液动冲击器与液压凿岩机的比较与启示

通过时液动冲击器与液压凿岩机的比较，提出了两点看法：（１）液压凿岩机的大液压小流量及高的能量利用系数，对液动冲击器的研制有借鉴作用；（２）水的液体弹簧性质对提高液动冲击器的工作性能具有重要作用。     

液动冲击回转钻探技术的应用

由于水文钻探口径较大、地层复杂、孔径变化乡及工程质量要求高等难点，如何在水文钻探中应用液动冲击器，是一个亟待研究解决的问题。经过充分调研，我们选用了地矿部勘探技术研究所研制的YS-108型液动冲击器，并以其为基础开展了一定工作，取得了一定效果。     

增大液动射流式冲击器单次冲击功的试验研究

:试验结果发现 ,当行程加大时 ,获得较高的冲锤末速度 (5 .43m/s) ,单次冲击功 34 6 .45J。当活塞运动所需瞬时流量已大大超过了水泵供水的供给量时 ,冲击器仍能稳定地工作 ,这体现了射流冲击器作为一开放的系统所特有的流量可自动补偿的优点。射流冲击器对负载的适应能力较高 ,且在大行程条件下 ,增加锤重可较大幅度地提高单次冲击功。     

液动冲击器阀程对时效的影响

液动冲击器的阀程，反映了冲频的高低及冲击功的大小，它必定对时效产生重要影响。但长期以来，人们对此重视不够，致使冲击器的使用效果有时不佳。为弄清阀程对时效的影响，以及阀程和钻进参数的影响，在花岗岩地层进行了对比试验，试验结果表明，阀程对时效的影响不可忽视。试验情况如下。     

液动冲击器的性能分析

根据我们研制工作中的体会和有关文献资料介绍，对几种主要型式的液动冲击器测试结果进行初步分析对比，供参考。一、液动冲击器性能参数的测定冲击器各种性能参数的正确测定，对于研究和改进冲击器结构设计，提高冲击器的性能，对冲击器的应用以及研究冲锤和阀的运动规律等，可提供出有效的数据。测定冲击功多通过测定冲锤冲击时的速度（即末     

应力波法测试液动冲击器性能参数的微型计算机系统

本文详细介绍了用应力波法测试液动冲击器性能参数的微机系统。该系统根据国际标准设计,具有方法先进,设备简单,采样速度快及计算准确等特点。使用该系统,可以很方便地测量冲击器的能量、频率、流量等重要指标。它提供了研究和改进液动冲击器的有效方法,进一步研究将会得知不同冲击器破碎岩石所需的能量。该系统首次在地质系统应用。     

射流元件损坏机理试验研究及分析

液动射流式冲击器在高压釜内进行模拟试验时发现其工作性能良好，展现了其良好的应用前景。而在石油钻井、大陆科学深钻等深孔钻进中应用液动射流式冲击器发现，射流元件寿命较低。故有必要对其破坏机理进行研究。在实验中采用对比的方法，发现在大泵量情况下射流元件工作室内出现水射流反射及脉冲现象。射流元件破坏主要由脉冲AWJ切割所造成。液动射流式冲击器用于深孔钻进时射流元件有必要对元件尺寸进行改进。     

液动射流式冲击器性能参数影响规律的研究

本文根据计算与模拟实验资料,分析了液动射流式冲击器的泵量、泵压、冲锤质量、冲击行程等,对冲击器性能参数的影响规律、电算模拟数据绘制了相应的影响规律曲线,其结果与室内模拟实验的结果吻合,为冲击器的设计与使用提供了依据。      

双作用液动冲击器仿真电算数学模型

分析了双作用液动贯通式冲击器闭阀加速运动、自由行程和回程各阶段的受力情况，建立了相应的仿真电算数学模型。     

铀矿科学深钻液动冲击器射吸结构仿真分析

液动冲击器是铀矿科学深钻采用的关键技术,采用固定射吸单元结构的液动冲击器可降低启动流量,稳定冲击频率。为探究固定射吸单元结构对冲锤抬升的作用机理,采用FLUENT软件对冲锤射吸结构流场进行了模拟仿真,分析了喷嘴射流长度和冲锤下腔压强变化,优选了射流卷吸结构参数。结果表明:冲锤射吸结构可提高冲锤上下腔压强差,降低冲击器的启动工作流量;喷嘴结构影响有效射流长度,建议喷嘴出口圆柱长度取值范围为5～10 mm,喷嘴收敛角取值范围为22°～23°,收敛段长度范围为40～60 mm;承喷距离和承喷喉管的增大,均可造成冲锤下腔压强减小,建议当喷嘴直径为10 mm时,承喷距离在12～14 mm之间,承喷喉管直径在16～17 mm为宜。分析结果可为优化绳索取心液动冲击器性能和改进结构设计提供参考。     

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.     

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     

OCEANOGRAPHY & MARINE GEOLOGY

正20140582 Fang Xisheng(Key Lab.of Marine Sedimentology and Environmental Geology,First Institute of Oceanography,State Oceanic Administration,Qingdao 266061,China);Shi Xuefa Mineralogy of Surface Sediment in the Eastern Area off the Ryukyu Islands and Its Geological Significance(Marine Geology Quaternary Geology,ISSN0256-1492,CN37     

ENVIRONMENTAL GEOLOGY

正20141810 Bian Yumei(Geological Environmental Monitoring Center of Liaoning Province,Shenyang 110032,China);Zhang Jing Zoning Haicheng,Liaoning Province,by GeoHazard Risk and Geo-Hazard Assessment(Journal of Geological Hazards and Environment Preservation,ISSN1006-4362,CN51-1467/P,24(3),2013,p.5-9,2 illus.,tables,refs.)