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喷锚网支护基坑监测及变形特性分析 总被引：5，自引：0，他引：5
喷锚网支护在6.0 m以内基坑施工中大量采用,但此类基坑的塌滑事故也时有发生。结合武汉市汉口地区一喷锚网支护基坑的成功监测实例,分析了喷锚网支护土质基坑边坡的变形特性,得出的一些有益的结论可供同类工程作参考。 相似文献
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基坑支护工程在我国城市化建设过程中具有重要的作用,一些新型支护形式的出现极大丰富了基坑支护的多样性。本文以衡水市现场基坑支护实验工程为背景,工程将装配式可回收支护结构和桩锚支护结构作为研究对象,通过室内土工试验数据确定本构模型参数,利用有限元软件PLAXIS3D建立三维有限元模型,模拟基坑开挖和支护的全过程,并分析基坑土体和支护结构的受力、变形特征。对比相同土体和开挖条件下装配式可回收支护结构和桩锚支护结构的稳定性,结果表明：装配式可回收深基坑支护形式能更好地控制土体隆起变形,更利于限制深层土体的位移,也可以更好地控制坑顶水平位移。装配式支护结构施工简单速度快,且能回收利用,符合我国绿色建筑理念。 相似文献
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以桂林漓江饭店地下室的基坑边坡喷锚网支护工程为例,介绍了喷锚网基坑支护法设计方案的选择及支护体系的稳定性验算.并结合该工程实际阐述了高压喷射灌浆止水技术在卵石层中应用时应注意的问题. 相似文献
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桩锚支护结构在基坑和边坡围护工程中有着广泛的应用,设计阶段对支护结构的水平变形作出准确预测意义重大。根据国内多地基坑工程围护墙变形实测结果,建立桩锚支护结构水平位移的计算模型和计算假定,计算基坑围护墙在各外力作用下的变形,利用弹性叠加法得出桩锚支护结构围护墙深层水平位移表达式,联立锚杆刚度方程求解出其中的参数,最终得到水平位移的简化计算结果。该简化算法适用于围护墙底变形较小的桩锚支护结构计算,通过温州某基坑工程实例对比,围护墙变形计算结果与实测数据较为吻合,验证了该简化算法的适用性。 相似文献
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土钉桩锚组合支护结构型式是近年来适用于城市密集空间的基坑边坡支护工程。土钉桩锚组合支护结构型式随基坑的开挖及稳定后的变形规律尚需探讨研究,对于该组合支护体系下的支护结构及基坑变形的研究离不开具体的基坑工程案例。针对参与的北京市平谷区一万德福广场B43项目的土钉桩锚组合支护结构型式下的基坑工程,采用有限差分软件FLAC~(3D)对该基坑的1—1剖面进行模拟分析。通过FLAC~(3D)模拟分析的结果与实测的基坑测斜仪监测的深层水平位移相比较,分析得出:土钉-桩锚组合支护结构型式下,桩锚部分比上部土钉墙位移要大,桩锚部分的位移明显随着开挖的进行增大,且对桩本身而言桩的位移呈现中后段位移较大,两端位移较小的形状分布,开挖上部土钉墙部分,会发生基坑隆起现象。数值模拟的土钉桩锚支护结构型式下基坑变形与实测的支护结构变形结果相吻合。 相似文献
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随着城市建设的飞速发展,高层建筑日益增多,随之出现了大量超大、超深基坑,复杂的工程地质条件与周边建筑环境,给基坑支护工程带来了很多难题,单一的基坑支护体系往往已无法满足基坑稳定性要求。以北京市某基坑工程为例,介绍了一种新型组合支护体系——灌注桩-钢管桩复合土钉墙,通过与桩锚支护体系的对比研究,得出该组合支护体系在深基坑支护工程中的优越性。利用Midas GTS有限元分析软件,对基坑开挖过程进行模拟研究,对比分析了支护结构位移变形、基坑周边道路沉降等数值模拟结果与现场监测数据,结果表明：该组合支护体系对增强结构稳定性、控制边坡位移变形、减小土方开挖过程中对周边建筑环境的影响等方面具有良好作用。 相似文献
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郝腾飞何林城 《地质灾害与环境保护》2023,(3):85-87
软土具有透水性差、压缩性高、强度低和灵敏度高等诸多不良特性。深层软土发育地区基坑支护的难度往往较大,常面临稳定性差、变形位移量大、经济成本高等问题。因此针对不同基坑支护工程的特点,灵活采用恰当的支护措施对提高支护工程的稳定性和对基坑变形位移量的控制十分重要。本文以南方湖相沉积地区某城市深层软土基坑支护工程为例,针对该工程的特点对基坑支护变形位移量的控制方案进行了有益的尝试,并取得了良好的效果。 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