台月效率、纯钻台时和钻孔质量均有所提高。但往往由于操作技术不当等原因,致使发生孔内事故。尤其是发生烧钻事故后,使内管总成打捞不上来,迫不得已移孔重打或套扫,因而耽误时间,增加成本。     

嵩县槐树坪大型金矿复杂地层泥浆及护壁堵漏技术

嵩县槐树坪金矿区域地质构造复杂,岩石破碎,部分岩层高岭土化,钻探施工中漏失、垮塌严重,经常发生钻孔缩径、卡钻、内管总成打捞困难等孔内事故,严重影响了钻进效率和钻孔质量。对该矿区施工所遇到的困难和需要重点解决的问题进行了分析,通过试验研究,确定采用聚合物低固相泥浆体系,并根据该矿区地层特点,确定了在不同条件下聚合物低固相泥浆的配方、配制方法、维护管理及护壁堵漏方法等,逐步在该矿区全面推广,大幅度减少了孔内事故、提高了纯钻效率和台月效率,有效地促进了该矿区的勘探进度,缩短了勘探周期,取得了显著的经济效益和社会效益。     

绳索取化特种提引接头

绳索取心钻进处理事故时用打捞器捞取内管时，由于座环碎裂或其它原因而夹住内管总成，使内管提拉不动，而打捞器又不能安全脱卡，这样在提升孔内钻具时，打捞钢丝绳则碍事。根据上述情况，我们设计了一种特种提升接头，使钻具全部提出孔外。该接头的具体结构如附图所示。     

超深涌水水平孔绳索取心钻具投送和打捞技术

为了精准查明拟建隧道沿线地质情况,通常采用水平孔绳索取心钻探技术。在超深涌水水平孔绳索取心钻进中,投放、打捞内管总成钻具和打捞器是施工中的难题。因此从研制专用水平钻机、选择大功率泥浆泵、封隔分流涌水、设计绳索取心钻具送绳器、定制专用内平绳索取心钻杆等几方面开展研究。全面分析了泥浆泵压力、钻杆内径大小、钻孔深度、钻杆的密封性、钻孔涌水量、涌水压力、孔壁间隙等因素对投送内管总成钻具和打捞器速度的影响,实现了高效、低成本、绿色钻探技术集成。经过精心组织,成功完成了千米级的大涌水水平孔绳索取心钻探施工,精准查明了隧道洞身段工程地质条件,取得了满意的技术效果,为隧道设计和施工提供了安全保障,也为超深涌水水平孔钻探提供了经验。     

S75-SF中深孔绳索取心钻具结构及应用

随着中深孔地质岩心钻探工作量的大幅增长,不仅对绳索取心钻柱提出了严格要求,对绳索取心钻具的功能和可靠性要求也越来越高。S75-SF绳索取心钻具采用了双弹卡结构,增强了悬挂机构的安全性,提高了内管总成的投放和打捞速度,减轻了孔内冲洗液压力波动,在正常钻进时可降低泥浆泵压力损失,有利于复杂地层孔壁稳定。内管总成机构与内岩心管采用插接的连接方式,拆卸方便,便于钻探施工人员采取岩心。该钻具在施工中效果良好,减轻了工人的劳动强度,提高了施工效率,可满足中深孔绳索取心钻探施工要求。     

介绍日本利根公司的绳索取心钻具

本文介绍一九七九年从日本利根公司引进的V型绳索取心钻具结构及其特点。一、概 述V型绳索取心钻具用于垂直钻孔包括HQT和NQT（T表示利根）两种尺寸（见表1），绳索取心钻具由单动双管和打捞器两部分组成。1．单动双管：由内管总成和外管总成构成（图1）：内管总成包括打捞接头①、弹卡机构②、悬挂定位装置③、调节机构④、单动装置⑤、内管⑥、岩心卡取机构⑦、报信装置⑧、缓冲装置⒄等组成；内管总成上部结构见图1所示。     

金塘大桥3号主桥墩ZK8号钻孔事故处理技术

针对金塘大桥3号主桥墩ZK8号钻孔烧钻断杆事故及事故处理不当发生的卡杆二次事故,认真分析了事故原因,制订了严密的钻具打捞方案,成功打捞了孔内钻具,为后续钻孔灌注桩的施工排除了障碍。介绍了事故状况及处理技术。     

绳索取心钻进技术在水平钻孔中应用

针对深100 m水平钻孔钻孔易倾斜和卡钻事故多发等问题,在2个工程中试验应用了绳索取心钻进技术成孔,把打捞器中的柔性钢丝绳改为硬质铁管,解决了内管总成的打捞和投放问题。并采取了一些相关技术措施,取得了良好的钻进效果,2个深100 m水平孔均没有发生过孔内卡钻或其它事故,而且钻进效率高、岩心采取率高,达到了地质勘探的目的和要求。结合工程实践,介绍了在水平孔中采用绳索取心钻进技术的技术要求和工艺措施。     

FDS-P型绳索取心钻具研制及试验研究

针对复杂地层绳索取心钻进时易出现的内管总成打捞失败问题,开展了FDS-P型绳索取心钻具研制。基于内管总成打捞失败原因分析,完成了FDS-P型绳索取心钻具设计,通过室内试验,初步验证了钻具结构设计的合理性。为进一步验证钻具性能,在贵州页岩气井开展了野外生产试验,先后完成16个回次取心钻进,累计进尺39.03 m,岩心采取率达到98%以上,其中有6个回次发生堵心,内管打捞全部成功,内管到位及堵心均得到了及时提示。实际应用结果表明,FDS-P型绳索取心钻具结构设计合理,具有良好的到位及堵心报信提示作用,内管总成打捞可靠性得到显著提升,有效提高了易堵心地层钻进效率及岩心采取质量。     

绳索取心钻杆内壁结垢成因与预防及清理装置的研发

绳索取心钻杆内壁结垢会造成钻杆腐蚀、打捞器与内管总成运行遇阻、孔壁失稳等问题,常见类型有涡区结垢、延伸结垢与渗漏结垢等。本文在分析结垢原因与影响因素的基础上,制定了冲洗液优选、钻进技术参数优化、钻孔结构与钻具组合优化等预防措施,同时,研发了泥皮清理装置,可通过供电绞车和铠装电缆将刮泥器送至孔内,主动清理钻杆内壁的吸附物或泥皮,保持钻杆内壁清洁,实现高效安全钻进。     

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