混凝土垫层对围护墙支撑效应的监测分析

控制基坑变形是保证基坑及周边环境安全的关键,而底板施工期间墙体变形的控制更是关注的重点。结合上海轨道交通某在建地铁车站基坑开挖时的变形监测数据及跟踪工况,对素混凝土垫层的支撑约束作用进行了监测分析。坑底暴露时间对底板施工阶段内的基坑变形有着显著影响,基坑暴露时间的长短是控制底板施工期间围护墙变形的关键。素混凝土垫层对围护墙体变形具有一定的支撑效应,在一定程度上能起到类似结构底板的作用。施工中应尽快完成混凝土垫层的浇筑工作,尽早发挥垫层对围护墙体的支撑作用。垫层对墙体的支撑效果与其自身的平直度等因素有很大关系,破坏垫层的整体性,则会削弱其对围护墙体的支撑作用。提出对坑底施工阶段基坑变形的控制措施,缩短底板施工阶段的暴露时间,提高垫层的整体性,加快底板施工,尽早形成底板混凝土对围护墙体的支撑作用,从而控制开挖阶段的基坑变形,对其他深基坑工程具有一定的参考价值。     

时空参数调整在深基坑工程中的应用

本文研究在深基坑开挖过程中不同时空参数对基坑变形的影响,根据时空效应原理并结合环境保护等级要求,通过对实测数据的反分析,优化制定施工参数,从控制连续墙变形进而控制周围土体的位移,该方法是基坑工程变形控制设计理论的工程应用。     

基坑全过程开挖及邻近地铁隧道变形实测分析

根据邻近已运营地铁隧道的基坑工程监测数据,对基坑开挖全阶段施工过程的深层土体侧向位移与邻近地铁隧道变形之间的规律展开研究,探讨基坑开挖的施工危险节点与重点影响区域。研究发现,基坑开挖前期围护结构施工和降水均对地层和邻近地铁产生了不容忽视的初始位移影响,围护结构长时间无支撑暴露是基坑侧移快速增长的危险时段;基坑开挖具有空间效应,中部侧向变形要大于边角,且单向开挖易造成后挖区土体的位移场和应力场叠加,引起邻近隧道的最大变形向后挖区偏移;基坑开挖深度与邻近地铁埋深相近时,隧道结构产生显著的水平位移和“横鸭蛋”式收敛变形,竖向位移波动不大;深层土体侧移曲线表现为“阶梯鼓肚形”,土体最大水平位移与隧道变形在小范围内呈线性关系,但随着侧移量的增大,隧道变形发生偏离拟合曲线的超线性增长,在工程中应值得关注。     

上海中山医院基坑逆作法施工时间效应分析

软土具有流变性,因此,分析基坑开挖时需要考虑时间效应。逆作法施工时,由于出土条件和结构施工条件的限制,导致施工周期延长,因此,基坑施工的时间效应尤为显著。以上海中山医院工程为例,考虑软土流变效应,建立有限元模型对逆作法基坑的施工过程进行模拟,分析了施工期间各工况的围护和土体的内力与变形性状,并与实测结果进行了对比分析。结果表明,考虑土体流变的分析方法能较好的模拟逆作法施工的时间效应,并合理地反映基坑开挖过程对围护以及周边环境的影响。逆作法基坑施工过程复杂,开挖周期相对较长,应合理安排施工流程和施工速度,以达到控制围护结构及土体变形、保护周边环境的目的。     

基坑施工对临近运营地铁影响控制标准及关键技术

随着城市的快速发展,地铁车站周边开发的建筑越来越多,周边建筑施工对地铁车站将产生不可避免的不利影响。本文结合某大型建筑深基坑工程的设计、施工及监测数据,通过有限元计算,分析基坑开挖施工力学特征,研究基坑施工对临近地铁车站的变形影响。研究发现,基坑采用合理的地下连续墙、钻孔灌注桩等围护体系、适当的被动区加固方式、科学的分基坑开挖施工组织等措施,可以保证基坑开挖施工对临近车站的影响在可控制、可接受的范围内,为软土地区类似基坑的设计、施工提供参考经验。     

紧邻地铁枢纽深基坑变形特性离心模型试验研究

对于紧邻地铁枢纽的深基坑工程,其开挖方式对基坑变形特性和施工安全控制有着显著影响。以上海某紧邻地铁隧道的深基坑工程为背景,其设计方案将该基坑工程划分为大、小基坑分别施工,重点研究大、小基坑的开挖方式对于围护结构及地铁隧道变形的影响。针对“先挖大基坑,后挖小基坑”的开挖方案,采用离心模型试验,研究开挖过程中地下连续墙和隧道结构的变形特性。试验结果表明,“先挖大基坑,后挖小基坑”的开挖方案可以有效地控制基坑变形,所得结论对于类似的紧邻地铁隧道深基坑工程设计与施工具有参考价值。     

A calculation method for deformation of diaphragm wall of narrow deep foundation pit in soft soil considering spatio-temporal effectEI北大核心

为准确评估软土地区基坑施工安全以及对周围环境的影响,开挖过程中的时间和空间影响因素不可忽视。以长江漫滩软土地区某深基坑开挖工程为依托,首先建立考虑顺逆结合施工过程的有限元模型,将地连墙水平位移的计算值与实测值进行对比,验证有限元计算的可靠性;基于理论分析、数值计算和实测数据,采用坑角效应影响系数和等效水平抗力系数来衡量时空效应对支护变形的影响,提出考虑时空效应的地连墙变形计算方法;通过工程实例验证了在软土地区基坑设计计算中考虑时空效应的必要性以及所提计算方法的合理性。该研究成果可为软土地区深基坑变形计算提供有益借鉴。     

长江漫滩区深大异形基坑施工对紧邻特大型桥梁影响及变形控制研究

随着地下空间资源的开发利用,越来越多深基坑呈现出开挖深、规模大、形状不规则等特点,其支护结构设计复杂,施工难度大,具有明显的空间效应。本文以南京地铁某基坑工程为例,分析基坑施工对邻近桥梁的影响。其场区位于长江下游漫滩相二元结构地层分布地段,上部软土层厚度大,下部承压含水层地下水位高、水量丰富,地质条件复杂,该基坑为典型的深大异形基坑,距离某大桥的双曲拱引桥仅为7. 2 m,由于之前桥梁已遭受其他地下工程施工产生的较大变形,所以后续工程对其影响变形控制要求极高。为此,该车站基坑支护结构设计基于地下空间实际功能采用设置分隔墙分区开挖及MJS超深工法墙综合变形控制方案。本文通过有限元数值模拟计算,开展复杂环境下基坑开挖引起的围护结构及桥梁桩基的变形预测分析,计算结果显示,该深大狭长异形基坑开挖对邻近桥梁沉降变形影响显著,通过设置分隔墙分区开挖及MJS工法墙进行变形控制,能够较好地控制基坑的空间效应,减少“长边效应”、“异形效应”等对桥梁沉降变形的影响。通过现场基坑开挖过程实际监测结果,验证这一综合变形控制方案的可行性。该研究成果对于类似复杂地质条件下深大狭长异形基坑的支护及施工设计具有很好的借鉴意义。     

基坑开挖卸载对地铁区间隧道影响的数值模拟

上海新金桥广场基坑工程位于地铁区间隧道的正上方,坑底距隧道顶的最小距离仅为4 m.基坑开挖对该地铁区间隧道影响的分析与计算成为该工程的关键.为此建立了该基坑工程的数值分析模型,模型充分考虑了设计中隧道周围土体加固、充分利用时空效应开挖土方等重要措施,并采用了能反应应力路径的上海软土卸荷模量.数值模型对实际施工工况进行模拟,动态地分析了施工过程中开挖卸荷对地铁隧道的影响.为优化设计和施工提供了有益的参考.     

邻近基坑开挖的运营地铁车站结构安全度分析

为保证既有地铁车站的正常运营和地下车站结构的安全,在邻近基坑开挖过程中就需要严格控制运营地铁车站结构的变形。结合上海某邻近基坑开挖的运营地铁车站,运用叠加原理,采用有限元荷载结构法和强制位移法,分别按照裂缝控制和强度控制来对车站标准段结构的稳定性及其允许变形进行分析和反算,为基坑施工提供车站结构变形的控制标准     

The terrestrial fauna of the Late Triassic Pant-y-ffynnon Quarry fissures,South Wales,UK and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia)

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.     

Définition d'une limite multicritère ; stratigraphie du passage Campanien–Maastrichtien du site géologique de Tercis (Landes,SW France)Definition of a multi-criteria boundary; stratigraphy of the Campanian–Maastrichtian interval of the geological site at Tercis (Landes,SW France)

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.     

The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts

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.     

Quaternary stresses revealed by calcite twinning inversion: insights from observations in the Savonnières underground quarry (eastern France)

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).     

NONMETALS DEPOSITS

正20141520 Bo Ying(Key Laboratory of Metallogeny and Mineral Assessment,MLR,Beijing 100037,China);Liu Chenglin Saline Spring Hydrochemical Characteristics and Indicators for Potassium Exploration in Southwestern and Northern Tarim Basin,Xinjiang(Acta Geoscientica Sinica,ISSN1006-3021,CN11-3474/P,34(5),2013,p.594-602,5 illus.,3 tables,28 refs.)     

MATHEMATICAL GEOLOGY

正20141243Chen Ge(Hangzhou Research Institute of Petroleum Geology,PetroChina,Hangzhou 310023,China);Si Chunsong Study on Sedimentary Numerical Simulation Method of Fan Delta Sand Body(Journal of Geology,     

PROSPECTING EXPLORATION

正20142599Chen Sanming(Guangxi Key Laboratory of Concealed Deposits Exploration,Guilin University of Technology,Guilin541004,China);He Yuzhou Block Model and Reserves Estimation of Panzhihua Iron Deposit Based on 3D Geological Modeling(Journal of Guilin University of Technology,ISSN1674-9057,CN45-1375/N,33(4),2013,p.610-615,9illus.,1table,15refs.)     

STRUCTURAL GEOLOGY

正20140594 Bai Daoyuan(Hunan Institute of Geology Survey,Changsha 410016,China);Zhong Xiang Faults in the Jingzhou Basin and Their Tectonic Settings(Geotectonica et Metallogenia,ISSN1001-1552,CN44-1595/P,37(2),2013,p.173-183,6illus.,59refs.)Key words:basin evolution,tectonic setting,South China In the Upper Paleozoic and Jurassic se-     

STRUCTURAL GEOLOGY

正20141912Cao Hui(State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)Gravitational Collapse and Folding during Orogenesis:A Comparative Study of FIA Trends and Fold Axial Plane Traces(Geology in China,ISSN1000-3657,CN11-1167/P,40(6),2013,p.1818-1828,9illus.,35refs.,with