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龙泉市鼎丰壹城桩基项目主要有桩径大、单桩极限承载力大等特点,最大桩径达2400 mm,单桩竖向极限承载力达89600 kN,建筑领域参考经验较少。本桩基工程主要面临砂层和卵石层易塌孔、入岩难和沉渣清理困难等三大挑战。结合国内桥梁、铁路桩基施工经验,通过增加砂层和卵石层稳定性、采用分级扩孔和孔底除渣等关键技术,针对性解决现场施工难题。灌注桩达到龄期后,经现场检测,施工完成的桩大多为I类桩。通过对本工程施工经验的总结,为大直径旋挖钻孔灌注桩在建筑领域的应用提供借鉴。 相似文献
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载体桩作为一种新型的桩基础形式近年来在工程中被广泛运用,其基本原理是通过柱锤夯击成孔并对桩端以下土层及填料夯实形成复合承载体,提高单桩竖向承载力。目前载体桩在砂土、黏性土、粉土及软土中均取得了一定的研究成果,而在卵石地层中的研究较少。以奉节地区某标准厂房桩基工程为例,研究载体桩在奉节草堂地区卵石地层的设计与施工,结合载荷试验成果对载体桩受力机理分析。研究结果表明:以卵石作为持力层的载体桩在奉节草堂地区具有较好的适用性,静载试验与沉降观测表明载体桩承载性能良好,是一种安全经济的基础形式;载体桩静载试验Q-s曲线一般呈缓变型,表明载体桩在卵石地层中的受力形式更接近于端承桩;卵石地层中载体桩的适用性与卵石成分、级配密切相关,土体大颗粒孤石可能使柱锤夯击受阻,施工前应先进行试桩及超前地质钻探。 相似文献
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我国长江中下游沿岸地基中分布有较厚的砂土层,砂土层是桩基的良好持力层。该地区砂性土埋藏浅,厚度大,往往夹杂粉土或粉质黏土,一般随深度增大,砂土变密实。已有研究成果中,针对桩身穿过多层砂土条件下桩基承载力的研究较少。砂土地基中打入桩试验结果表明,砂性土的状态对打入式预制桩的施工产生很大的影响,在松散或稍密的砂性土中沉桩一般比较容易,而在中密或密实的砂性土中则较为困难。本文通过某电厂工程灌注桩现场静载试验,研究了砂土地基中桩身沉降随荷载变化规律,分析了桩身轴力随地层深度变化特征及不同土层的桩侧摩阻力。设计钻孔灌注桩桩径为800mm,桩长为47.2m,桩身混凝土强度等级为C35,桩身穿过9层土层,由现场3根桩静载试桩结果可知,荷载与沉降关系呈非线性,Q-s曲线分为弹性阶段、弹塑性阶段和整体破坏3个阶段, 15m深度以下的粉细砂层侧摩阻力对桩身轴力影响较大, 15m以上粉质黏土和淤泥质土对桩轴力影响较小。根据Q-s曲线确定单桩极限载荷约为4800～5400kN,平均值为5201kN,可满足设计要求,地基中下部砂土层承载力较大,砂土侧摩阻力大于黏性土的侧摩阻力,最大可达到70kPa。所得结论可为该类地基进一步的理论研究及工程设计提供有益的参考。 相似文献
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针对饱和砂土地区盾构隧道超近接高铁桥墩摩擦桩的工程问题,采用钻孔灌注桩及高压旋喷桩组合隔断隧桩间位移。分别对钻孔灌注桩、高压旋喷桩及盾构上下行线近接高铁桥梁桩基引起的高铁桩基的变形及变位开展现场试验,对现场实测数据及规律进行分析。结果表明,钻孔灌注桩施工使高铁桥墩产生沉降,占施工过程最大沉降量的 75%～125%;高压旋喷桩施工导致桥墩产生隆起,占施工过程最大沉降量的-50%,旋喷桩施工完成后将持续一段时间;盾构施工对高铁桥墩竖向变形产生影响,距离高铁桩基越近影响越大,同时累计沉降跟盾构施工控制有较大关系。 相似文献
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多年冻土区桥梁工程钻孔灌注桩温度场研究 总被引：2，自引：1，他引：1
针对多年冻土区钻孔灌注桩施工中混凝土水化热对冻土温度扰动问题,以青藏公路214沿线查拉坪旱桥桩基为实例,结合桩基施工完成后现场地温观测数据,进行了钻孔灌注桩水化热对桩周土体温度的影响研究,并分析桩周土回冻过程中地温场的变化规律.结果表明：混凝土水化热对距桩0.6 m与0.9 m处冻土温度影响较大.距桩2 m的测温孔温度曲线受混凝土水化热的影响较小,可以忽略.桩基施工完成后33天后桩侧开始出现负温,119天后桩侧各土层均降至负温,134天后桩侧土形成稳定冻土,201天后桩侧各土层温度与天然孔较接近. 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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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
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正20142002 Wei Hualing(Institute of Geophysical and Geochemical Exploration,Chinese Academy of Geological Sciences,Langfang065000,China);Zhou Guohua Element Content and Mineral Compositions in Different Sizes of Soil in Tongling Area,Anhui Province(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(11),2013,p.1861 相似文献
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正20141768 An Shaopeng(Institute of Rock and Soil Mechannics,Chinese Academy of Sciences,Wuhan 430071,China);Wei Lide Experimental Study on Mechanical Behavior of Xigeda Formation Siltstone and Structure Interface(Journal of Engineering Geology,ISSN1004-9665,CN11-3249/P,21(5),2013,p.702-708,9illus.,1 table,16 refs.) 相似文献