强化工程造价管理,加大城建投资监管力度

改革开放以来,特别是“九五”期间,我国加大了城市建设的力度,巨额资金不断注入,建设者们日夜辛劳,城市面貌由此产生了巨变。 以广州市为例,1998～2002年,用于市政、公用等城市基础设施的建设资金每年都保持在140亿元以上,这五年城建投资的总量达到了750亿元,比过去几十年的投资总和还多几倍。但由于我国城     

Quaternary high-resolution opal record and its paleoproductivity implication at ODP Site 1143,southern South China Sea

The correlation of opal content and MAR with oxygen isotopic records of benthonic foraminifera at Site 1143, southern South China Sea indicates that,since about 900 ka,the increasing opal content and MAR during the interglacial periods is inferred to reflect the bigher surface productivity ,for the intensified summer monsoon during the interglacial periods would result in the enhanced upwelling and nutrient supply,Time-sequence spectral analyses of oxygen isotopic record ,opal content and MAR at intervals of 0-900 ka reveal that the changes of surface productivity were dominantly forced by the variations of the earth orbital cycles.     

溪洛渡施工总布置三维动态可视化图形仿真研究

溪洛渡水电站是在金沙江拟建的最大水电站，为直观准确地描述其施工总布置设计所涉及的各施工环节之间复杂的动态空间关系，将施工总布置系统分为若干子系统，对整个设计施工过程进行动态可视化图形仿真研究。设计3维动态图形仿真数据流向，将溪洛渡施工总布置动态图形仿真数据分为空间数据和属性数据，以GIS为平台组织数据结构，构造施工总布置3维动态可视化数字模型；在3维动态可视化数字基础上实现施工总布置3维动态可视化图形仿真演示和动态图形仿真数据可视化查询，给施工总布置设计与决策提供一个科学、直观的可视化分析途径。     

解乘数法用于工程保障组织的优化分析

工程保障组织优化分析属于多目标决策问题，定性分析与判断是其原则上的指导。通过对兵力与工程任务分配问题进行数学建模，经量化分析与计算生成合理组织方案，实现最大的工程保障效能。“解乘数法”用于求解工程保障组织数学模型，计算简便，结果直观。     

在硅基材料上用Sol-gel法制备涂层测定氧扩散系数研究

提出一种测定氧扩散系数新方法。用Sol-gel法制备了Y2O3/SiO2均匀致密的薄膜,能成功解决其它方法无法得到的冶炼所得到的熔体,光学椭偏测定氧化层的膜厚。探讨了氧在薄膜中的扩散,在Wagner理论基础上,用数学方法表达在掺杂SiO2薄膜氧扩散系数与氧化层膜厚的关系。     

在硅基材料上用Sol-gel法制备涂层测定氧扩散系数研究

提出一种测定氧扩散系数新方法.用Sol-gel法制备了Y2O3/SiO2均匀致密的薄膜,能成功解决其它方法无法得到的冶炼所得到的熔体,光学椭偏测定氧化层的膜厚.探讨了氧在薄膜中的扩散,在Wagner理论基础上,用数学方法表达在掺杂SiO2薄膜氧扩散系数与氧化层膜厚的关系.     

对非经营性政府投资工程管理模式的比较与选择

对我国目前政府投资项目中的非经营性政府投资工程建设管理中存在的问题进行了分析，指出其管理上的弊端，提出要对这类项目推行专业化的建设管理制度、比较了目前我国内地两种典型政府投资项目工程管理模式的优缺点，提出了可供选择的政府投资工程管理的过渡模式．     

聚氨酯建筑密封材料在渠道防渗工程中的施工及应用

渠道及水工建筑物在运行管理中，保证工程安全和效益充分发挥是水利工程管理单位的首要任务，防渗工程设计和施工质量的好坏直接影响工程的安全和效益，选择安全、可靠的防渗止水材料及施工技术是防渗工程成功的关键。     

Evolution of the South China Sea and monsoon history revealed in deep-sea records

As the third summary report of ODP Leg 184 to the South China Sea (SCS), this paper discusses the evolution of the East Asian monsoon and the SCS basin. A multi-proxy approach, involving geochemistry, micropale-ontology, pollen and other analyses, was adopted for reconstructing the evolutionary history of the East Asian monsoon, which was characterized by a series of paleo-climate events especially at 8, 3.2, 2.2 and 0.4 Ma. The new record indicates similar stages in the development of the East and South Asian monsoons, with an enhanced winter monsoon over East Asia being the major difference. The rich spectrums of monsoon variability from the southern SCS also reveal other characteristic features of the low latitude ocean. Evidence for the evolution of the SCS includes the hemipelagic Oligocene sediments, implying the existence of deep water environments during the early seafloor spreading stage of the SCS basin. The four major unconformities and some remarkabl ediagenetic features in upper Oligocene deposits indicate the strongest tectonic events in the region. From a careful comparison of lithologies and sedimentation rates, we conclude that the prominent differences in sedimentary environments between the southern and northern SCS were established only by ～3 Ma.