非饱和全空间埋置隧道动力响应半解析模型

将非饱和地基土视为由固、液、气组成的三相介质,圆形隧道衬砌简化为无限长的Flügge薄壁圆柱壳,分别采用Helmholtz矢量分解定理以及分离变量法求解非饱和地基土的波动方程和Flügge薄壁圆柱壳的振动控制方程。结合位移和应力连续性等边界条件,建立移动简谐荷载下非饱和地基土中埋置隧道动力响应的半解析模型。基于该模型,探讨了非饱和地基土-隧道系统的动力响应特征及饱和度对系统动力响应的影响。结果表明,饱和度对土体的动位移、动应力、超孔隙水压力及土体临界速度等影响较大,计算时应考虑饱和度的影响。     

成层地基中静压单桩挤土效应试验

采用室内模型试验研究了成层地基中静压桩沉桩过程,对模型桩整个沉桩过程中的挤土效应进行了分析研究。通过模型试验对在均质不同软硬地基中静力压入单桩过程产生的位移场进行了比较分析,获得了浅层土体、桩身周围、桩端处土体不同的位移变化模式,并揭示了桩周不同位置特别是软硬土层交界处土体位移随水平和深度方向的变化规律。试验结果表明,均质地基挤土位移的最大值与压桩深度存在滞后效应;对于成层地基,最大径向、竖向位移均出现在软硬土层交界面处,由于软硬土层力学性质的差异,土体位移主要表现为,软层处位移变大,硬层处位移变小。试验获得的结果便于进一步明确静压桩沉桩过程中挤土效应的内在机理,对预估沉桩的施工影响和指导沉桩设计都具有现实意义。     

饱和分层地基上列车运行引起的地面振动分析

基于薄层法原理,将圆柱坐标系下饱和土的Biot轴对称波动方程在竖向进行离散,沿切向坐标及轴向分别进行Fourier级数分解和Hankel变换,得到饱和层状介质中频域～波数域中的位移基本解表达式,再利用Hankel逆变换和Fourier综合,求得频域柱坐标系下的位移表达式。结合运行列车～轨道～地基的振动模型,对饱和分层地基上列车运行引起的地面振动进行分析。详细讨论了渗透系数、孔隙率、流体粘滞系数和剪切波速等饱和土层参数对振动传播与衰减的影响规律。研究表明：地基的第一层土体参数对列车运行引起的地面振动的影响比第二层土体参数的影响显著,饱和土体的渗透系数、孔隙流体动力粘滞系数、孔隙率和剪切波速是影响地面振动的主要参数。     

非饱和土半空间表面在垂直集中力作用下的Lamb问题

以多孔介质混合物理论为基础,同时引入土体双变量本构关系,得到了非饱和土中的一组动力控制方程。利用Hankel积分变换方法,直接对频域内的波动方程进行求解,得到了轴对称情况下土体骨架位移及应力分量在变换域内的解。在此基础上研究了非饱和土半空间体在垂直集中力作用下的动力响应,给出了Lamb问题积分形式解。当不计土中水、气的存在时,上述结果退化到单相弹性半空间中的经典Lamb解。通过数值计算分析,进一步研究了各物理参数对地基动力响应的影响规律。     

垂直集中表面荷载作用下非饱和土半空间中的Lamb问题

以多孔介质混合物理论为基础,同时引入土体双变量本构关系,得到了非饱和土中的一组动力控制方程.利用Hankel积分变换方法,对频域内的轴对称问题进行了求解.在此基础上研究了非饱和土半空间体在垂直集中力作用下的动力响应,给出了Lamb问题的积分形式解.当不计土中水、气的存在时,上述结果退化到单相弹性半空间中的经典Lamb解.数值计算结果表明:激振频率、渗透系数对地表位移影响显著,随激振频率的升高或渗透系数的降低,近场地表位移幅值减小,但当渗透系数低于一定值时,地表位移基本不再随其变化;饱和度对地表位移的直接影响是饱和度升高时,地表位移幅值略有减小.     

青藏铁路冻土路基活动层形成特性研究

在环境温度季节性变化的条件下进行室内模拟试验,探索了模拟冻土路基活动层形成的试验方法,研究了青藏高原多年冻土区路基活动层的形成活动规律。试验表明：活动层从初始形成到基本稳定过程中,近地表土层对外界温度场的变化响应灵敏,随外界温度的改变出现规律的波动;深层土层对外界温度的变化表现出滞后性,温度曲线波动幅度较小;活动层在趋于稳定的过程中土层的温度特征呈现出较为明显的区域相似性,在一定外温影响范围内土层温度场变化规律接近;在环境负温的初期表层土层迅速降温,活动层厚度开始逐渐减小,受外界气温及深层冻土冷源作用的共同影响,活动层冻结过程中会出现从上下边界同时冻结的现象,加快了活动层的冻结速度。     

饱和地基三维非轴对称动力响应

通过Laplace变换，建立了各向同性弹性饱和土在圆柱坐标系下，基于Laplace变换域内的Biot非轴对称波动方程；利用方位角的Fourier变换和径向Hankel变换，将波动方程转入为一组二阶常微分方程组；求解波动方程后，得到有限层厚的饱和地基的位移和应力通解;进而结合饱和地基的边界条件和排水条件，求解了任意竖向力作用下，饱和半空间地基的动力响应问题。     

黄土地区地上两层地铁车站抗震性能振动台试验

为研究黄土地区地下一层地上两层地铁车站结构的抗震性能,进行包括地上、地下结构及周围土层的振动台试验研究.在简要介绍模型设计和试验工况的基础上,重点根据试验中各传感器所记录的数据,对模型土箱的边界效应、模型地基与模型结构的动力反应、土与结构的相互作用等进行分析探讨.试验结果表明:地下一层地上两层地铁车站模型结构地上部分受输入地震动峰值加速度影响较大,地上部分的最终破坏模式是整体侧向倒塌;车站模型结构地下部分受地下结构周围土层影响较大,土层位移不大时地下结构无明显破坏;地上地下结构交接处的破坏最为严重.模型车站结构的存在对土体动力反应的影响较小,并随输入地震动峰值的增大而减弱.     

青藏铁路冻土路基活动层形成特性的试验研究

在环境温度季节性变化的条件下进行室内模拟试验,探索了模拟冻土路基活动层形成的试验方法,研究了青藏高原多年冻土区路基活动层的形成活动规律。试验表明:活动层从初始形成到基本稳定过程中,近地表土层对外界温度场的变化响应灵敏,随外界温度的改变出现规律的波动;深层土层对外界温度的变化表现出滞后性,温度曲线波动幅度较小;活动层在趋于稳定的过程中土层的温度特征呈现出较为明显的区域相似性,在一定外温影响范围内土层温度场变化规律接近;在环境负温的初期表层土层迅速降温,活动层厚度开始逐渐减小。受外界气温及深层冻土冷源作用的共同影响,活动层冻结过程中会出现从上下边界同时冻结的现象,加快了活动层的冻结速度。     

地铁运行振动诱发地层和地表动力响应分析

采用FLAC3D三维弹塑性动力有限差分模型,综合考虑地层和地表受振相互效应现象,对广州地铁某区间隧道运行列车振动诱发的地层和地表动力响应进行了分析。结果表明,在地铁运行振动作用下,地层的位移响应和速度响应向下和两侧衰减较快,但向上衰减较慢,对地表产生了较大范围的影响;地表振动加速度在隧道正上方强度最大,往两侧逐渐减弱,而在离开隧道轴线一定距离部位出现了一加强区。计算结果与现场实测数据吻合良好。     

Characterization of Ordovician carbonate reservoirs, southeastern Saskatchewan, Canada

The discovery of the prolific Ordovician Red River reservoirs in 1995 in southeastern Saskatchewan was the catalyst for extensive exploration activity which resulted in the discovery of more than 15 new Red River pools. The best yields of Red River production to date have been from dolomite reservoirs. Understanding the processes of dolomitization is, therefore, crucial for the prediction of the connectivity, spatial distribution and heterogeneity of dolomite reservoirs.The Red River reservoirs in the Midale area consist of 3～4 thin dolomitized zones, with a total thickness of about 20 m, which occur at the top of the Yeoman Formation. Two types of replacement dolomite were recognized in the Red River reservoir: dolomitized burrow infills and dolomitized host matrix. The spatial distribution of dolomite suggests that burrowing organisms played an important role in facilitating the fluid flow in the backfilled sediments. This resulted in penecontemporaneous dolomitization of burrow infills by normal seawater. The dolomite in the host matrix is interpreted as having occurred at shallow burial by evaporitic seawater during precipitation of Lake Almar anhydrite that immediately overlies the Yeoman Formation. However, the low δ18O values of dolomited burrow infills (-5.9‰～ -7.8‰, PDB) and matrix dolomites (-6.6‰～ -8.1‰, avg. -7.4‰ PDB) compared to the estimated values for the late Ordovician marine dolomite could be attributed to modification and alteration of dolomite at higher temperatures during deeper burial, which could also be responsible for its 87Sr/86Sr ratios (0.7084～0.7088) that are higher than suggested for the late Ordovician seawaters (0.7078～0.7080). The trace amounts of saddle dolomite cement in the Red River carbonates are probably related to "cannibalization" of earlier replacement dolomite during the chemical compaction.     

A computer generator for randomly layered structures

AcomputergeneratorforrandomlylayeredstructuresYUJia shun1,2,HEZhen hua2(1.TheInstituteofGeologicalandNuclearSciences,NewZealand;2.StateKeyLaboratoryofOilandGasReservoirGeologyandExploitation,ChengduUniversityofTechnology,China)Abstract:Analgorithmisintrod…     

海南岛地体及其毗邻陆缘晚中生代—新生代古地磁研究和构造演化

本文叙述了对海南岛及其毗邻大陆边缘白垩纪到第四纪地层岩石进行古地磁研究的全部工作过程。通过分析岩石中剩余磁矢量的磁偏角及磁倾角的变化,提出海南岛白垩纪以来经历的构造演化模式如下:早期伴随顺时针旋转而向南迁移,后期伴随逆时针转动并向北运移。联系该地区及邻区的地质、地球物理资料,对海南岛上述的构造地体运动提出以下认识:北部湾内早期有一拉张作用,主要是该作用使湾内地壳显著伸长减薄,形成北部湾盆地。从而导致了海南岛的早期构造运动,而海南岛后期的构造运动则主要是受南海海底扩张的影响。海南地体运动规律的阐明对于了解北部湾油气盆地的形成演化有重要的理论和实际意义。     

Exciton Seebeck in Molecular Systems

Various applications relevant to the exciton dynamics,such as the organic solar cell,the large-area organic light-emitting diodes and the thermoelectricity,are operating under temperature gradient.The potential abnormal behavior of the exicton dynamics driven by the temperature difference may affect the efficiency and performance of the corresponding devices.In the above situations,the exciton dynamics under temperature difference is mixed with     

Achieving Unusual States of Matter Under High Pressure

The elongation method,originally proposed by Imamura was further developed for many years in our group.As a method towards O(N)with high efficiency and high accuracy for any dimensional systems.This treatment designed for one-dimensional(ID)polymers is now available for three-dimensional(3D)systems,but geometry optimization is now possible only for 1D-systems.As an approach toward post-Hartree-Fock,it was also extended to     

《Chinese Science Bulletin》SUBJECT INDEX TO VOLUME 59(2014)

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An on-line scaling method for improving scalability of a database cluster

The explosive growth of the Internet and database applications has driven database to be more scalable and available, and able to support on-line scaling without interrupting service. To support more client's queries without downtime and degrading the response time, more nodes have to be scaled up while the database is running. This paper presents the overview of scalable and available database that satisfies the above characteristics. And we propose a novel on-line scaling method. Our method improves the existing on-line scaling method for fast response time and higher throughputs. Our proposed method reduces unnecessary network use, i.e. , we decrease the number of data copy by reusing the backup data. Also, our on-line scaling operation can be processed parallel by selecting adequate nodes as new node. Our performance study shows that our method results in significant reduction in data copy time.     

An improved R-tree based on childnode''s probability

R-Tree is a good structure for spatial searching. But in this indexing structure,either the sequence of nodes in the same level or sequence of traveling these nodes when queries are made is random. Since the possibility that the object appears in different MBR which have the same parents node is different, if we make the subnode who has the most possibility be traveled first, the time cost will be decreased in most of the cases. In some case, the possibility of a point belong to a rectangle will shows direct proportion with the size of the rectangle. But this conclusion is based on an assumption that the objects are symmetrically distributing in the area and this assumption is not always coming into existence. Now we found a more direct parameter to scale the possibility and made a little change on the structure of R-tree, to increase the possibility of founding the satisfying answer in the front sub trees. We names this structure probability based arranged R-tree (PBAR-tree).     

An Index mechanism for multi-scale view in spatial databases

There are numerous geometric objects stored in the spatial databases. An importance function in a spatial database is that users can browse the geometric objects as a map efficiently. Thus the spatial database should display the geometric objects users concern about swiftly onto the display window. This process includes two operations:retrieve data from database and then draw them onto screen. Accordingly, to improve the efficiency, we should try to reduce time of both retrieving object and displaying them. The former can be achieved with the aid of spatial index such as R-tree, the latter require to simplify the objects. Simplification means that objects are shown with sufficient but not with unnecessary detail which depend on the scale of browse. So the major problem is how to retrieve data at different detail level efficiently. This paper introduces the implementation of a multi-scale index in the spatial database SISP (Spatial Information Shared Platform) which is generalized from R-tree. The difference between the generalization and the R-tree lies on two facets: One is that every node and geometric object in the generalization is assigned with a importance value which denote the importance of them, and every vertex in the objects are assigned with a importance value,too. The importance value can be use to decide which data should be retrieve from disk in a query. The other difference is that geometric objects in the generalization are divided into one or more sub-blocks, and vertexes are total ordered by their importance value. With the help of the generalized R-tree, one can easily retrieve data at different detail levels.Some experiments are performed on real-life data to evaluate the performance of solutions that separately use normal spatial index and multi-scale spatial index. The results show that the solution using multi-scale index in SISP is satisfying.     

Integrating GIS Web services based on mediating architecture

The geographic information service is enabled by the advancements in general Web service technology and the focused efforts of the OGC in defining XML-based Web GIS service. Based on these models, this paper addresses the issue of services chaining,the process of combining or pipelining results from several interoperable GIS Web Services to create a customized solution. This paper presents a mediated chaining architecture in which a specific service takes responsibility for performing the process that describes a service chain. We designed the Spatial Information Process Language (SIPL) for dynamic modeling and describing the service chain, also a prototype of the Spatial Information Process Execution Engine (SIPEE) is implemented for executing processes written in SIPL. Discussion of measures to improve the functionality and performance of such system will be included.