自流水对施工水下混凝土桩的危害

在高压自流水盆地条件下进行混凝土灌注桩施工在国内实属罕见。因其特殊的水文地质条件给桩施工带来的难题，形成了常规混凝土灌注桩施工所不可能遇到的工程现象。作者通过参与该工程的病害处理，较完整地阐述了在该类地区进行混凝土灌注桩施工中钻孔因地下水喷涌而坍塌，灌注砼时形成负压引起自流水脉冲式侵入，桩顶微通道溢水现象及桩头混凝土保护层缺失等系列工程问题。作者分析了此类工程现象的形成机制，并对施工对策、防治手段     

后插钢筋笼法成桩在华正大厦基坑支护工程中的应用

后插钢筋笼法成桩就是先施工素混凝土桩，然后再用专用设备插入钢筋笼形成钢筋混凝土灌注桩。结合工程实例介绍了其施工工艺、配套设备、机具、施工要点、施工中遇到的问题及解决办法。     

水下混凝土灌注桩施工方法

在抗滑桩、地基桩基础、桥梁桩基础等桩基工程施工中,由于桩基处于水中或桩孔内渗水量大,桩孔内有大量积水不能及时抽排而出,按普通方法施工混凝土将导致混凝土离析形成断桩导致工程质量事故。因此,在该情况桩基施工中,通常采用水下混凝土浇筑法进行。     

水下混凝土灌注桩施工方法

在抗滑桩、地基桩基础、桥梁桩基础等桩基工程施工中,由于桩基处于水中或桩孔内渗水量大,桩孔内有大量积水不能及时抽排而出,按普通方法施工混凝土将导致混凝土离析形成断桩导致工程质量事故。因此,在该情况桩基施工中,通常采用水下混凝土浇筑法进行。     

软土地基中咬合桩桩身下沉问题的探讨

软土地基中咬合桩套管内灌注混凝土极容易造成桩体下沉,不但影响钢笼标高,也造成混凝土超方,影响工程质量和经济效益。结合具体的工程实例,对软土地基中咬合桩桩身下沉问题进行了探讨。咬合桩桩身下沉主要由桩端虚土压缩、桩端土压缩沉降和桩身砼凝固沉降组成。在施工前可根据经验系数K1值先预估桩身下沉的理论量,然后在施工中预留相同量土柱高度和相应的混凝土加灌高度,以保证在施工完成后桩身能够满足设计要求。     

钻孔压灌粉煤灰混凝土桩复合地基的应用研究

通过工程实例，介绍了钻孔压灌粉煤灰混凝土桩的施工技术，说明了其施工工艺及特点，并利用6组静荷载试验成果，对粉煤灰混凝土桩复合地基的承载力特性进行了分析。     

无锡财富广场住宅楼两种桩型的技术经济评价

针对无锡财富广场的具体施工条件，通过对钻孔灌注桩、静压预应力高强度混凝土管桩两种桩型的施工技术条件及经济因素分析，得出了该工程应优先选用静压预应力高强度混凝土管桩的结论，并指出在静压管桩施工中需要做好挤土效应的预防工作。     

长螺旋CFG桩施工中的几个技术问题

为避免长螺旋CFG桩施工中产生质量问题,施工中应注意在桩位控制、桩基施工、混凝土质量、冬季施工措施、褥垫层设置、成桩后防护等方面引起重视,针对以上几个技术问题进行了经验总结和探讨。     

人工挖孔桩遇水处理

人工挖孔桩只要配以简易的施工机具就可以将孔挖到设计要求的持力层(硬土或岩层),使桩作为端承构件,不仅沉降量小,而且还能获得极大的单桩承载力。所以这种桩被广泛应用于工程建设中。由于人工挖孔桩的地下施工特性,且难以避开水源,遇水处理是人工挖孔桩施工过程中经常出现的问题。下面结合工程实际介绍几种处理方法:1 采用干海带堵漏人工挖孔桩一般采用Mu 10砖、M7.5水泥砂浆砌体或C10-C20混凝土护壁。砌体施工时,由于砂浆饱满度不密实、渗水洗刷砂浆、下轮砌体顶部与上轮砌体底部搭接处形成缝隙;混凝土浇筑时,由于混凝土本身不密实、含…     

预应力管桩—水泥土搅拌桩组合法加固软土地基

由预应力混凝土管桩、水泥土搅拌桩及桩间土组成的复合地基，其承载力是由桩和桩间土共同分担的。通过预应力混凝土管桩和水泥土搅拌桩的施工，实现对桩问土的挤密加固，可充分发挥和利用地基土的承载潜力，有效地解决软土地基承载力不足的问题。本文结合工程实例，采用多种试验测试方法对这类复合地基进行检测和分析，表明：在一定地质条件下，混凝土管桩-水泥土搅拌桩复合地基不失为一种节约投资、行之有效的软基处理方法。     

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.     

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).     

HYDROGEOLOGY

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     

METAMORPHIC PETROLOGY

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),     

SERIALS

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GEOPHYSICAL EXPLORATION

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-     

QUATERNARY GEOLOGY & GEOMORPHOLOGY

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-     

PETROLEUM GEOLOGY

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.)     

GEOCHEMISTRY

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