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增加松软煤层穿层孔煤孔段的长度可以提高穿层孔单孔瓦斯抽采效果,利用挠性钻具组合施工煤孔段可以达到延长煤孔段的目的。本文建立了挠性钻具施工的力学模型,研究了强造斜的运动学特征,并提出了造斜过程的运动学曲线;根据力学模型及运动学特征,研究了强造斜钻进工艺,尽可能增加钻孔煤层钻遇率。 相似文献
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针对我国松软低透气性煤层瓦斯抽采难题,提出了采用跟管钻进和水力压裂技术提高松软煤层钻孔深度和煤层透气性,通过布孔设计、应力分析论证了该方法的施工可行性,讨论了该方法的施工步骤。该技术有望成为解决松软低透气性煤层瓦斯抽采难题的新工艺方法。 相似文献
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随钻测量梳状定向钻进技术目前主要应用于煤矿瓦斯防治、地质异常体探测和探放水等领域。但该技术还未与水力压裂增透强化抽采技术相结合应用于煤层瓦斯防治领域,由于水力压裂增透强化抽采技术对钻孔特殊要求,相应钻探装备、钻孔设计和钻进成孔工艺均需要进行研究突破。本次研究成果融合了井下梳状定向长钻孔瓦斯抽采技术及水力压裂增透强化抽采技术的优点,形成了一套适合分段水力压裂梳状定向钻孔施工设备及工艺流程,能够满足对松软煤层瓦斯远距离与区域增透技术的需求,解决松软煤层透气性差、瓦斯抽采孔成孔性差、抽采距离短、抽采区域小等难题。 相似文献
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我国的地质条件和煤层特征差异大,复杂地层中构造煤发育,瓦斯含量高,地应力大,煤层破碎松软,易发生塑性流变。采用套管钻进技术替代传统的常规钻杆进行钻孔瓦斯抽采,可提高工作效率,防止卡钻、塌孔等事故的发生,提高瓦斯抽采的效率,并可以不起钻取出钻头等孔底钻具组合下筛管,解决在井下复杂地层中钻孔瓦斯抽采的难题。介绍了套管强度及孔底组合钻具结构,探讨了套管钻进技术在煤矿复杂地层中的应用前景。 相似文献
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松软煤层钻孔在钻进及抽采瓦斯过程中,容易发生钻孔形变、缩径、坍塌甚至堵孔等工程问题,造成瓦斯钻孔成孔率低、密封性差、服务时间短及瓦斯抽采阻力大等抽采问题。针对上述技术难题,基于松软煤层的构造演化过程,分析了自重应力、构造应力、采动应力及瓦斯应力等因素对松软煤层瓦斯钻孔稳定性的影响,得出了松软煤层钻孔的多应力耦合作用失稳机制。同时,针对松软煤层瓦斯钻孔失稳规律,提出以护孔为基础,自适应动态密封为关键的"护-封"一体化松软煤层瓦斯钻孔密封技术。工程试验结果表明,该技术可使单孔瓦斯抽采体积分数增加至90%以上,单孔瓦斯体积分数提高2~3倍,且抽采浓度稳定。 相似文献
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针对碎软煤层顺层钻孔成孔深度浅、成孔率低、存在抽采盲区等突出问题,基于贵州省青龙煤矿煤层及顶底板岩层赋存特征,提出利用底板梳状钻孔进行碎软煤层长距离、区域瓦斯抽采与治理。首先分析了底板梳状钻孔的施工工艺原理及技术优势所在,从布孔层位、分支点位和钻孔间距的选择等方面总结了底板梳状钻孔的设计原则。通过钻进装备的优选、钻进工艺参数和钻具组合的优化,成功穿越破碎煤岩层孔段,并实现了127 mm套管全程护孔下放,在21605底抽巷施工完成了多组底板梳状定向钻孔。瓦斯抽采效果表明：底板梳状定向钻孔瓦斯抽采流量大、浓度高、衰减速度慢,单孔瓦斯抽采浓度60%～85%、抽采纯量08～25 m3/min,实现了碎软煤层瓦斯高效抽采。为碎软煤层矿井区域瓦斯抽采与治理提供了重要的借鉴。 相似文献
7.
中风压钻进在煤矿井下的应用 总被引：5，自引：0，他引：5
根据煤矿井下沿煤层瓦斯抽采(放)钻孔中风压压风钻进工艺及设备的发展情况,介绍了中风压钻进工艺和配套设备的选择、研制以及在丁集矿和成庄矿的钻进工艺试验,证明在松软突出煤层的沿煤层瓦斯抽采(放)孔钻进施工中,中风压钻进工艺较为理想、是值得推广的钻进工艺。 相似文献
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以穿层钻孔方式进行松软煤层瓦斯预抽采极大地克服了松软煤层瓦斯治理难的问题,然而部分矿区煤层顶（底）板岩石坚硬,影响了钻孔施工效率。结合地质岩心钻探的优势,将液动潜孔锤与高强PDC钻头结合应用于煤矿井下穿层瓦斯抽采孔施工中。淮南潘一煤矿现场试验表明,该工艺方法较传统回转钻进方法,钻进效率提高了83%,钻头进尺寿命提高近5倍,具有良好的经济性能。采用清水为冲洗介质,无粉尘污染,噪声污染小,较为适合空间狭小的煤矿井下巷道施工。 相似文献
11.
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
13.
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