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1.
全金属容积式动力钻具是当前深部钻探研究的热点之一,其在井下工作受到金属摩擦、高速冲蚀、高温腐蚀、拉伸、扭转、振动等复杂工况影响,对制造材料提出了较高的要求。本文首先调研了当前井下机具马达部件定转子的常见选材成分、力学特性和加工性能;随后介绍了超深井对全金属动力钻具马达部件的要求并分析了现存难点;初步优选了定子、转子制造材料,并考虑转子部件上采用新型铜基-铁基材料复合结构;调研分析了其加工处理技术发展现状;提出了加工建议。为全金属动力钻具马达部件的设计和寿命研究提供了参考依据。  相似文献   

2.
螺杆钻具作为一种容积式动力钻具,具有良好的输出硬特性,是当前应用最广泛的井下动力钻具之一。螺杆钻具的耐温性是其研究的热点所在,可扩大其应用范围和延长工作寿命,在深部高温钻探领域,具有良好的发展前景。本文在阐明螺杆钻具的基本原理和特性基础上,调研分析了常规螺杆钻具的发展现状,重点调研分析了美国全金属螺杆钻具的研发现状与国内全金属螺杆钻具的发展,提出了全金属螺杆钻具的关键技术,为国内开展这项前沿钻具技术的研发提供参考。  相似文献   

3.
曹彦伟  李谦 《探矿工程》2021,48(11):84-93
钻进时的振动会引起钻具疲劳失效和损坏,为提高井下钻具的稳定性,本文设计了依靠行星齿轮系驱动内外钻头同轴双向回转的钻具结构。通过对其核心的齿轮、密封、轴承等部件进行的强度校核,证明该结构的设计强度能够满足正常的使用工况。同时基于数值模拟对该结构的振动效果进行了验证,将钻进时钻头与岩石的相互作用简化为简谐荷载,对双向回转钻具整体结构进行谐响应分析。结果显示,相比于普通单向回转钻进结构,同等条件下双向回转的钻具结构能够有效抑制扭转振动。  相似文献   

4.
螺杆钻具是由多个可以旋转的转轴通过万向联轴器连接成的一个轴系,主要用来传递转矩从而带动钻头运动。但是在安装或者在万向联轴器自身磨损消耗下,钻具会出现轴线上的不对中,进而引发一系列故障,比如螺杆钻具的螺杆马达转子联轴器偏移、轴承移动、转轴发生形变、油膜失稳等,导致机器发生振动并造成一系列的危害。因此,在实验室条件下,研究井下动力钻具不对中的故障产生机理,掌握不同故障的特征,并及时进行故障诊断,对减小或避免由于转子联轴器不对中而产生的故障具有十分重要的意义。本文借助于DHRMT双跨转子台高度模拟井下的钻具故障,设置转子不对中的不同故障类型,通过实验获得钻具转子不对中故障造成的振动特征,为井下动力钻具设计及改进提供参考依据。  相似文献   

5.
井下动力钻具微钻试验装置是为研制新型动力钻具提供试验条件的关键装备,该装备用于原理样机的试验测试,可降低试验成本并缩短研发周期,试验测试结果可为全尺寸物理样机的制造提供参考。本文依据井下动力钻具的工作特点和钻具试验装置测试原理,设计了一套井下动力钻具微钻试验装置,该试验装置区别于常规和传统的微钻实验台,其采用数控闭环控制钻井液动力循环和钻压,实现了水力驱动与钻压给进的精确控制,并验证了井下动力钻具微钻试验装置的可行性,为水力驱动的钻具样机试验研究提供了平台。  相似文献   

6.
井下动力钻具用轴承承受着冲击、摩擦、腐蚀等恶劣工况,其可靠性和寿命对保障钻进的顺利进行至关重要,是井下钻具的关键部件之一。本文对井下动力钻具常用的止推轴承、扶正轴承进行了详细调研,分别对金属滚动轴承、滑动止推轴承和扶正轴承等发展现状、主要特点、发展趋势等进行深入分析,并指出了井下动力轴承的发展与改进方向,可为其选用提供参考。  相似文献   

7.
本文重要介绍了转盘(顶驱)+螺杆钻具复合钻进工艺在干热岩钻井中的应用。为进一步提高干热岩钻井施工效率和减少孔内事故,在青海共和干热岩GR1井进行了转盘+螺杆钻具复合钻进应用,根据现场高温井况下螺杆钻具的工作特性,改进优选了螺杆钻具的耐高温橡胶和转子定子的配合间隙,是螺杆钻具复合钻进工艺在深孔高温干热岩钻孔(孔深3705m,孔底温度236℃)施工的首次成功尝试,并取得了良好效果,经受住了硬岩和高温的考验,为进一步改进螺杆钻具在高温井况下的应用提供了宝贵的现场施工经验,也将为我国干热岩科学钻探与深部地热资源勘探提供新的技术支撑。  相似文献   

8.
为评价雪峰古陆周缘页岩含气性,2019年在沅麻盆地施工了页岩气地质调查井湘桃地1井,完钻井深1850.88 m,全井取心,平均岩心采取率97.24%。施工中应用XY-8型钻机,采用三开井身结构,配合录井及测井技术,并优选钻具组合、钻头、钻进参数、钻井液性能。因牛蹄塘组碳质泥岩失稳掉块及钻探工艺调整不及时发生了卡钻、埋钻、钻具折断等井下复杂,采取螺杆马达侧钻绕障予以解决,侧钻后同径继续钻进806.87 m至完钻。该井的顺利完钻和井下复杂处理方法为同类地区地质调查井施工提供了可借鉴的经验。  相似文献   

9.
作为智能化钻探的重要组成部分,钻具系统的智能化对煤矿井下钻探的智能化发展起着至关重要的作用。为深入探究智能化钻具的发展方向,结合石油天然气行业发展经验,从定向钻具、随钻测量系统以及智能化钻杆、钻头等方面系统梳理了煤矿井下智能化钻探配套钻具的研究成果与技术特点,总结了存在的不足。指出目前煤矿井下智能化钻探定向钻具多以螺杆马达为主,主要研究集中于螺杆马达的线形设计、定子橡胶抗疲劳研究与不同工艺个性化定制,旋转导向钻具的开发与石油天然气行业存在较大差距,仅处于起步阶段;随钻测量系统可监测参数较少,监测的数据以轨迹参数为主,逐步加入了伽马地层识别,数据传输以有线与泥浆脉冲方式为主,存在数据容量小、传输效率低的问题,无线电磁波方式传输距离较短,仅能满足500 m以内钻孔;智能化钻杆研究主要为通缆钻杆的优化与改进,智能化钻头的研究尚未开展。为实现煤矿井下智能化钻探,提出开展以旋转导向为主,多种定向钻具综合运用的钻具定向系统研究;随钻监测系统应集成瓦斯监测、地下水探测及地应力感知煤矿钻进特种需求的功能,并配合多种传输方式并存的随钻测量系统研究以适配不同钻进工艺,同时提升传输速率,实现信息高速双向传输...  相似文献   

10.
和鹏飞  孔志刚 《探矿工程》2013,40(11):45-48,51
通过对PowerDriveXceed指向式旋转导向钻具外部结构、内部组成以及工作原理的简要说明,对该钻具和泥浆马达钻具在安全性、时效性2方面进行了对比。最后通过PowerDriveXceed指向式旋转导向钻具在渤海某油田的应用,进行了其与泥浆马达钻具在轨迹控制、机械钻速以及近钻头连续井斜方位的对比分析,给出了渤海在水平井常用的泥浆马达钻具和PowerDriveXceed指向式旋转导向钻具的使用模式,为其它地区使用该工具提供了参考经验。  相似文献   

11.
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.  相似文献   

12.
Robert L. Linnen   《Lithos》2005,80(1-4):267-280
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.  相似文献   

13.
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).  相似文献   

14.
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  相似文献   

15.
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),  相似文献   

16.
17.
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-  相似文献   

18.
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-  相似文献   

19.
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.)  相似文献   

20.
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  相似文献   

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