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根据浃里陈大桥桥头试验段的地表沉降与分层沉降的现场监测结果，对真空联合堆载预压加固软基中的地表沉降以及分层沉降随时间与空间的变化规律进行了分析，表明该方法能大幅度减少工后沉降量，达到防止“桥头跳车”的作用。 相似文献
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增压式真空预压处理软基的加固机理 总被引：1，自引：0，他引：1
常规的真空预压往往由于竖向排水板堵塞引起排水固结效果差、工期长。对此,笔者采用增压式真空预压处理某一站场软土地基弥补上述不足。通过分析对比增压式和常规真空预压处理方式下地基在加固期内的沉降、孔隙水压力变化特征,评价增压条件下的处理效果。结果表明：采用增压式真空预压三、四区地表沉降量明显大于常规处理的一区,且孔隙水压力消散速度也快于一区;而1.0 m间距的三区产生的预压沉降量较1.2 m间距的四区增加约30%;增压式真空预压利用增压管的增压作用能加速软基排水过程并改良排水板易淤积的不良性能。 相似文献
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真空排水预压下土体变形的应力路径分析 总被引：4，自引：0，他引：4
通过室内试验, 对真空排水预压下土体变形特性进行了应力路径分析, 测定软土地基在真空预压加固后应力路径的改变对沉降量的影响, 论证真空排水预压加固软土地基不能消除其剪应力引起的剪切变形, 结合实例, 计算其后期沉降量与固结沉降量的比值, 并推算软土地基在真空预压下其最终沉降量计算公式的修正系数。 相似文献
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根据某一级公路软土路基的各类监测数据结果,详细地分析了地表沉降、孔隙水压力、土体水平位移等随时间和空间的变化规律,结果表明:淤泥层的沉降量占路基总沉降量的65%,低液限黏土层(15m以下)的水平位移较小,这与其土体强度较大有关; 由于过快的填筑速率可能促使总的超静孔隙水压力大于0,所以在堆载过程中需要对孔压数据进行密切观测,以防止路基失稳; 加固区30m以外基本无地表水平位移,软基处理过程不会对江堤安全性产生影响; 结合孔压和土体分层沉降可知,真空联合堆载预压的有效影响深度可以达到排水板以下2m的范围。 相似文献
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真空预压法在大型刚性基础软基处理中的应用效果分析 总被引：1，自引：0，他引：1
浙江某污水处理厂大型钢筋混凝土结构软土地基处理工程采用了真空预压方法。采用该方法处理后土体强度满足了设计要求，各土层的物理力学性质指标有了明显改善，取得了良好的加固效果。本文通过现场地表沉降、孔隙水压力、侧向位移等实测资料及加固前后室内、原位试验数据对比分析了处理效果，并利用现场实测沉降曲线推算出最终沉降量及工后沉降量，对真空预压法应用于大型刚性基础的软基处理的可行性及存在问题进行了初步的探讨。 相似文献
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在工程用土资源越来越紧张和环境日益恶化的情况下淤泥资源化利用成为一个亟待解决的问题。通过向河底淤泥中掺入一定量的生石灰,再用真空预压结合外加剂木质素磺酸钙来改善土体的渗透、强度和变形等特性,总结并分析了掺木量对稳定排水量,稳定沉降量、强度、孔隙等的影响以及真空预压后石灰稳定土龄期下土体强度的变化规律。试验结果表明,抽真空后改良土具有较低含水率,土体强度增长较大,孔隙较小,后期沉降较小,加固土体以满足填筑用土要求,经济性分析表明该法是可以接受的。 相似文献
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针对沿海地区深厚淤泥软土的特点和工程建设时效性的要求,本文在总结软土排水固结S-T曲线规律的基础上提出应用短程超载真空预压动力排水固结法加固深厚淤泥的方法,发现深厚淤泥软土在真空负压、超载正压和动力冲击三者优化组合的作用下,主固结沉降可在短时间内完成,土体强度提高的同时地表吹填土在动力冲击作用下形成超固结的硬壳层。深厚淤泥软土加固后能够满足地基承载力的要求并且能够有效控制工后沉降和不均匀沉降。并通过工程实例,对地基处理后的效果进行分析评价,证明了该工法的可行性和有效性,为沿海地区广泛分布的深厚淤泥软土地基的加固提供了新的途径。 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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Emmanuel Skourtsos Daniel Vachard Alexandra Zambetakis-Lekkas Rossana Martini Louisette Zaninetti 《Comptes Rendus Geoscience》2002,334(12):925-931
Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by Paradunbarula (Shindella) shindensis, Hemigordiopsis cf. luquensis and Colaniella aff. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions. To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931. 相似文献
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正20141596 Liu Yunhuan(School of Earth Sciences and Resources,Chang’an University,Xi’an 710054,China);Shao Tiequan Early Cambrian Quadrapyrgites Fossils of Xixiang Boita in Southern Shaanxi Province(Journal of Earth Sciences and Environment,ISSN1672-6561,CN61-1423/P,35(3),2013,p.39-43,3 illus.,20 refs.) 相似文献
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正20141719 Chen Zhijun(State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China);Chen Jianguo Automated Batch Mapping Solution for Serial Maps:A Case Study of Exploration Geochemistry Maps(Journal of Geology,ISSN1674-3636,CN32-1796/P,37(3),2013,p.456-464,2 illus.,2 tables,10 refs.) 相似文献
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正20140962 Chen Fenning(Xi’an Institute of Geology and Mineral Resources,Xi’an710054,China);Chen Ruiming Late Miocene-Early Pleistocene Ostracoda Fauna of Gyirong Basin,Southern Tibet(Acta Geologica Sinica,ISSN0001-5717,CN11-1951/P,87(6),2013,p.872-886,6illus.,56refs.) 相似文献
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正1.IGNEOUS PETROLOGY20142008Cai Jinhui(Wuhan Center,China Geological Survey,Wuhan 430205,China);Liu Wei Zircon U-Pb Geochronology and Mineralization Significance of Granodiorites from Fuzichong Pb-Zn Deposit,Guangxi,South China(Geology and Mineral Resources of South China,ISSN1007-3701,CN42-1417/P,29(4),2013,p.271-281,7illus., 相似文献
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正20141205Cheng Weiming(State Key Laboratory of Resources and Environmental Information System,Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing 100101,China);Xia Yao Regional Hazard Assessment of Disaster Environment for Debris Flows:Taking Jundu Mountain,Beijing as an 相似文献
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正20141266Fan Chaoyan(Guangdong Provincial Key Laboratory of Mineral Resources and Geological Processes,Guangzhou 510275,China);Wang Zhenghai On Error Analysis and Correction Method of Measured Strata Section with Wire Projection Method(Journal of 相似文献