YCJF20型冲击反循环钻机进行地下 连续墙成槽施工技术

成槽施工是地下连续墙施工的重要工序,厦门地铁3号线湖滨东路站地下连续墙施工中采用YCJF20型冲击反循环钻机冲击钻进法进行成槽施工。介绍了YCJF20型钻机的主要技术参数、特点和工作原理,以及导墙和导孔施工、钻机布置、泥浆制备、冲钻成槽等成槽施工过程。     

地下连续墙施工技术

地下连续墙是一种科学先进的施工方法。由于地下连续墙既可用作地下工程的防渗挡土结构墙,又可用作建筑物的承重基础墙,所以已成为地下工程的一种基本的选择方案。根据８个地下连续墙工程项目的施工经验,叙述地下连续墙的导墙、成槽、钢筋混凝土灌注、泥浆处理等施工工艺,并列举了３个工程实例。     

地下连续墙施工力学机理三维数值分析

采用三维有限差分方法,模拟了地下连续墙成槽开挖及混凝土浇筑施工全过程,研究了连续墙槽段外围土层在地下连续墙施工过程中的应力状态与变形形态,并将计算结果和现场实测结果进行比较。结果表明,数值计算应力结果与实测结果规律基本一致,但槽段底部数值计算应力变化梯度比实测值略大,采用该计算方法模拟地下连续墙施工全过程具有一定的可行性和较强的可靠性。     

CJF-12型钻机在地下超薄连续墙工程中的应用

介绍了CJF－12型钻机反循环钻机在黄河堤岩荷泽段施工地下超薄连续墙的概况。根据工程实际情况，对钻机进行了改造，并设计了专用钻具，取得了较好效果。     

软土地层地下连续墙成槽护壁泥浆研究

含砂性土等软土地层地下连续墙成槽施工,基槽侧壁易扰动坍塌,影响地下连续墙施工质量。降低泥浆失水量、适当提高泥浆粘度和防塌是护壁成槽的关键。结合宁波轨道交通车站基坑地下连续墙成槽施工,采用部分水解聚丙烯酰胺(PHP)、聚丙烯腈钙(CPAN)和硝基腐植酸钾(NKHm)作为添加剂,根据正交试验测定泥浆性能优化配比。研究表明：PHP失水量小,泥皮薄;CPAN和NKHm对降失水量效果明显,粘度适中。将试验结果应用于工程实践,护壁效果好。     

冲击反循环钻机施工地下连续墙与大口径灌注桩简介

简要介绍了CJF－20型冲击反循环钻机的特点、技术参数，以及应用冲击循环钻机施工三峡二期堰地下连续墙、部分大口径钻孔灌注桩工程实例。     

大直径空心桩技术现状及环形孔钻具的研究

概述了大直径空心桩施工技术的发展现状,在调研分析的基础上,借鉴地下连续墙施工技术,提出了一种新型的环形孔钻具,并对其结构、工作原理、应用条件及施工步骤等进行了阐述。     

插管悬挂式气举反循环钻具在地热井施工中的应用及改进

插管悬挂式气举反循环钻具是一种新型结构的气举反循环钻具。它不同于双壁式气举反循环钻具,而是通过插入一根独立的插管建立压缩空气通道,具有结构简单、使用方便、耐用性好、通用性强的特点。以工程实例为基础,对插管悬挂式气举反循环钻具在地热井施工中的钻具配置、专用工具及应用注意事项进行了说明,针对在地热井施工中出现的问题及改进方法进行了详细研究。     

地下连续墙成槽过程槽壁土体变形测试

为了分析地下连续墙成槽施工过程中对槽壁周边土体变形的影响程度,在南京河西地区某基坑工程的地下连续墙正式施工前进行了墙厚1.2 m、宽度4.5 m、深度61.0 m的成槽试验。结果表明,当成槽机向下开挖时,土体在不同深度处出现不同程度的向坑外的位移现象,部分监测数据显示为负值。在成槽施工完成后,水平位移变化出现缓慢回弹的趋势,并在成槽后的两天时间内变化速率渐渐变小。单幅地下连续墙成槽过程中槽壁周边土体的变形对环境影响不大。     

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。     

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.     

Inter-regional correlation of transgressions and regressions in the Cretaceous period

Well investigated platforms have been selected in each continent, and the history of Cretaceous transgressions and regressions there is concisely reviewed from the available evidence. The factual records have been summarized into a diagram and the timing of the events correlated between distant as well as adjoining areas.On a global scale, major transgressions were stepwise enlarged in space and time from the Neocomian, via Aptian-Albian, to the Late Cretaceous, and the post-Cretaceous regression was very remarkable. Minor cycles of transgression-regression were not always synchronous between different areas. Some of them were, however, nearly synchronous between the areas facing the same ocean.Tectono-eustasy may have been the main cause of the phenomena of transgression-regression, but certain kinds of other tectonic movements which affected even the so-called stable platforms were also responsible for the phenomena. The combined effects of various causes may have been unusual in the Cretaceous, since it was a period of global tectonic activity. The slowing down of this activity followed by readjustments may have been the cause of the global regression at the end of the Cretaceous.     

The lamprophyres of Afyon stratovolcano,western Anatolia,Turkey: description and genesis

The Afyon stratovolcano exhibits lamprophyric rocks, emplaced as hydrovolcanic products, aphanitic lava flows and dyke intrusions, during the final stages of volcanic activity. Most of the Afyon volcanics belong to the silica-saturated alkaline suite, as potassic trachyandesites and trachytes, while the products of the latest activity are lamproitic lamprophyres (jumillite, orendite, verite, fitztroyite) and alkaline lamprophyres (campto-sannaite, sannaite, hyalo-monchiquite, analcime–monchiquite). Afyon lamprophyres exhibit LILE and Zr enrichments, related to mantle metasomatism.     

METAMORPHIC PETROLOGY

正20140751 Guo Xincheng(Geological Party,BGMRED of Xinjiang,Changji 831100,China);Zheng Yuzhuang Determination and Geological Significance of the Mesoarchean Craton in Western Kunlun Mountains,Xinjiang,China(Geological Review,ISSN0371-5736,CN11-1952/P,59(3),2013,p.401-412,8     

GEOCHEMICAL EXPLORATION

正20141058 Chen Ling(Key Laboratory of Mathematical Geology of Sichuan Province,Chengdu University of Technology,Chengdu610059,China);Guo Ke Study of Geochemical Ore-Forming Anomaly Identification Based on the Theory of Blind Source Separation(Geosci-     

SEISMIC GEOLOGY

正20141334 Chen Kun(Institute of Geophysics,China Earthquake Administration,Beijing100081,China);Yu Yanxiang Shakemap of Peak Ground Acceleration with Bias Correction for the Lushan,Sichuan Earthquake on April20,2013(Seismology and Geology,ISSN0253-4967,CN11-2192/P,35(3),2013,p.627-633,2 illus.,1 table,9 refs.)Key words:great earthquakes,Sichuan Province     

HISTORICAL GEOLOGY & STRATIGRAPHY

正20141624 Cai Xiongfei(Key Laboratory of Geobiology and Environmental Geology,Ministry of Education,China University of Geosciences,Wuhan 430074,China);Yang Jie A Restudy of the Upper Sinian Zhengmuguan and Tuerkeng Formations in the Helan Mountains(Journal of Stratigraphy,ISSN0253-4959CN32-1187/P,37(3),2013,p.377-386,5 illus.,2 tables,10 refs.)     

PALEONTOLOGY

正20142263Lü Shaojun(Geological Survey of Jiangxi Province,Nanchang 330030,China)Early-Middle Permian Biostratigraphical Characteristics in Qiangduo Area,Tibet(Resources SurveyEnvironment,ISSN1671-4814,CN32-1640/N,34(4),2013,p.221-227,2illus.,2tables,22refs.)Key words:biostratigraphy,Lower Permian,Middle Permian,Tibet     

MATHEMATICAL GEOLOGY

正20142560Hu Hongxia(Regional Geological and Mineral Resources Survey of Jilin Province,Changchun 130022,China);Dai Lixia Application of GIS Map Projection Transformation in Geological Work(Jilin Geology,ISSN1001-2427,CN22-1099/P,32(4),2013,p.160-163,4illus.,2refs.)     

GEOCHEMISTRY

正20140692 Duo Tianhui(No.402 Geological Team,Exploration of Geology and Mineral Resources of Sichuan Authority,Chengdu611730,China);Wang Yongli Computer Simulation of Neptunium Existing Forms in the Groundwater(Computing Techniques for Geophysical and Geochemical Exploration,ISSN1001-1749,CN51-1242/P,35(3),