共查询到20条相似文献，搜索用时 453 毫秒
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高压旋喷桩主要适用于淤泥质土、黏性土、粉土、砂土、黄土和碎石土等地层，在卵砾石地层或动水条件下的应用较少。我国某露天矿在施工旋喷桩止水帷幕的过程中，采用RJP工法进行帷幕施工，成功将高压旋喷注浆技术应用于卵砾石含水层中，通过试桩和筛分试验将卵砾石层特征对桩径大小的影响进行了分析研究，结果表明，RJP工法在卵砾石含水层中成桩效果良好、质量可靠，其桩径大小与卵砾石颗粒大小及含砂量有关。围井试验结果显示，高压旋喷桩帷幕墙完整，止水效果显著。研究成果表明高压旋喷注浆技术可在卵砾石含水层的加固和止水领域进行推广应用。 相似文献
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新泰盛世佳苑基坑工程中,采用施工简便的单层锚索排桩结构围护边坡,高压摆喷隔水帷幕阻水,基坑内集水明排降水方案,造价低廉的锚索通过对其施加合理的预应力可大大减小基坑变形,其效果不亚于施工复杂、造价昂贵的内支撑。该支护技术的成功应用为新泰市今后的深基坑工程在设计、施工等诸多方面积累了许多宝贵的经验。 相似文献
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介绍十天高速公路嘉陵江1#大桥水中墩基础施工中采用高压旋喷桩作为闭水帷幕的方案设计、施工及施工效果。旋喷桩止水帷幕有效地解决了基坑涌水,保证了后续施工的无水作业,对同类基坑防水施工具有一定的参考和借鉴价值。 相似文献
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太园泵站反虹涵工程的地基为深厚,强透水性的中粗砂,砂卵石层。基坑开挖较深,基坑防渗采用高压喷射灌浆构造防渗板墙技术。实践证明,高压喷射防渗板墙渗透系数Ｋ＝１＊１０＾－６ｃｍ／ｓ,基坑透水较少,高喷墙的防渗效果显著。 相似文献
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大粒径卵砾石地层影响半径大、渗透系数高、地下水补给量大,若采用降水方法进行地下水控制,将导致严重的水资源浪费;而该类地层可适用的帷幕止水方法种类较少,且不同止水方案对工期、造价影响较大。以北京地区某深基坑工程实例为分析条件,提出了多管同步注浆止水帷幕方案,通过开展工程场区内的现场注浆模型试验,系统研究了多管同步注浆的施工工艺、注浆材料及施工参数等关键技术指标。通过现场测定及室内分析,大粒径卵砾石地层袖阀管同步注浆扩散半径大于0. 5 m,注浆固结体渗透系数约5, 2×10~(-6) cm/s,可有效降低卵砾石地层的渗透性、极大程度减少基坑抽排水量,是一种可靠的深基坑工程止水辅助施工技术,可为类似地层条件下深基坑工程地下水控制设计及施工提供参考。 相似文献
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以北京市通州区运河核心区某项目为实例,探讨紧邻地铁隧道及车站深基坑设计的技术难点和施工过程的关键控制点.项目基坑深度12.1～22.1 m,基坑周边环境复杂,基坑东侧临近地铁北京6号线新华大街站与其区间隧道,距离地铁车站附属结构最近距离为6 m,距离6号线隧道最近距离为16.619 m,由于地铁对位移要求较高,须保证基坑支护与止水不对地铁造成扰动,因此应加强基坑支护变形控制,确保地铁能够安全运营.综合考虑地层岩性及周边环境情况,基坑支护采用挡土墙(土钉墙)+桩锚支护方案,地下水控制采用三重管高压旋喷帷幕止水与搅喷桩止水帷幕结合坑内疏干井的止水方案.项目实施过程中对周边建筑物及基坑进行了全过程监测,监测结果表明,在此类复杂环境下采用桩锚支护+三重管高压旋喷帷幕止水与搅喷桩止水帷幕+坑内疏干井的方案是安全且经济合理的.施工工艺及施工工序合理,保证了基坑开挖过程中已有地铁的安全. 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