共查询到20条相似文献，搜索用时 62 毫秒
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相邻基坑土条土压力计算方法探讨 总被引：2，自引：0，他引：2
基坑工程实践中,经常遇到相邻基坑土条土压力如何计算的问题,现行基坑规范尚没有计算方法。通过理论探索和工程实践,对前、后期的基坑支护型式进行了归类和组合,提出了相临基坑宽度的确定原则;提出了建立在库仑土压力理论基础之上的简化计算方法--叠加法,推导并给出了非黏性土和黏性土在不同坡率和地面分布有荷载条件下主动土压力系数和土压力的计算公式,并提出了临界宽度的概念和土条土压力折减系数的计算公式。利用所提出的叠加法、临界宽度的概念和土条土压力折减系数的计算公式,可以简捷地计算不同土层、不同坡率和地面荷载条件下的土条土压力合力及土压力强度。工程实践表明,该方法概念清晰、理论依据充分、计算公式简便,以此设计的基坑支护结构安全合理,可供类似基坑支护工程设计参考。 相似文献
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某商住大厦基坑支护工程设计及施工技术 总被引：1，自引：0，他引：1
概述了某商住大厦基坑支护工程设计及施工技术,由于采用密排钻孔灌注桩加预应力锚索及冠梁腰梁挡土支护、外加旋喷止水注浆孔进行桩缝止水的组合支护结构作为基坑挡土防渗支护体系,基坑经受特大暴风雨没有发生任何问题,为类似工程的设计与施工提供了一种既安全可靠又经济实用的参考方案,与地下连续墙相比,经济效益可观。 相似文献
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基床系数室内测试方法研究 总被引：1，自引：0，他引：1
《岩土工程技术》2017,(6)
通过对宁波轨道交通基坑开挖范围内典型软土层开展固结试验及三轴试验,得到了各层地基土的基床系数,并将试验值与规范经验值进行对比、分析后,提出了适用于宁波土层的室内试验基床系数修正公式,经修正后得到了各地基土层较为合理的标准基床系数,验证了室内试验测定地基土基床系数的有效性,解决了批量测定地基土基床系数的问题,可为工程设计和施工所使用。 相似文献
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鉴于基坑支护中常见的直撑设计一般都没有考虑基坑位移和土压力的变化,总结了土压力和基坑位移之间非线性关系的研究现状,分析了随坑壁转动时土压力大小和方向的变化规律。在此基础上,推导了直撑轴力和坑壁位移之间、以及直撑纵向变形与坑壁位移之间的数学关系式。结合工程实例,进一步研究了直撑轴力和变形随基坑初始位移、支撑点、土压力作用点、土体与挡土结构间摩擦角等因素变化时的发展变化规律。研究表明,直撑轴力及其变形随基坑位移、支撑点高度、土体与挡土结构之间摩擦角的增加而减小,随土压力作用点高度的增加而增大,与基坑初始位移值基本无关。 相似文献
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北京市轨道交通基坑工程地表变形特性 总被引：1，自引：0，他引：1
根据基坑开挖深度、地层条件的不同,对北京市轨道交通80个明挖顺作法基坑工程实测结果进行统计分析,研究确定北京砂卵石和黏性土地区深基坑开挖引起的周边地表变形规律。研究表明：基坑工程周边地表最大变形的实测结果分布形态为正态分布或半整体分布,地表沉降变形值较大;最大地表沉降的平均值约为砂卵石地区0.11%H（H为开挖深度）,黏性土地区0.20%H;地表变形与桩体向基坑内、外的水平位移值有一定的对应关系;地表沉降随插入比的增大而减小,黏性土地区基坑支撑系统刚度对地表沉降有明显的影响;北京地区基坑工程周边主要影响区约为0.6H或0.7H范围以内。研究成果可对未来北京及其他地区城市轨道交通基坑工程变形大小、安全性的预测和评估、指导基坑工程设计与施工和对防止基坑事故的发生等具有重要意义。 相似文献
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土钉支护因其施工简单、造价低、工期短和施工技术成熟等优点,在工程中得到广泛应用,但目前其设计计算理论缺乏,且现行规范给出的变形允许值存在不足,如现行土钉规范（规程）仅是简单地规定一个变形允许值,没有结合基坑的特点、支护类型、周边环境等因素来规定,更没有将基坑的变形与基坑稳定联系起来综合确定其监测指标预警值等,因此,导致这种性价比很好的支护技术有减少应用的趋势。利用变模量强度折减法对土钉支护变形和稳定关系进行了探讨性研究,经大量的计算分析,给出了土钉支护的变形与稳定统一判定指标--位高比 ,且计算发现,同一种土质、同一稳定系数K对应的不同高度H的位高比几乎相等。给出了一定强度和一定深度土钉支护位移预警值和最大位移允许值,利用给出的表格,可直接确定其位移预警值和最大位移允许值,便于工程师应用,也为实际土钉支护结构确定变形预警值提供了参考。提出的方法不仅能够确定土钉支护结构变形值,且对类似支护结构确定变形值也提供了一种方法和思路,对推进基坑规范完善和改进具有一定的参考和借鉴作用。 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