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煤矿坑道钻探装备技术在发展过程中受到诸多不利条件的限制,导致新技术发展滞后,随着我国煤矿大力推进智能化建设,给煤矿坑道钻探装备技术带来了革命性的发展机遇。通过分析了国外坑道钻探装备的技术特点和发展状况,以及国内坑道钻探装备技术的三个阶段发展,包括初级阶段的分体式钻机与稳定组合钻具轨迹控制方法,蓬勃发展阶段的履带式钻机、定向钻进装备技术及松软煤层钻进技术,新发展阶段的自动化和智能化装备技术,提出了今后我国煤矿智能化发展阶段钻探装备技术需要解决的关键问题,为推进钻探装备技术的智能化水平提高提供支撑。 相似文献
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经过近60年的发展,煤矿坑道钻探装备已经形成满足多种用途、适用于多种钻进孔深要求的多规格、多系列产品,但现有成熟钻探装备主要以全液压驱动和人工操作为主。随着我国煤矿企业在智能化方面建设的大力投入,传统全液压驱动的坑道钻探装备已无法满足当前煤矿智能化发展需要。结合坑道钻探的施工特点,分析了国外典型坑道钻探装备的技术现状和功能特点,以及存在的问题,重点针对国内坑道钻探装备不同施工需求的智能化方面的进展情况进行概述,分别介绍了常规自动化钻机、钻孔机器人、大功率自动化定向钻机、自动化防冲击钻机等方面的研究进展,提出了我国煤矿井下钻探装备智能化建设方面还需解决的关键问题,并通过分步实施方式,加快推进煤矿井下钻探装备的智能化水平。 相似文献
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从矿山坑道内直接对附近的矿体和构造进行钻探勘察,要比远距离的地表钻探经济而迅速,也比坑道探矿具有更多的优越性.但在我国的人造金刚石钻头尚未研究成功以前,其发展受到了限制.近年来,随着金刚石钻探工艺技术的推广应用,我国的坑道钻探工艺及设备也得到了快速发展. 六十年代,我国曾进口过一些坑内钻机(如苏联??-1型、瑞典X-4型、日本SA-I S型等),但均属四十年代的产品,性能不理想. 相似文献
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煤矿井下智能化钻探技术装备是煤矿智能化建设的重要组成部分,也是当前煤矿企业深入推进减人增效工作所急需的先进技术装备。系统总结了“十三五”期间我国煤矿井下智能化钻探技术装备所取得的阶段性成果,重点介绍了自动化钻机、随钻参数监测系统和旋转导向系统等关键技术装备的发展现状。全面分析了制约井下智能化钻探技术装备研发与应用的关键因素:钻机智能化水平较低、随钻探测数据类型少、多系统集成控制难。在此基础上提出深入推进数字化、网络化、智能化技术与传统坑道钻探技术结合,强化多学科融合和协同创新能力;并不断加强智能化钻探技术装备研发与应用人才的培养力度,以技术装备为支撑、以数字化平台为保障、以人才队伍建设为基础;在智能化钻机、高精度数据获取与传输技术、钻孔轨迹智能优化与控制技术、辅助关联设备集成控制技术、数字化钻进平台开展攻关,以实现煤矿井下钻孔全流程智能化施工作业。 相似文献
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介绍了螺纹插装阀的技术特点及其在煤矿坑道钻机中的发展应用情况。煤矿坑道钻机应用螺纹插装阀技术不仅可以实现复杂的液压控制系统,还能简化管路,方便整机布局。通过几个典型实例展示了螺纹插装阀在煤矿坑道钻机中的具体应用情况,验证了螺纹插装阀技术在煤矿坑道钻机液压系统中的实用性和良好的应用前景。 相似文献
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北京大安山煤矿地表只有少数钻孔控制到+550 m水平,为探明下部煤层赋存条件,提高资源储量级别,应用ZDY1000G型全液压坑道钻机、S75绳索取心钻进工艺进行了硐内深孔钻探,完成了坑道内试验钻探孔深505.17 m。随之在2012-2014年共计钻探进尺8237 m,勘探增加资源储量1877.7万t。深孔钻探技术不仅加快了对深部水平煤层的勘探,探明了深部水平煤层赋存条件。为开拓工程部署提供了可靠的地质资料,而且减少了巷探成本,提高了工程效率。本文对井下硐内深孔钻探进行了介绍。 相似文献
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煤矿井下钻探装备技术现状及展望 总被引：2，自引：0，他引：2
煤矿井下钻探装备对保障矿井安全高效生产起着至关重要的作用,经过四十多年的发展,其技术水平得到很大的提高。结合产品特点、技术类型和应用领域,总体介绍了国内外煤矿井下钻探装备的技术现状,分析了国外钻机的应用效果和存在问题,重点对国内钻机开发的历程和现状进行概述,详细论述了分体钻机、履带式钻机、电液控制钻机、胶轮自行式钻机和定向钻机5个具有代表性机型的技术现状,对产品开发思路和相关应用情况也做了必要阐述,最后分析了煤矿井下钻探装备的信息化、自动化和智能化的发展趋势。 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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Gilles Serge Odin 《Comptes Rendus Geoscience》2002,334(6):409-414
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. 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20141520 Bo Ying(Key Laboratory of Metallogeny and Mineral Assessment,MLR,Beijing 100037,China);Liu Chenglin Saline Spring Hydrochemical Characteristics and Indicators for Potassium Exploration in Southwestern and Northern Tarim Basin,Xinjiang(Acta Geoscientica Sinica,ISSN1006-3021,CN11-3474/P,34(5),2013,p.594-602,5 illus.,3 tables,28 refs.) 相似文献
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正20141243Chen Ge(Hangzhou Research Institute of Petroleum Geology,PetroChina,Hangzhou 310023,China);Si Chunsong Study on Sedimentary Numerical Simulation Method of Fan Delta Sand Body(Journal of Geology, 相似文献
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正20142599Chen Sanming(Guangxi Key Laboratory of Concealed Deposits Exploration,Guilin University of Technology,Guilin541004,China);He Yuzhou Block Model and Reserves Estimation of Panzhihua Iron Deposit Based on 3D Geological Modeling(Journal of Guilin University of Technology,ISSN1674-9057,CN45-1375/N,33(4),2013,p.610-615,9illus.,1table,15refs.) 相似文献
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正20140594 Bai Daoyuan(Hunan Institute of Geology Survey,Changsha 410016,China);Zhong Xiang Faults in the Jingzhou Basin and Their Tectonic Settings(Geotectonica et Metallogenia,ISSN1001-1552,CN44-1595/P,37(2),2013,p.173-183,6illus.,59refs.)Key words:basin evolution,tectonic setting,South China In the Upper Paleozoic and Jurassic se- 相似文献
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正20141912Cao Hui(State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)Gravitational Collapse and Folding during Orogenesis:A Comparative Study of FIA Trends and Fold Axial Plane Traces(Geology in China,ISSN1000-3657,CN11-1167/P,40(6),2013,p.1818-1828,9illus.,35refs.,with 相似文献