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唐-曹高速公路软土的微结构特征研究 总被引:1,自引:0,他引:1
对软土地基处理技术研究己成为改善投资环境、加快环渤海地区建设、科学合理利用土地资源的重要研究课题。软土地基处理方法的科学合理与否,关键是从软土本身的结构特征揭示出影响软土变形和强度的本质因素。以唐-曹(唐山市至曹妃甸)高速公路通过地区的沉积软土为研究对象,综合海积软土的基本物理力学性质和微结构特征建立软土微结构量化参数。通过室内综合实验和理论分析,对海积软土微结构与宏观力学性质关系进行系统地研究,对海积软土的结构强度与工程效应进行论证,提出以建立在分维分形理论基础上的孔隙结构因子作为衡量海积软土结构强度和破坏趋势的综合性参数,且可以在求解先期固结压力的同时定量地确定土的结构强度,值得同行借鉴。 相似文献
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海积软土是一种结构性土,具有结构连结强度。其压缩曲线呈现出超固结土的压缩的曲线形式。强度曲线为二段折线,在应力小于σ'k时表现出超固结土的力学特征。而当应力水平高于这一临界值时,表现出正常固结土的力学特性。对其结构连结的成因进行了简单探讨。 相似文献
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实验室软土多级固结蠕变试验成果表明,海积软土具有非线性、不可逆的、与时间相关的固结变形特性。在此基础上,提出了时间效应系数的概念,并构造了反映海积软土一维固结蠕变的本构关系。 相似文献
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土结构性模型是 2 1世纪土力学学科的核心问题。基于海积软土一维固结蠕变的宏观力学性状与微观结构定量分析相结合的方法 ,提出了软土在外荷作用下微观结构的演变模式 ,由此建议了一个含结构参数的固结变形本构关系。用试验资料和工程实例进行了初步验证 ,表明所建模型可以预测多级加载条件下海积软土的变形规律。 相似文献
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结构性海积软土的弹塑性研究 总被引:6,自引:1,他引:5
通过对天津市欠固结海积软土进行的大量试验,研究了土的结构性和弹塑性变形本构关系两个方面的问题。首次引入结构强度系数,建立了微结构定量参数与力学参数之间的关系,并提出一种综合考虑结构性影响的应力应变关系模型,为海积软土的结构性模型研究及实际应用提供了一条新的途径。 相似文献
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天津地区海积软土结构强度及其对力学特性的影响 总被引:1,自引:1,他引:1
海积软土是一种结构性土,具有结构连结强度.其压缩曲线呈现出超固结土的压缩曲线形式.强度曲线为二段折线,在应力小于σ'k时表现出超固结土的力学特性.而当应力水平高于这一临界值时.表现出正常固结土的力学特性.对其结构连结的成因进行了简单探讨. 相似文献
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河口滨海区浅层海积软土工程特性研究 总被引:1,自引:0,他引:1
永定新河河口地区覆盖了厚约18 m的海积软土.通过对上百组试验数据的统计和回归分析,研究了永定新河河口地区海积软土的工程参数特性及其随深度的变化规律,建立了相应的回归方程.研究结果认为,研究区海积软土具有高含水量、高孔隙比、高压缩性、低强度、弱渗透性和高盐度等特性.天然含水量是软土的基本参数,其与其它工程参数的相关分析结果表明利用天然含水量可粗略评估其它工程参数特性.软土的工程参数随深度变化存在一定的规律性,其变化规律不仅受软土类型制约,而且与埋设深度密切相关. 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 Lozach 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