聚合物泥浆在地下连续墙施工中试验

本文简要叙述了一种新型地下连续墙施工稳定液-聚合物泥浆的研制,这种新型聚合物泥浆克服了目前使用的地下连续墙稳定液品种单一、性能较差的缺点,满足复杂地层的地下连续墙施工需要。同时阐述了这种稳定液的组成成份和性能及它的主要特点。     

地下连续墙施工稳定液的试验研究

目前，我国使用的地下连续墙稳定液品种单一、性能较差，不能满足复杂地怪的地下连续墙施工。根据现代地下连续墙成槽工艺及地下连续墙对稳定液的要求，我们在室内研制了聚合物溶液，以满足现代地下施工的需要。     

地下连续墙施工中低固相不分散聚合物稳定液的应用

针对上海外滩金融中心基坑围护工程地下连续墙施工中地层及环境情况，在分析传统的膨润土-NaCMC泥浆体系存在缺点的基础上，研制了新型的低固相不分散聚合物稳定液。     

110 kV自忠变电站地下连续墙的施工及质量控制

结合具体的工程实例，从地下连续墙施工方案、工艺的选择和施工方法的具体实施及其质量控制方面论述了地下连续墙施工技术。     

地下连续墙槽壁稳定的研究

从三个主要影响地下连续墙槽壁稳定的方面出发,分析和研究影响地下连续墙槽壁稳定的几个因素:地质条件、施工机械和成槽方法、稳定液的类型和质量对槽壁稳定起着至关重要的作用。探讨了槽壁的失稳机理,分析致稳和失稳两方面的因素。通过对槽壁稳定的研究,为解决槽壁坍塌问题提供理论依据和研究方法。     

连续闭合钢箱接头地下连续墙施工技术

目前许多深基坑工程对于超深地下连续墙的刚度及防渗性能要求较高。在分析传统常用的接头形式在施工过程中存在问题的基础上,提出了一套行之有效的施工方法——连续闭合钢箱接头。详细介绍了连续闭合钢箱接头地下连接墙施工技术及其施工效果。     

PBA暗挖地铁车站洞内地下连续墙施工力学响应分析

北京某地铁PBA暗挖车站采用边导洞内施工地下连续墙止水，在国内尚属首例。以该工程为依托，采用MIDAS软件模拟了PBA工法施工过程中洞内地下连续墙的力学响应规律，并与现场监测数据进行了对比分析。研究结果表明：（1）地下连续墙施工引起的地表沉降量较小，约占地表总沉降量的9%;(2)扣拱施工阶段、站厅和站台层开挖支护阶段地下连续墙水平位移变化较大，在实际工程中需对这三个施工阶段加强监测和施工控制；（3）地下连续墙竖向位移整体以隆起变形为主，沉降变形不明显，沿地连墙纵向各施工阶段中墙顶的沉降量略有波动，整体上趋近均匀分布；（4）车站主体结构施工完成后，地下连续墙墙体所受的拉、压应力均未超过混凝土抗拉、抗压强度允许值，地下连续墙结构处于安全状态。     

地下连续墙用方形锤头的设计及应用

方形锤头是地下连续墙成槽施工的重要钻具,本文简要介绍了一种新型地下连续墙方形锤头的结构设计、施工工法及应用情况。新型方形锤头整体框架采用焊接而成,结构合理,尺寸可根据用户需要优化调整,且具有导向性好、单位面积冲击功高、过水面积大和方便打捞等优点。锤头研制成功后,配合冲击反循环钻机,采用气举反循环工艺,先后在厦门、深圳等多个城市地铁工地施工,施工效率明显,取得了良好的经济效益和社会效益。新型方形锤头的研制成功,为地下连续墙成槽施工提供了一种更优的钻具选择。     

双导向孔穿越城市立交桥铺设电力管线非开挖施工技术

上海市长春藤名品商厦地下连续墙为二墙合一的设计，对沉渣厚度和混凝土浇灌质量要求很高，采用了气举反循环清底和置换稳定液的技术，使沉渣厚度和稳定液密度大幅度降低，确保了工程质量。同时分析了气举反循环清底和置换稳定液技术存在的问题。     

气举反循环技术在上海长春藤名品商厦地下连续墙施工中的应用

上海市长春藤名品商厦地下连续墙为二墙合一的设计，对沉渣厚度和混凝土浇灌质量要求很高，采用了气举反循环清底和置换稳定液的技术，使沉渣厚度和稳定液密度大幅度降低，确保了工程质量。同时分析了气举反循环清底和置换稳定液技术存在的问题。     

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).     

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.)