共查询到20条相似文献，搜索用时 109 毫秒
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地热井花岗岩地层钻进提速技术研究与应用进展北大核心CSCD 总被引：1，自引：0，他引：1
地热资源是一种非碳基清洁能源,开发地热资源可为实现碳中和提供有力支撑。随着地热资源勘查开发进度的不断加快,花岗岩地层的钻遇率不断提高。花岗岩地层岩石硬度高、可钻性差,钻进难度大,开展花岗岩地层钻进提速技术及应用研究对促进地热资源开发利用有重要意义。本文系统梳理了国内外花岗岩地层钻进提速技术,分别介绍了螺杆马达、涡轮钻具、蓄能式提速工具、液动冲击器、气动潜孔锤等井下提速工具的特点和研究进展,结合钻探工程应用实践对每种提速钻进工具的应用情况进行了分析,针对不同工程地质特点总结提出了提速技术优选建议。对于常规地热井或温度小于150℃的花岗岩地层,宜采用螺杆马达配合牙轮钻头复合钻进技术;对于不含水或出水量较小的花岗岩地层,宜采用气动潜孔锤钻进提速技术;对于温度高于150℃或硬度高、研磨性强的花岗岩地层,采用涡轮钻具复合钻进技术提速效果更为明显。 相似文献
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射流式液动锤回转冲击孕镶金刚石钻头钻进的实践与分析 总被引：2，自引：0，他引：2
金刚石本身力学性质、金刚石钻头结构特点及射流式液动锤冲击力特点决定了射流式液动锤带金刚石钻头进行冲击回转钻进是可行的。经射流式液动锤在科学钻探主孔先导孔中的应用实践，证明了由于液动锤冲击动载作用钻头底唇面与岩面微量问隙有规律地变化，改善钻头金刚石颗粒受力状况、碎岩状态，提高钻头金刚石颗粒切入深度，改善胎体磨损状况、钻头冷却，成倍地提高了榴辉岩、片麻岩等坚硬地层中钻进回次进尺、机械钻速及钻头平均寿命。 相似文献
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油气勘探钻井用液动射流式冲击器的研究与应用 总被引：20，自引：0，他引：20
冲击回转钻进技术是当前解决硬岩进难题最有效的方法之一,将液动冲击回转钻进技术成功地推广应用于油气田勘探钻井中,预期可使硬岩平均钻进效率提高３０％－５０％,成本下降１５％－２０％。笔者就液动射流式冲击器应用于石油钻井的可行性和意义进行了较详细的分析论证,对所设计的石油钻井用液动射流式冲击器的结构和工作原理进行了说明,最后总结了生产性试验中存在的问题,提出了进一步改进的方案。 相似文献
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由长春地质学院和无锡钻探工具厂共同研制成功的SC—150型射流式液动冲击器,于1991年5月上旬在长春市通过部级鉴定。液动射流式冲击器是用射流元件控制冲击器的一种新型钻具。它以钻进冲洗液作工作介质,经过一个双稳射流元件,使钻具的活塞冲锤产生冲击,传至岩芯管和钻头,使钻具的纯回转钻进变为冲击回转钻进。该钻具的特点是:钻进效率高,比普通回转钻进小时效率提高210％,回次进尺和合班进尺分别提 相似文献
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小秦岭复杂地层液动锤绳索取心钻探试验研究 总被引：2，自引：0，他引：2
小秦岭地区是我国主要的矿产资源地,属于严重的破、碎、硬、漏等复杂地层,特别是岩石结构致密、颗粒细、研磨性较弱的坚硬地层,采用传统回转钻进工艺时,钻头经常出现"打滑"现象,从而导致钻头寿命低、钻探效率低、事故率高、钻探成本高等问题。针对这些问题并结合生产,本文选择了3处典型复杂地层进行了液动潜孔锤+绳索取心"二合一"和传统金刚石绳索取心钻探试验。试验结果表明:与传统金刚石绳索取心钻进工艺相比,液动锤平均回次进尺可提高44%,机械钻速提高21.34%~30.3%,平均综合钻探成本降低了21%~28%,其中钻头费用可降低66.5%。同时,由于碎岩方式的改变,液动潜孔锤钻探具有钻孔防斜效果好、事故率低、钻头使用寿命长等特点。 相似文献
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为了提高内蒙古意1井3000 m以深下部井段机械钻速,采用了射流冲击器旋冲钻井提速技术。根据地层岩性特点,通过冲击器台架性能测试,优选出了冲击器的冲击功及冲击频率,确定了旋冲钻井参数。射流冲击器配合牙轮钻头应用井段为3675～3817 m,通过合理确定水力参数及冲击器的性能参数,取得了预期的提速效果,达到了提速增效的目的。冲击器纯钻共计185 h,总进尺142 m,采用旋冲钻井技术,在相同地层及钻头条件下,旋冲钻井2趟钻进进尺较以前转盘钻进4趟钻进进尺多10 m,提高机械钻速达42％,为白音查干区块钻井提供了一项新的技术手段。 相似文献
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射流元件损坏机理试验研究及分析 总被引：13，自引：0，他引：13
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。 相似文献
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Emily Keeble David I. Whiteside Michael J. Benton 《Proceedings of the Geologists' Association. Geologists' Association》2018,129(2):99-119
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
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The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts 总被引：4，自引：0，他引：4
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
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Muriel Rocher Stéphane Baize Stéphane Jaillet Edward Marc Cushing Yannick Lozac&#x;h Francis Lemeille 《Comptes Rendus Geoscience》2003,335(8):701-708
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
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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
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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
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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
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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
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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
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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