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1.
一般传统钻机主要由主机、操作台、泵站三大件组成,质量大,搬运不方便。ZDY4000LS型煤矿用履带式全液压坑道钻机是一种新型的钻机,结构布置合理,辅助功能齐全,它能有效地改善中小煤矿钻孔施工效率,提高钻掘产量,降低工人劳动强度。主要介绍了ZDY4000LS型煤矿用履带式全液压坑道钻机的主要技术参数、结构布局特点、液压系统及生产试验情况。试验应用表明,对于巷道较小或者有运输皮带限制的煤矿巷道,该钻机具有推广价值。  相似文献   

2.
针对我国煤矿松软突出煤层中的煤巷、高应力巷道等小断面巷道,以及皮带运输巷中钻机需频繁让道、在掘进巷道中钻机需绕前施工等通过空间狭小的复杂钻孔施工条件,结合煤矿钻孔现场施工对孔比较繁琐及搬运迁移比较困难的现状,进行了ZLY2500L型煤矿用履带式坑道钻机的研制。目前常用的整体式履带钻机存在这样的缺陷:不能将井下机动灵活、外形尺寸小、操作人员安全性高等特点高度融合,使瓦斯抽采钻孔施工效率低,钻机对复杂钻场和矿井条件适应性差。该机型结构布置合理,辅助功能齐全,它能有效地改善中小煤矿钻孔施工效率,提高钻掘产量,降低工人劳动强度, 可用于瓦斯抽采穿层钻孔、瓦斯抽采顺层钻孔和探放水以及底板注浆等钻孔施工。本文主要介绍ZLY2500L型煤矿用履带式坑道钻机的主要技术参数、结构布局特点及液压系统。经试验表明,对于中小煤矿钻孔施工具有良好的应用前景。  相似文献   

3.
GYD-20型全液压动力头工程钻机的研制   总被引:1,自引:1,他引:0       下载免费PDF全文
杨付伟  鲁建军 《探矿工程》2014,41(11):34-36
针对传统工程钻机生产制造周期长、自动化程度低、劳动强度大、施工效率低等弊端,研制了GYD-20型全液压动力头工程钻机。介绍了该钻机的结构特点及其应用于大口径基础桩孔、煤矿通风孔钻进的情况和效果。  相似文献   

4.
多功能液压桩孔钻机是一种高效率、多用途的灌注桩成孔设备,它能够快速地改变机器形态,配备长螺旋钻、短螺旋钻、筒形钻、岩石钻等钻具进行旋挖成孔,配备摆管器等钻具进行全套管护壁成孔,或者配备各种抓斗实施地下连续墙作业。介绍了多功能液压桩孔钻机的结构及特点。  相似文献   

5.
针对目前国内防渗墙、灌注桩桩孔施工及水井钻凿的主要设备CZ-22型钢绳冲击式钻机在使用过程中的一些不足之处,研制开发了CZ-1200型冲击钻机。介绍了钻机的结构特点及其在防渗墙、水井施工中的应用。  相似文献   

6.
某地基不均匀沉降的三维分析   总被引:3,自引:2,他引:3  
某地基处理原拟采用CFG复合地基。但由于地层情况复杂 ,施工难度大 ,决定采用CFG桩和人工挖孔桩进行地基处理 ,但是这种处理方案可能会引发地基不均匀沉降从而对上部结构产生不良影响 ,因此合理的的选取人工挖孔桩桩间距非常重要。通过对四种桩间距情形下地基的三维沉降分析 ,选取了合理的人工挖孔桩桩间距 ,解决了这一工程难题.  相似文献   

7.
唐爱国 《探矿工程》2015,42(10):55-58
主要为大口径基础灌注桩施工而设计的YCJF-25型全液压冲击反循环钻机具有碎岩能量大、破岩效率高、排渣速度快、能有效避免孔底岩屑的重复破碎的特点。介绍了YCJF-25型全液压冲击反循环钻机性能参数,阐明了钻机的结构特点,对比分析了钻机的施工效率。  相似文献   

8.
长螺旋钻机成孔CFG桩施T是近年来新兴的一项基础工程施工技术,在工程建设领域有着广泛的应用,尤其适用于对软土地基的处理。该技术施工噪声低,成桩速度快,效果好,得到了广大施工技术人员的青睐。CFG桩复合地基可以大大提高地基承载力,减小地基的沉降,进而满足设计要求。本文介绍了长螺旋钻机成孔CFG桩的成桩工艺流程、理论设计、质量控制措施,并以工程实例进行佐证,以期该施工技术得到更加广泛应用和发展。  相似文献   

9.
本文就法基与边坡的基础处理用钻掘设备,包括桩孔钻机、软土地基处理机、锚固钻机、微桩钻机以及连续墙成槽机等分类进行了全面的论述,并指出了国内工距、今后我国的发展方向等。文章附有表格,详细列出了世界主要厂商的系列设备产品。  相似文献   

10.
李致宗 《探矿工程》1992,(2):44-44,37
我局第二水文工程地质队在某泵站工作施工中,需要处理一批基桩孔。这些基桩孔分布在厚度为0.4—0.6m的混凝土地基上面,由于混凝土的骨料为质地坚硬的卵石及灰岩片石,钻机钻进时跳动大,曾损坏伞齿轮两付,钻头两个。同时,施工进度慢,一个口径为600mm的基桩孔从钻进到灌桩需要6—7d时间才能完成。为了提高经济效益和赶工期,我们采用控制爆破进行开孔,然后安装钻机进行施工。  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.
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.
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   

14.
15.
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   

16.
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   

17.
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   

18.
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   

19.
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   

20.
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   

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