基于动三轴试验和土层地震反应对地震液化的判别

以汉口某场地典型钻孔剖面为研究对象,结合动三轴试验成果,采用等效线性化方法考虑土层的非线性特征,利用一维波动方法进行场地土层地震反应分析,探讨场地内埋深10~36 m范围内的各土层在不同地震作用下的液化可能性。结果表明,汉口地区埋深超过20 m的砂土层在Ⅶ度、Ⅷ度地震作用下有液化的可能性;土层液化的可能性随着埋深的增大而减小;输入地震动的频谱特性及平稳段持续时间等因素可影响液化判别结果。该方法可为深层液化判别提供参考。     

陕西省西咸新区黄土场地海绵设施渗漏对建筑物的影响

黄土场地近建筑物海绵设施建设时常铺设防渗膜,以避免雨水入渗引起地基变形破坏。施工过程中防渗膜的意外破损时有发生,讨论近建筑物基础防渗膜局部破坏引起的工程风险有助于推进类似地区海绵城市建设。以陕西省西咸新区海绵城市建设中某一典型工程为依托,采用Geo Studio软件对周边建筑物典型海绵设施发生的渗漏问题进行数值模拟分析,得到了渗漏后土体饱和度、基础沉降和地基土应力分布变化特性,分析了渗漏点雨水入渗对地基的影响。结果表明:渗漏会使地基产生不均匀沉降;渗漏点距基础边缘水平距离越近,所产生的附加沉降越大,渗漏导致的最大沉降量约为4 mm,满足《建筑地基基础设计规范》(GB 50007—2011)要求。另外,当渗漏点距基础边缘水平距离大于1 m时,渗漏对地基强度的影响迅速降低;当距离大于3 m时,渗漏对地基的影响可以忽略。在本文工程背景下,渗漏导致地基破坏可能性较小。     

塔河油田海西早期岩溶古水系识别方法及其特征

塔河油田海西早期形成了复杂的碳酸盐岩岩溶缝洞系统,其发育规模在东部地区和西部地区表现出显著的差异性。岩溶水作为岩溶发育的关键因素,在不同地质背景下表现出的水文学特征及水动力作用与岩溶缝洞系统的发育密切相关。为了深入认识和阐述岩溶储层发育机制,基于三维地震资料,通过地震属性技术结合现代岩溶理论成果恢复了塔河油田埋深5 000 m以下的古水文网络,精细描述了水系发育特征。研究结果表明:东部地区地表水系统具有较大汇水量,水系以强烈的垂向侵蚀作用为主,发育了完整的地表-地下双重水系型水文网络系统;西部地区地表水以水平溶蚀作用为主,地貌较为平缓,尚未产生大型地下水系网络系统,属于地表水系型水文网络系统。东、西部地区地表、地下水文系统动力学机制的不同,为这2个地区岩溶储层发育的差异性提供了合理解释。      

对太原地区浅层地下水的脆弱性评价

参照DRASTIC模型,选择地下水埋深、净补给量、土壤介质及包气带介质作为评价因子构建DRSI模型。基于DRSI模型,通过MapGIS软件的空间分析功能对太原地区浅层地下水进行了脆弱性评价,评价结果表明,太原地区浅层地下水整体上西部脆弱性高于东部,南部高于北部。     

高压旋喷注浆法在建筑物桩基托换加固中的应用

针对兰州某小区商住楼已形成不均匀沉降的地基,根据场地施工条件、地基条件和建筑物的结构特征,对该工程地基选择了高压旋喷注浆法进行加固,加固结果表明:加固前及加固初期地基沉降速率较大,加固施工完成后沉降速率变小,加固完成两个月后沉降稳定,加固效果良好。通过该工程实践表明:高压旋喷注浆法在复杂地基中对既有建筑物的加固处理虽然是可行的,但同时必须根据地基土的特点采取相应的切实可行的技术措施,才能使地基加固处理达到预期的效果。其加固原理既有旋喷桩的托换加固之功效,又有静压注浆加固之作用。     

黄河三角洲地区砂土路基液化机理探讨及处置

从砂土路基液化机理人手,结合黄河三角洲地区地基土工程地质特征,对该地区路基砂土液化做现场振动试验,找出影响砂土路基液化的影响因素,主要内因有土体的密实度、含水量和土体中是否存在软弱区;主要外因有荷载的大小、作用时间和荷载频率。并针对砂土液化的内外因,结合青银高速公路强夯处理案例展开分析,提出了处理方法。     

平顶山市平原区第四系工程地质特征浅议

本文拟对平顶山城市平原区埋深在30m以内的松散土体,进行了工程地质层的划分,并对各层的工程地质特征进行了测试和论述,这对城建工程规划部署将是有益的。     

郑州大学东校区场地地震地质条件及抗震设防应对措施

通过校区建筑场地钻孔岩土剖面与剪切波速测试结果以及地震地质背景条件、活动断裂及其影响和主要抗震设防参数的分析研究 ,作者认为建筑场地属中软土 ,但不存在液化可能性 ,建筑场地类别可定为Ⅱ类 ;并提出近场区存在 6级及小于 6级的地震背景 ,其地震烈度可估评为 7度。鉴于此 ,建议建筑场地可采用换土垫层法以加固地基 ,对高层建筑可采用大直径灌注桩基础、框架柱可一柱一桩、剪力墙宜设基础梁并适当扩大桩距、建筑体适当埋深和设置地下室等系列抗震设防措施     

基于PS-InSAR技术的廊坊北部地区地面沉降监测研究

采用PS-InSAR技术对覆盖廊坊北部地区的33景Envisat ASAR影像进行处理,获取该地区2007～2010年平均形变速率场与季度时序沉降信息,并与沉降影响场数据进行耦合分析。结果表明： 1)宋庄-燕郊与五百户-大口屯等地区沉降发育较显著,季节性变动特征明显;2)山前与杨各庄-马坊地区呈高沉降梯度,平原区较高沉降梯度区多与-16 mm/a、0 mm/a等值线形态一致,差异性沉降特征显著;3)因第四系厚度、结构显著差异与断裂活动影响,北、东部断层两侧多表现为较高或渐变的形变梯度;4)差异性沉降展布与水源地、水位降深区具较好空间响应,且较严重沉降多为中深层承压水超采与城镇化建设所致。     

武汉主城区液化潜能分区研究

搜集并整理武汉主城区地震安全性评价控制性钻孔SPT-N资料,配合武汉市地震动参数小区划成果,采用规范法对各场地土层在罕遇地震作用下液化可能性进行判别。以液化指数作为分区指标并结合各场地坐标,绘制武汉主城区液化潜能分区图。分区图初步预测了罕遇地震发生以后,可能发生液化的区域及其严重性,且表明无论是分布面积还是液化潜能,长江右岸均大于长江左岸。通过与4次历史大震液化资料的对比分析,武汉主城区可能液化场地具有地下水位埋深浅、液化土层分布范围广、埋藏深度大的特点。     

Thermohaline structure inhomogeneity associated with polynia at the northern margin of Emery Ice-shelf

Based on the hydrographic data in austral summer during the 22nd Antarctic Expedition of China(2005/2006),some features can be found about the northern margin of Emery ice shelf as follows.The heat content in the surface layer(0-50 m) at the eastern end and the western end of the ice-shelf margin is much higher than that at the middle.The upper mixing-layer depth and the seasonal thermocline depth at the middle of the ice-shelf northern margin are much shallower than those at the both ends.However there is much less difference between the middle and the ends in the bottom layer.The remote sensing photos show that the inhomogeneity in the surface-layer water is closely related to the spatial distribution of the floes and polynia in the area.     

Phylogenetic analysis of cultivable bacteria isolated from Arctic sea-ice

Phylogenetic analysis based on 16S rDNA of 8 strains of cultivable bacteria isolated from Arctic sea-ice was studied.The results showed that strain BJ1 belonged to genus Planococcus,which was a genus of low mole percent G C gram-positive bacteria;strain BJ6 belonged to genus Burkholderia of β-proteobacteria and the rest 6 strain all belonged to γ-proteobacteria,of which strain BJ8 was a species of Pseudoalteromonas,strain BJ2-BJ5 and BJ7 were members of genus Psychrobacter.Phylogenetic analysis also indicated that bacteria of genus Psychrobacter of the isolates formed a relatively independent phylogenetic cluster in comparison with other bacteria belonged to genus Psychrobacter.     

Information for authors

正1 Aims and Scope Advances in Polar Science(APS)is an international,peer-reviewed journal jointly sponsored by the Polar Research Institute of China and the Chinese Arctic and Antarctic Administration.APS is a comprchensive academic journal dedicated to presentation of multi-disciplinary achievements in Arctic and Antarctic expeditions and research.Its primary purpose is to publish achievements in fundamental research,applied     

Advances in Polar Science CONTENTS(Volume 25,2014)

正~~     

Guide to Authors： Journal of Mountain Science

<正>AIMS AND SCOPE(Editorial Policy)The Journal of Mountain Science(JMS)is devoted to mountains and their surrounding lowlands-ecoregions of particular global importance,with a particular emphasis on the important highlands/mountains in the world,such as the Tibetan Plateau,the Himalayas,the Alps,the Andes,the Rockies and many other mountain ranges of our planet.     

Journal of Mountain Science(JMS)

<正>The Journal of Mountain Science(JMS),founded in2004,is an international English-language journal on mountain sciences.JMS is supervised by the Chinese Academy of Sciences(CAS),sponsored by the Chengdu Institute of Mountain Hazards and Environment,CAS,published by Science Press China,and distributed by Springer exclusively throughout the world(excluding Mainland China).The JMS is published bimonthly,fulltexted in SpringerLink and CNKI,indexed/abstracted by     

Relationship of Arctic sea ice and Northern Hemispheric 500 hPa Polar vortices

Using the NCEP/NCAR reanalysis monthly 500 hPa height data on a 2.5 latitude-longitude grid and 1°×1° sea ice data,the polar vortex area,intensity index and arctic sea ice area index are calculated respectively,and the meridional distribution,period variation and the abrupts in the long range trend are analyzed to study their relationship.The results show that the meridional distribution of sea ice and polar vortex h-ave distinctive difference,the relative positions of them are different in the eastern and western hemispheres,and exept they have periods of 4 months,quasi half year,quasi year,4-5 years and 10 years commonly,and each of them has its own respective variation as well.The sea ice area is decreasing apparently since 1980's,so is the polar vortex area,but their abrupt changge time are different totally.The area of sea ice and polar vortex has prominent positive correlation,but the relationship of sea ice intensity,polar vortex intensity,polar vortex area is complicated.     

Author Index for Journal of Mountain Science Volume 11,2014,pp 1-1656

<正>~~     

Information for Authors

<正>The Journal of Ocean University of China(Oceanic and Coastal Sea Research)is a comprehensive academic quarterly sponsored by the Ocean University of China,published one volume per year.This journal is devoted to the publication of the theoretical and applied research